{"type": "FeatureCollection", "features": [{"id": "10.3389/feart.2021.660333", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-08-25T16:19:05Z", "type": "Journal Article", "created": "2021-03-12", "title": "Editorial: Novel Isotope Systems and Biogeochemical Cycling During Cryospheric Weathering in Polar Environments", "description": "Cryospheric weathering processes in permafrost and glaciated environments play an essential role in carbon cycling within the Earth system. Chemical weathering of silicate, carbonate and sulfidebearing rocks releases cations and anions that can consume (or release) atmospheric carbon dioxide (CO2), as well as biologically important nutrients such as phosphorous, iron and silicon, which can impact downstream ecosystems (Figure 1). How these cryospheric weathering processes will respond to future climate-driven changes in permafrost thaw and glacial melt is difficult to predict due to the role of complex forcing mechanisms and feedbacks. Isotope geochemistry utilizes changes in the relative abundance of different isotopes due to physical, chemical and biological reactions, allowing some of the complexities of cryospheric weathering processes to be unpicked. In recent years, there has been an explosion in the range of stable and radiogenic isotope systems used for the study of high-latitude environments, including isotopes of major elements such as carbon, oxygen, and silicon (e.g., Opfergelt et al., 2013; Kutscher et al., 2017), and trace metal isotopes such as strontium (Hindshaw et al., 2014), lithium (Murphy et al., 2019), iron (Zhang et al., 2015), uranium-series (e.g., Arendt et al., 2018) and rare earth elements (e.g., Clinger et al., 2016). This research topic explores some of the developments in high-latitude field and experimental studies that utilize such geochemical tools to trace the degree and nature of weathering reactions that play a critical role in carbon cycling. The nine contributions to the research topic involve the analysis of traditional (C, N, S, O) and non-traditional (Mg, Li, Si, Ge) isotopes from different samples types such as river waters, lake waters, rocks, sediments, or mineral separates from locations both in the Northern (Greenland, Iceland, Canada, Svalbard) and Southern Hemisphere (Patagonia, Antarctica). Two papers use isotope geochemistry to explore organic and inorganic carbon cycling within permafrost and active layer soils. Jones et al. show that biogeochemical processes and decomposition pathways of organic carbon in ice-wedge polygons in Svalbard are dependent upon water and organic carbon content. Sulfur (\u03b434S) and oxygen (\u03b418O) isotopes show that iron and sulfate reduction processes dominate in water saturated, high organic carbon environments, whereas sulfide oxidation dominates in drier areas with less organic carbon. Zolkos and Tank use an experimental approach in combination with stable carbon isotopes (\u03b413CO2) to show that carbonate weathering coupled with sulfide oxidation in recently or previously unthawed Canadian permafrost sediments is a net source of inorganic CO2 to the atmosphere, albeit partly counterbalanced by carbonate buffering.", "keywords": ["glacier", "550", "Science", "Q", "551", "cryosphere", "01 natural sciences", "7. Clean energy", "13. Climate action", "14. Life underwater", "isotope", "permafrost", "geochemistry", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.3389/feart.2021.660333"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Frontiers%20in%20Earth%20Science", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.3389/feart.2021.660333", "name": "item", "description": "10.3389/feart.2021.660333", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.3389/feart.2021.660333"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-03-11T00:00:00Z"}}, {"id": "10.3389/fevo.2023.1106461", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-08-25T16:19:06Z", "type": "Journal Article", "created": "2023-03-20", "title": "Primary production in subsidized green-brown food webs", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Ecosystems worldwide receive large amounts of nutrients from both natural processes and human activities. While direct subsidy effects on primary production are relatively well-known (the green food web), the indirect effects of subsidies on producers as mediated by the brown food web and predators are poorly considered. With a dynamical green-brown food web model, parameterized using empirical estimates from the literature, we illustrate the effect of organic and inorganic nutrient subsidies on net primary production (NPP) (i.e., after removing loss to herbivory) in two idealized ecosystems\u2014one terrestrial and one aquatic. We find that nutrient subsidies increase net primary production, an effect that saturates with increasing subsidies. Changing the quality of subsidies from inorganic to organic tends to increase net primary production in terrestrial ecosystems, but less often so in aquatic ecosystems. This occurs when organic nutrient inputs promote detritivores in the brown food web, and hence predators that in turn regulate herbivores, thereby promoting primary production. This previously largely overlooked effect is further enhanced by ecosystem properties such as fast decomposition and low rates of nutrient additions and demonstrates the importance of nutrient subsidy quality on ecosystem functioning.</p></article>", "keywords": ["2. Zero hunger", "Ekologi", "ecosystem modeling", "food web", "Ecology", "nutrient subsidy", "Evolution", "organic fertilization", "15. Life on land", "551", "trophic cascade", "13. Climate action", "ecosystem function", "QH359-425", "QH540-549.5", "primary production"], "contacts": [{"organization": "Zelnik, Yuval, Manzoni, Stefano, Bommarco, Riccardo,", "roles": ["creator"]}]}, "links": [{"href": "https://pub.epsilon.slu.se/30719/1/zelnik-y-r-et-al-20230421.pdf"}, {"href": "https://doi.org/10.3389/fevo.2023.1106461"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Frontiers%20in%20Ecology%20and%20Evolution", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.3389/fevo.2023.1106461", "name": "item", "description": "10.3389/fevo.2023.1106461", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.3389/fevo.2023.1106461"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2023-03-20T00:00:00Z"}}, {"id": "10.3390/rs12101671", "type": "Feature", "geometry": null, "properties": {"updated": "2026-08-25T16:19:21Z", "type": "Journal Article", "created": "2020-05-25", "title": "Temporal Calibration of an Evaporation-Based Spatial Disaggregation Method of SMOS Soil Moisture Data", "description": "<p>The resolution of current satellite surface soil moisture (SM) estimates is very low, of tens of kilometers, which proves to be insufficient for various agricultural and hydrological applications. Amongst the existing downscaling approaches of remotely sensed SM, DISPATCH (DISaggregation based on a Physical And Theoretical scale CHange) improves the resolution of SMOS (Soil Moisture and Ocean Salinity) soil moisture data using soil evaporative efficiency (SEE) estimates at high resolution (HR) and a SEE(SM) model implemented at low resolution (LR). Defined as the ratio of actual to potential soil evaporation, SEE can be derived from the remotely sensed land surface temperature (LST) and normalized difference vegetation index (NDVI). The current version of DISPATCH uses a linear SEE(SM) model. This study aims at improving the SEE(SM) model and testing different calibration strategies, to ultimately have more robust and better downscaled SM products. A nonlinear SEE(SM) model is introduced and its influence on the derived HR SM products is studied over a range of conditions. Each model, linear and nonlinear, is calibrated from remote sensing data on a daily and a multi-date basis. The approaches were tested over two mixed dry and irrigated areas in Catalonia, Spain, and over one dry area in Morocco. When using the linear model, better statistical results were generally obtained using a daily calibration (current version of DISPATCH), most notably over one Spanish site. However, the best results were systematically obtained for an annually calibrated nonlinear model, in terms of all metrics considered: correlation coefficient, slope of the linear regression, bias, unbiased root mean square error. In particular, when using the annually calibrated nonlinear SEE (SM) model, the temporal slope of the linear regression between disaggregated and in situ soil moisture increased to 1.16 and 0.75 for one Spanish site and for the Moroccan site (as opposed to 0.44 and 0.58, respectively, when using the linear model with a daily calibration). The temporal correlation coefficient increased to 0.47 and 0.54 over the Spanish sites (as opposed to 0.18 and 0.27, respectively, when using the linear model with a daily calibration). Those contrasted results indicate compensation effects between the model type and the calibration strategy. Taking into account studies that report the strong nonlinear behavior of the SEE with respect to SM, the introduction of the nonlinear SEE(SM) model in DISPATCH, combined with a multi-date calibration, is proven to perform significantly better under various conditions, leading to more robust disaggregated SM products. The SEE modeling based on the nonlinear SM model, with a multi-date calibration, could be integrated into the CATDS\uffe2\uff80\uff94Centre Aval de Traitement des Donn\uffc3\uffa9es SMOS as a future product, as well as into existing evapotranspiration models, which are based on a combination of thermal and microwave data.</p>", "keywords": ["550", "Science", "Evaporation", "0207 environmental engineering", "02 engineering and technology", "551", "01 natural sciences", "evaporation", "Disaggregation", "Downscaling", "14. Life underwater", "[SDU.STU.HY]Sciences of the Universe [physics]/Earth Sciences/Hydrology", "0105 earth and related environmental sciences", "Q", "downscaling", "15. Life on land", "[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces", " environment", "6. Clean water", "MODIS", "13. Climate action", "disaggregation", "[SDU.STU.HY] Sciences of the Universe [physics]/Earth Sciences/Hydrology", "Soil moisture", "[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces", "soil moisture", "environment", "SMOS"]}, "links": [{"href": "http://www.mdpi.com/2072-4292/12/10/1671/pdf"}, {"href": "https://www.mdpi.com/2072-4292/12/10/1671/pdf"}, {"href": "https://doi.org/10.3390/rs12101671"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Remote%20Sensing", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.3390/rs12101671", "name": "item", "description": "10.3390/rs12101671", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.3390/rs12101671"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2020-05-23T00:00:00Z"}}, {"id": "10.5194/bg-11-2027-2014", "type": "Feature", "geometry": null, "properties": {"updated": "2026-08-25T16:19:46Z", "type": "Journal Article", "created": "2014-04-10", "description": "<p>Abstract. The LPJ-GUESS dynamic vegetation model uniquely combines an individual- and patch-based representation of vegetation dynamics with ecosystem biogeochemical cycling from regional to global scales. We present an updated version that includes plant and soil N dynamics, analysing the implications of accounting for C\uffe2\uff80\uff93N interactions on predictions and performance of the model. Stand structural dynamics and allometric scaling of tree growth suggested by global databases of forest stand structure and development were well reproduced by the model in comparison to an earlier multi-model study. Accounting for N cycle dynamics improved the goodness of fit for broadleaved forests. N limitation associated with low N-mineralisation rates reduces productivity of cold-climate and dry-climate ecosystems relative to mesic temperate and tropical ecosystems. In a model experiment emulating free-air CO2 enrichment (FACE) treatment for forests globally, N limitation associated with low N-mineralisation rates of colder soils reduces CO2 enhancement of net primary production (NPP) for boreal forests, while some temperate and tropical forests exhibit increased NPP enhancement. Under a business-as-usual future climate and emissions scenario, ecosystem C storage globally was projected to increase by ca. 10%; additional N requirements to match this increasing ecosystem C were within the high N supply limit estimated on stoichiometric grounds in an earlier study. Our results highlight the importance of accounting for C\uffe2\uff80\uff93N interactions in studies of global terrestrial N cycling, and as a basis for understanding mechanisms on local scales and in different regional contexts.                     </p>", "keywords": ["570", "QE1-996.5", "info:eu-repo/classification/ddc/550", "550", "Ecology", "ddc:550", "Geology", "15. Life on land", "551", "01 natural sciences", "Earth sciences", "Life", "13. Climate action", "ddc:570", "QH501-531", "616", "XXXXXX - Unknown", "nitrogen cycle", "carbon cycle (biogeochemistry)", "ecosystems", "QH540-549.5", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.5194/bg-11-2027-2014"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Biogeosciences", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.5194/bg-11-2027-2014", "name": "item", "description": "10.5194/bg-11-2027-2014", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5194/bg-11-2027-2014"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2013-11-28T00:00:00Z"}}, {"id": "10.5194/bg-16-3747-2019", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-08-25T16:19:47Z", "type": "Journal Article", "created": "2019-10-02", "title": "Reviews and syntheses: Turning the challenges of partitioning ecosystem evaporation and transpiration into opportunities", "description": "<p>Abstract. Evaporation (E) and transpiration (T) respond differently to ongoing changes in climate, atmospheric composition, and land use. It is difficult to partition ecosystem-scale evapotranspiration (ET) measurements into E and T, which makes it difficult to validate satellite data and land surface models. Here, we review current progress in partitioning E and T and provide a prospectus for how to improve theory and observations going forward. Recent advancements in analytical techniques create new opportunities for partitioning E and T at the ecosystem scale, but their assumptions have yet to be fully tested. For example, many approaches to partition E and T rely on the notion that plant canopy conductance and ecosystem water use efficiency exhibit optimal responses to atmospheric vapor pressure deficit (D). We use observations from 240 eddy covariance flux towers to demonstrate that optimal ecosystem response to D is a reasonable assumption, in agreement with recent studies, but more analysis is necessary to determine the conditions for which this assumption holds. Another critical assumption for many partitioning approaches is that ET can be approximated as T during ideal transpiring conditions, which has been challenged by observational studies. We demonstrate that T can exceed 95\uffe2\uff80\uff89% of ET from certain ecosystems, but other ecosystems do not appear to reach this value, which suggests that this assumption is ecosystem-dependent with implications for partitioning. It is important to further improve approaches for partitioning E and T, yet few multi-method comparisons have been undertaken to date. Advances in our understanding of carbon\uffe2\uff80\uff93water coupling at the stomatal, leaf, and canopy level open new perspectives on how to quantify T via its strong coupling with photosynthesis. Photosynthesis can be constrained at the ecosystem and global scales with emerging data sources including solar-induced fluorescence, carbonyl sulfide flux measurements, thermography, and more. Such comparisons would improve our mechanistic understanding of ecosystem water fluxes and provide the observations necessary to validate remote sensing algorithms and land surface models to understand the changing global water cycle.                     </p>", "keywords": ["550", "STOMATAL CONDUCTANCE", "0207 environmental engineering", "02 engineering and technology", "551", "01 natural sciences", "Life", "CARBONYL SULFIDE COS", "QH501-531", "SOIL-WATER", "QH540-549.5", "0105 earth and related environmental sciences", "QE1-996.5", "info:eu-repo/classification/ddc/550", "VAPOR-PRESSURE DEFICIT", "RAINFALL INTERCEPTION", "Ecology", "ddc:550", "Biology and Life Sciences", "Geology", "STABLE-ISOTOPE", "15. Life on land", "540", "6. Clean water", "SURFACE-ENERGY BALANCE", "Environmental sciences", "Earth sciences", "Ecology", " evolutionary biology", "13. Climate action", "Earth and Environmental Sciences", "NET PRIMARY PRODUCTIVITY", "WATER-USE EFFICIENCY", "Geosciences", "EDDY COVARIANCE DATA"]}, "links": [{"href": "https://bg.copernicus.org/articles/16/3747/2019/bg-16-3747-2019.pdf"}, {"href": "https://doi.org/10.5194/bg-16-3747-2019"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Biogeosciences", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.5194/bg-16-3747-2019", "name": "item", "description": "10.5194/bg-16-3747-2019", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5194/bg-16-3747-2019"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-10-01T00:00:00Z"}}, {"id": "10.5194/bg-19-5125-2022", "type": "Feature", "geometry": null, "properties": {"updated": "2026-08-25T16:19:47Z", "type": "Journal Article", "created": "2022-11-10", "title": "Management-induced changes in soil organic carbon  on global croplands", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Abstract. Soil organic carbon (SOC), one of the largest terrestrial carbon (C) stocks on Earth, has been depleted by anthropogenic land cover change and agricultural management. However, the latter has so far not been well represented in global C stock assessments. While SOC models often simulate detailed biochemical processes that lead to the accumulation and decay of SOC, the management decisions driving these biophysical processes are still little investigated at the global scale. Here we develop a spatially explicit data set for agricultural management on cropland, considering crop production levels, residue returning rates, manure application, and the adoption of irrigation and tillage practices. We combine it with a reduced-complexity model based on the Intergovernmental Panel on Climate Change (IPCC) tier\u00a02 method to create a half-degree resolution data set of SOC stocks and SOC stock changes for the first 30\u2009cm of mineral soils. We estimate that, due to arable farming, soils have lost around 34.6\u2009GtC relative to a counterfactual hypothetical natural state in 1975. Within the period 1975\u20132010, this SOC debt continued to expand by 5\u2009GtC (0.14\u2009GtC\u2009yr\u22121) to around 39.6\u2009GtC. However, accounting for historical management led to 2.1\u2009GtC fewer (0.06\u2009GtC\u2009yr\u22121) emissions than under the assumption of constant management. We also find that management decisions have influenced the historical SOC trajectory most strongly by residue returning, indicating that SOC enhancement by biomass retention may be a promising negative emissions technique. The reduced-complexity SOC model may allow us to simulate management-induced SOC enhancement \u2013 also within computationally demanding integrated (land use) assessment modeling.                     </p></article>", "keywords": ["570", "AGRICULTURE", "550", "Supplementary Data", "QH301 Biology", "agricultural management", "crop production", "SEQUESTRATION", "551", "01 natural sciences", "630", "NITROGEN-CYCLE", "QH301", "Life", "land cover", "QH501-531", "SDG 13 - Climate Action", "soil carbon", "SDG 2 - Zero Hunger", "EMISSIONS", "CROPS", "QH540-549.5", "global change", "SDG 15 - Life on Land", "0105 earth and related environmental sciences", "2. Zero hunger", "QE1-996.5", "Ecology", "INTENSIFICATION", "VEGETATION MODEL", "Geology", "LAND-USE CHANGE", "15. Life on land", "carbon sequestration", "CLIMATE", "COVER CHANGE", "agricultural land", "13. Climate action", "trajectory", "Intergovernmental Panel on Climate Change"]}, "links": [{"href": "https://bg.copernicus.org/articles/19/5125/2022/bg-19-5125-2022.pdf"}, {"href": "https://doi.org/10.5194/bg-19-5125-2022"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Biogeosciences", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.5194/bg-19-5125-2022", "name": "item", "description": "10.5194/bg-19-5125-2022", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5194/bg-19-5125-2022"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2020-12-22T00:00:00Z"}}, {"id": "10.5194/essd-13-4349-2021", "type": "Feature", "geometry": null, "properties": {"updated": "2026-08-25T16:19:52Z", "type": "Journal Article", "created": "2021-09-07", "title": "ERA5-Land: a state-of-the-art global reanalysis dataset for land applications", "description": "<p>Abstract. Framed within the Copernicus Climate Change Service (C3S) of the European Commission, the European Centre for Medium-Range Weather Forecasts (ECMWF) is producing an enhanced global dataset for the land component of the fifth generation of European ReAnalysis (ERA5), hereafter referred to as ERA5-Land. Once completed, the period covered will span from 1950 to the present, with continuous updates to support land monitoring applications. ERA5-Land describes the evolution of the water and energy cycles over land in a consistent manner over the production period, which, among others, could be used to analyse trends and anomalies. This is achieved through global high-resolution numerical integrations of the ECMWF land surface model driven by the downscaled meteorological forcing from the ERA5 climate reanalysis, including an elevation correction for the thermodynamic near-surface state. ERA5-Land shares with ERA5 most of the parameterizations that guarantees the use of the state-of-the-art land surface modelling applied to numerical weather prediction (NWP) models. A main advantage of ERA5-Land compared to ERA5 and the older ERA-Interim is the horizontal resolution, which is enhanced globally to 9\uffe2\uff80\uff89km compared to 31\uffe2\uff80\uff89km (ERA5) or 80\uffe2\uff80\uff89km (ERA-Interim), whereas the temporal resolution is hourly as in ERA5. Evaluation against independent in situ observations and global model or satellite-based reference datasets shows the added value of ERA5-Land in the description of the hydrological cycle, in particular with enhanced soil moisture and lake description, and an overall better agreement of river discharge estimations with available observations. However, ERA5-Land snow depth fields present a mixed performance when compared to those of ERA5, depending on geographical location and altitude. The description of the energy cycle shows comparable results with ERA5. Nevertheless, ERA5-Land reduces the global averaged root mean square error of the skin temperature, taking as reference MODIS data, mainly due to the contribution of coastal points where spatial resolution is important. Since January\uffc2\uffa02020, the ERA5-Land period available has extended from January\uffc2\uffa01981 to the near present, with a 2- to 3-month delay with respect to real time. The segment prior to 1981 is in production, aiming for a release of the whole dataset in summer/autumn\uffc2\uffa02021. The high spatial and temporal resolution of ERA5-Land, its extended period, and the consistency of the fields produced makes it a valuable dataset to support hydrological studies, to initialize NWP and climate models, and to support diverse applications dealing with water resource, land, and environmental management. The full ERA5-Land hourly (Mu\uffc3\uffb1oz-Sabater,\uffc2\uffa02019a) and monthly (Mu\uffc3\uffb1oz-Sabater,\uffc2\uffa02019b) averaged datasets presented in this paper are available through the C3S Climate Data Store at https://doi.org/10.24381/cds.e2161bac and https://doi.org/10.24381/cds.68d2bb30, respectively.                     </p>", "keywords": ["QE1-996.5", "550", "IN-SITU", "LEAF-AREA", "[SDU.STU]Sciences of the Universe [physics]/Earth Sciences", "Geology", "OPERATIONAL IMPLEMENTATION", "15. Life on land", "551", "SOIL-MOISTURE", "SURFACE-TEMPERATURE", "01 natural sciences", "LAKE PARAMETERIZATION", "[SDU] Sciences of the Universe [physics]", "Environmental sciences", "[SDU]Sciences of the Universe [physics]", "13. Climate action", "Earth and Environmental Sciences", "[SDU.STU] Sciences of the Universe [physics]/Earth Sciences", "SNOW MODELS", "GE1-350", "WEST-AFRICA", "SATELLITE", "NUMERICAL WEATHER PREDICTION", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://centaur.reading.ac.uk/106796/1/essd-13-4349-2021.pdf"}, {"href": "https://essd.copernicus.org/articles/13/4349/2021/essd-13-4349-2021.pdf"}, {"href": "https://doi.org/10.5194/essd-13-4349-2021"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Earth%20System%20Science%20Data", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.5194/essd-13-4349-2021", "name": "item", "description": "10.5194/essd-13-4349-2021", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5194/essd-13-4349-2021"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-03-15T00:00:00Z"}}, {"id": "10.5194/gmd-10-2875-2017", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-08-25T16:19:53Z", "type": "Journal Article", "created": "2017-07-27", "title": "The Analytical Objective Hysteresis Model (AnOHM v1.0): methodology to determine bulk storage heat flux coefficients", "description": "<p>Abstract. The net storage heat flux (\uffce\uff94QS) is important in the urban surface energy balance (SEB) but its determination remains a significant challenge. The hysteresis pattern of the diurnal relation between the \uffce\uff94QS and net all-wave radiation (Q\uffe2\uff88\uff97) has been captured in the Objective Hysteresis Model (OHM) parameterization of \uffce\uff94QS. Although successfully used in urban areas, the limited availability of coefficients for OHM hampers its application. To facilitate use, and enhance physical interpretations of the OHM coefficients, an analytical solution of the one-dimensional advection\uffe2\uff80\uff93diffusion equation of coupled heat and liquid water transport in conjunction with the SEB is conducted, allowing development of AnOHM (Analytical Objective Hysteresis Model). A sensitivity test of AnOHM to surface properties and hydrometeorological forcing is presented using a stochastic approach (subset simulation). The sensitivity test suggests that the albedo, Bowen ratio and bulk transfer coefficient, solar radiation and wind speed are most critical. AnOHM, driven by local meteorological conditions at five sites with different land use, is shown to simulate the \uffce\uff94QS flux well (RMSE values of \uffe2\uff88\uffbc\uffe2\uff80\uffaf30\uffe2\uff80\uffafW\uffe2\uff80\uffafm\uffe2\uff88\uff922). The intra-annual dynamics of OHM coefficients are explored. AnOHM offers significant potential to enhance modelling of the surface energy balance over a wider range of conditions and land covers.                     </p>", "keywords": ["QE1-996.5", "13. Climate action", "11. Sustainability", "0207 environmental engineering", "Geology", "02 engineering and technology", "15. Life on land", "551", "01 natural sciences", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://centaur.reading.ac.uk/71108/8/gmd-10-2875-2017.pdf"}, {"href": "https://gmd.copernicus.org/articles/10/2875/2017/gmd-10-2875-2017.pdf"}, {"href": "https://doi.org/10.5194/gmd-10-2875-2017"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Geoscientific%20Model%20Development", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.5194/gmd-10-2875-2017", "name": "item", "description": "10.5194/gmd-10-2875-2017", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5194/gmd-10-2875-2017"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-01-10T00:00:00Z"}}, {"id": "10.5194/gmd-12-3503-2019", "type": "Feature", "geometry": null, "properties": {"updated": "2026-08-25T16:19:53Z", "type": "Journal Article", "created": "2019-08-12", "title": "ORCHIDEE MICT-LEAK (r5459), a global model for the production, transport, and transformation of dissolved organic carbon from Arctic permafrost regions \u2013 Part 1: Rationale, model description, and simulation protocol", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Abstract. Few Earth system models adequately represent the unique permafrost soil biogeochemistry and its respective processes; this significantly contributes to uncertainty in estimating their responses, and that of the planet at large, to warming. Likewise, the riverine component of what is known as the \u201cboundless carbon cycle\u201d is seldom recognised in Earth system modelling. The hydrological mobilisation of organic material from a \u223c1330\u20131580\u2009PgC carbon stock to the river network results in either sedimentary settling or atmospheric \u201cevasion\u201d, processes widely expected to increase with amplified Arctic climate warming. Here, the production, transport, and atmospheric release of dissolved organic carbon (DOC) from high-latitude permafrost soils into inland waters and the ocean are explicitly represented for the first time in the land surface component (ORCHIDEE) of a CMIP6 global climate model (Institut Pierre Simon Laplace \u2013 IPSL). The model, ORCHIDEE MICT-LEAK, which represents the merger of previously described ORCHIDEE versions MICT and LEAK, mechanistically represents (a)\u00a0vegetation and soil physical processes for high-latitude snow, ice, and soil phenomena and (b)\u00a0the cycling of DOC and CO2, including atmospheric evasion, along the terrestrial\u2013aquatic continuum from soils through the river network to the coast at 0.5 to 2\u2218 resolution. This paper, the first in a two-part study, presents the rationale for including these processes in a high-latitude-specific land surface model, then describes the model with a focus on novel process implementations, followed by a summary of the model configuration and simulation protocol. The results of these simulation runs, conducted for the Lena River basin, are evaluated against observational data in the second part of this study.                     </p></article>", "keywords": ["QE1-996.5", "550", "Geology", "15. Life on land", "551", "01 natural sciences", "6. Clean water", "Sciences de la terre et du cosmos", "[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry", "13. Climate action", "[SDU.STU.GC] Sciences of the Universe [physics]/Earth Sciences/Geochemistry", "[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology", "Sciences pharmaceutiques", "[SDU.STU.GL] Sciences of the Universe [physics]/Earth Sciences/Glaciology", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://dipot.ulb.ac.be/dspace/bitstream/2013/292778/1/doi_276405.pdf"}, {"href": "https://doi.org/10.5194/gmd-12-3503-2019"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Geoscientific%20Model%20Development", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.5194/gmd-12-3503-2019", "name": "item", "description": "10.5194/gmd-12-3503-2019", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5194/gmd-12-3503-2019"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-03-25T00:00:00Z"}}, {"id": "21.11116/0000-0009-5A8B-6", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-08-25T16:22:39Z", "type": "Journal Article", "created": "2021-08-28", "title": "Impacts of Drying and Rewetting on the Radiocarbon Signature of Respired CO2 and Implications for Incubating Archived Soils", "description": "Abstract<p>The radiocarbon signature of respired CO2 (\uffe2\uff88\uff8614C\uffe2\uff80\uff90CO2) measured in laboratory soil incubations integrates contributions from soil carbon pools with a wide range of ages, making it a powerful model constraint. Incubating archived soils enriched by \uffe2\uff80\uff9cbomb\uffe2\uff80\uff90C\uffe2\uff80\uff9d from mid\uffe2\uff80\uff9020th century nuclear weapons testing would be even more powerful as it would enable us to trace this pulse over time. However, air\uffe2\uff80\uff90drying and subsequent rewetting of archived soils, as well as storage duration, may alter the relative contribution to respiration from soil carbon pools with different cycling rates. We designed three experiments to assess air\uffe2\uff80\uff90drying and rewetting effects on \uffe2\uff88\uff8614C\uffe2\uff80\uff90CO2 with constant storage duration (Experiment 1), without storage (Experiment 2), and with variable storage duration (Experiment 3). We found that air\uffe2\uff80\uff90drying and rewetting led to small but significant (\uffce\uffb1\uffc2\uffa0&lt;\uffc2\uffa00.05) shifts in \uffe2\uff88\uff8614C\uffe2\uff80\uff90CO2 relative to undried controls in all experiments, with grassland soils responding more strongly than forest soils. Storage duration (4\uffe2\uff80\uff9314\uffc2\uffa0y) did not have a substantial effect. Mean differences (95% CIs) for experiments 1, 2, and 3 were: 23.3\uffe2\uff80\uffb0 (\uffc2\uffb16.6), 19.6\uffe2\uff80\uffb0 (\uffc2\uffb110.3), and 29.3\uffe2\uff80\uffb0 (\uffc2\uffb129.1) for grassland soils, versus \uffe2\uff88\uff9211.6\uffe2\uff80\uffb0 (\uffc2\uffb14.1), 12.7\uffe2\uff80\uffb0 (\uffc2\uffb18.5), and \uffe2\uff88\uff9224.2\uffe2\uff80\uffb0 (\uffc2\uffb113.2) for forest soils. Our results indicate that air\uffe2\uff80\uff90drying and rewetting soils mobilizes a slightly older pool of carbon that would otherwise be inaccessible to microbes, an effect that persists throughout the incubation. However, as the bias in \uffe2\uff88\uff8614C\uffe2\uff80\uff90CO2 from air\uffe2\uff80\uff90drying and rewetting is small, measuring \uffe2\uff88\uff8614C\uffe2\uff80\uff90CO2 in incubations of archived soils appears to be a promising technique for constraining soil carbon models.</p", "keywords": ["Dewey Decimal Classification::500 | Naturwissenschaften::550 | Geowissenschaften", "soil archives", "ddc:631.41", "04 agricultural and veterinary sciences", "incubation", "15. Life on land", "01 natural sciences", "climate change", "13. Climate action", "ddc:551.9", "ddc:550.724", "radiocarbon", "0401 agriculture", " forestry", " and fisheries", "soil carbon", "soil carbon modeling", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2020JG006119"}, {"href": "https://doi.org/21.11116/0000-0009-5A8B-6"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Geophysical%20Research%3A%20Biogeosciences", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "21.11116/0000-0009-5A8B-6", "name": "item", "description": "21.11116/0000-0009-5A8B-6", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/21.11116/0000-0009-5A8B-6"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-09-01T00:00:00Z"}}, {"id": "2117/345717", "type": "Feature", "geometry": null, "properties": {"updated": "2026-08-25T16:22:40Z", "type": "Journal Article", "created": "2021-05-17", "title": "Estimating lockdown-induced European NO2 changes using satellite and surface observations and air quality models", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Abstract. This study provides a comprehensive assessment of NO2 changes across the main European urban areas induced by COVID-19 lockdowns using satellite retrievals from the Tropospheric Monitoring Instrument (TROPOMI) onboard the Sentinel-5p satellite, surface site measurements, and simulations from the Copernicus Atmosphere Monitoring Service (CAMS) regional ensemble of air quality models. Some recent TROPOMI-based estimates of changes in atmospheric NO2 concentrations have neglected the influence of weather variability between the reference and lockdown periods. Here we provide weather-normalized estimates based on a machine learning method (gradient boosting) along with an assessment of the biases that can be expected from methods that omit the influence of weather. We also compare the weather-normalized satellite-estimated NO2 column changes with weather-normalized surface NO2 concentration changes and the CAMS regional ensemble, composed of 11 models, using recently published estimates of emission reductions induced by the lockdown. All estimates show similar NO2 reductions. Locations where the lockdown measures were stricter show stronger reductions, and, conversely, locations where softer measures were implemented show milder reductions in NO2 pollution levels. Average reduction estimates based on either satellite observations (\u221223\u2009%), surface stations (\u221243\u2009%), or models (\u221232\u2009%) are presented, showing the importance of vertical sampling but also the horizontal representativeness. Surface station estimates are significantly changed when sampled to the TROPOMI overpasses (\u221237\u2009%), pointing out the importance of the variability in time of such estimates. Observation-based machine learning estimates show a stronger temporal variability than model-based estimates.</p></article>", "keywords": ["[SDE] Environmental Sciences", "550", "QC1-999", "551", "COVID-19 (Malaltia)", "01 natural sciences", "COVID-19 (Malaltia) -- Aspectes ambientals", "COVID-19 (Disease)", "Lockdown", "11. Sustainability", "Satellite images", "QD1-999", "0105 earth and related environmental sciences", "info:eu-repo/classification/ddc/550", "Air quality models", "Physics", "Aire -- Qualitat", "COVID-19", "Surface observations", "Satellite observations", "Chemistry", "Meteorology and Atmospheric Sciences", "13. Climate action", "[SDE]Environmental Sciences", "Air quality", "Meteorologi och atmosf\u00e4rsvetenskap", "\u00c0rees tem\u00e0tiques de la UPC::Desenvolupament hum\u00e0 i sostenible::Degradaci\u00f3 ambiental::Contaminaci\u00f3 atmosf\u00e8rica", ":Desenvolupament hum\u00e0 i sostenible::Degradaci\u00f3 ambiental::Contaminaci\u00f3 atmosf\u00e8rica [\u00c0rees tem\u00e0tiques de la UPC]"]}, "links": [{"href": "https://doi.org/2117/345717"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Atmospheric%20Chemistry%20and%20Physics", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "2117/345717", "name": "item", "description": "2117/345717", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/2117/345717"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-05-17T00:00:00Z"}}, {"id": "10.7185/geochemlet.1506", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-08-25T16:21:50Z", "type": "Journal Article", "created": "2015-06-04", "title": "Copper isotope evidence for large-scale sulphide fractionation during Earth\u2019s differentiation", "description": "The differentiation of Earth into a metallic core and silicate mantle left its signature on the chemical and isotopic composition of the bulk silicate Earth (BSE). This is seen in the depletion of siderophile (metal-loving) relative to lithophile (rock-loving) elements in Earth\u2019s mantle as well as the silicon isotope offset between primitive meteorites (i.e. bulk Earth) and BSE, which is generally interpreted as a proof that Si is present in Earth\u2019s core. Another putative light element in Earth\u2019s core is sulphur; however, estimates of core S abundance vary significantly and, due to its volatile nature, no unequivocal S isotopic signature for core fractionation has thus far been detected. Here we present new high precision isotopic data for Cu, a chalcophile (sulphur-loving) element, which shows that Earth\u2019s mantle is isotopically fractionated relative to bulk Earth. Results from high pressure equilibration experiments suggest that the sense of Cu isotopic fractionation between BSE and bulk Earth requires that a sulphide-rich liquid segregated from Earth\u2019s mantle during differentiation, which likely entered the core. Such an early-stage removal of a sulphide-rich phase from the mantle presents a possible solution to the long-standing 1st terrestrial lead paradox.", "keywords": ["S in the core", "Terrestrial Pb paradox", "GB", "550", "NDAS", "[SDU.ASTR.EP] Sciences of the Universe [physics]/Astrophysics [astro-ph]/Earth and Planetary Astrophysics [astro-ph.EP]", "551", "01 natural sciences", "Planetary differentiation", "13. Climate action", "Core formation", "GB Physical geography", "[SDU.STU.GC] Sciences of the Universe [physics]/Earth Sciences/Geochemistry", "Cu isotopes", "BDC", "Terrestrial Pb paradox.", "R2C", "0105 earth and related environmental sciences"]}, "links": [{"href": "http://dro.dur.ac.uk/15741/1/15741.pdf"}, {"href": "https://doi.org/10.7185/geochemlet.1506"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Geochemical%20Perspectives%20Letters", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.7185/geochemlet.1506", "name": "item", "description": "10.7185/geochemlet.1506", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.7185/geochemlet.1506"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2015-01-01T00:00:00Z"}}, {"id": "10.7185/gold2021.7214", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-08-25T16:21:51Z", "type": "Journal Article", "created": "2021-11-08", "title": "Radium inputs into the Arctic Ocean from rivers: a basin-wide estimate", "description": "Abstract<p>Radium isotopes have been used to trace nutrient, carbon, and trace metal fluxes inputs from ocean margins. However, these approaches require a full accounting of radium sources to the coastal ocean including rivers. Here, we aim to quantify river radium inputs into the Arctic Ocean for the first time for 226Ra and to refine the estimates for 228Ra. Using new and existing data, we find that the estimated combined (dissolved plus desorbed) annual 226Ra and 228Ra fluxes to the Arctic Ocean are [7.0\uffe2\uff80\uff939.4] \uffc3\uff97 1014 dpm y\uffe2\uff88\uff921 and [15\uffe2\uff80\uff9318] \uffc3\uff97 1014 dpm y\uffe2\uff88\uff921, respectively. Of these totals, 44% and 60% of the river 226Ra and 228Ra, respectively are from suspended sediment desorption, which were estimated from laboratory incubation experiments. Using Ra isotope data from 20 major rivers around the world, we derived global annual 226Ra and 228Ra fluxes of [7.4\uffe2\uff80\uff9317] \uffc3\uff97 1015 and [15\uffe2\uff80\uff9327] \uffc3\uff97 1015 dpm y\uffe2\uff88\uff921, respectively. As climate change spurs rapid Arctic warming, hydrological cycles are intensifying and coastal ice cover and permafrost are diminishing. These river radium inputs to the Arctic Ocean will serve as a valuable baseline as we attempt to understand the changes that warming temperatures are having on fluxes of biogeochemically important elements to the Arctic coastal zone.</p", "keywords": ["550", "Radium isotopes", "F700", "15. Life on land", "551", "01 natural sciences", "river fluxes", "River fluxes", "radium isotopes", "13. Climate action", "Arctic Ocean", "SDG 14 - Life Below Water", "14. Life underwater", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://nrl.northumbria.ac.uk/id/eprint/50000/9/JGR%20Oceans%20-%202022%20-%20Bullock%20-%20Radium%20Inputs%20Into%20the%20Arctic%20Ocean%20From%20Rivers%20%20A%20Basin%E2%80%90Wide%20Estimate.pdf"}, {"href": "https://doi.org/10.7185/gold2021.7214"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Goldschmidt2021%20abstracts", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.7185/gold2021.7214", "name": "item", "description": "10.7185/gold2021.7214", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.7185/gold2021.7214"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-01-01T00:00:00Z"}}, {"id": "10138/579229", "type": "Feature", "geometry": null, "properties": {"updated": "2026-08-25T16:21:58Z", "type": "Journal Article", "created": "2024-06-11", "title": "Impact of Dust Source Patchiness on the Existence of a Constant Dust Flux Layer During Aeolian Erosion Events", "description": "Abstract<p>Dust emission fluxes during wind soil erosion are usually estimated using a dust concentration vertical gradient, by assuming a constant dust flux layer between the surface and the dust measurement levels. Here, we investigate the existence of this layer during erosion events recorded in Iceland and Jordan. Size\uffe2\uff80\uff90resolved dust fluxes were estimated at three levels between 2 and 4\uffc2\uffa0m using the eddy\uffe2\uff80\uff90covariance method. Dust fluxes were found mainly constant only between the two upper levels in Iceland, the lower dust flux being often stronger and richer in coarse particles, while dust fluxes in Jordan were nearly constant across all levels. The wind dynamics could not explain the absence of a constant dust flux layer in Iceland. We show that the presence of stationary dust source patches in Iceland, related to surface humidity, created a non\uffe2\uff80\uff90uniform dust layer near the surface, named dust roughness sublayer (DRSL), where individual plumes behind each patch interact but do not fully mix. The lowest dust measurement level was probably located within this sublayer while the upper ones were located above, such that there the emitted dust became spatially well\uffe2\uff80\uff90mixed. This explains near the surface in Iceland, the more intermittent dust concentration, its low correlation with the dust concentrations above, and the richer dust flux in coarse particles due to their lower deposition contribution. Our findings highlight the importance of estimating dust fluxes above a dust blending height whose characteristics depend on the dust source patchiness caused by surface humidity or the presence of sparse non\uffe2\uff80\uff90erosive elements.</p", "keywords": ["[SDE] Environmental Sciences", "Aeolian erosion events", "Geologie", " Hydrologie", " Meteorologie", "550", "dust flux", "Soil wind erosion", "Ensure access to affordable", " reliable", " sustainable and modern energy for all", "Dust flux layer", "0207 environmental engineering", "02 engineering and technology", "Constant flux layer", "\u00c0rees tem\u00e0tiques de la UPC::Enginyeria agroaliment\u00e0ria::Ci\u00e8ncies de la terra i de la vida", "551", "01 natural sciences", "http://metadata.un.org/sdg/7", "Make cities and human settlements inclusive", " safe", " resilient and sustainable", "Dust flux", "Simulaci\u00f3 per ordinador", "Atmospheric surface layer", "size distribution", "Climate science", "0105 earth and related environmental sciences", "info:eu-repo/classification/ddc/550", "ddc:550", "Size distribution", "15. Life on land", "520", "Physical sciences", "Earth sciences", "13. Climate action", "[SDE]Environmental Sciences", "Soil erosion", "soil wind erosion", "http://metadata.un.org/sdg/11", "constant flux layer"]}, "links": [{"href": "https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2023JD040657"}, {"href": "https://hal.inrae.fr/hal-04618242/file/JGR%20Atmospheres%20-%202024%20-%20Dupont%20-%20Impact%20of%20Dust%20Source%20Patchiness%20on%20the%20Existence%20of%20a%20Constant%20Dust%20Flux%20Layer%20During.pdf"}, {"href": "https://doi.org/10138/579229"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Geophysical%20Research%3A%20Atmospheres", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10138/579229", "name": "item", "description": "10138/579229", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10138/579229"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-06-11T00:00:00Z"}}, {"id": "2336203031", "type": "Feature", "geometry": null, "properties": {"updated": "2026-08-25T16:22:45Z", "type": "Journal Article", "created": "2016-04-20", "title": "Modeling soil evaporation efficiency in a range of soil and atmospheric conditions using a meta\u2010analysis approach", "description": "Abstract<p>A meta\uffe2\uff80\uff90analysis data\uffe2\uff80\uff90driven approach is developed to represent the soil evaporative efficiency (SEE) defined as the ratio of actual to potential soil evaporation. The new model is tested across a bare soil database composed of more than 30 sites around the world, a clay fraction range of 0.02\uffe2\uff80\uff930.56, a sand fraction range of 0.05\uffe2\uff80\uff930.92, and about 30,000 acquisition times. SEE is modeled using a soil resistance (rss) formulation based on surface soil moisture (\uffce\uffb8) and two resistance parameters   and \uffce\uffb8efolding. The data\uffe2\uff80\uff90driven approach aims to express both parameters as a function of observable data including meteorological forcing, cut\uffe2\uff80\uff90off soil moisture value   at which SEE=0.5, and first derivative of SEE at  , named  . An analytical relationship between   and   is first built by running a soil energy balance model for two extreme conditions with rss\uffe2\uff80\uff89=\uffe2\uff80\uff890 and   using meteorological forcing solely, and by approaching the middle point from the two (wet and dry) reference points. Two different methods are then investigated to estimate the pair   either from the time series of SEE and \uffce\uffb8 observations for a given site, or using the soil texture information for all sites. The first method is based on an algorithm specifically designed to accomodate for strongly nonlinear   relationships and potentially large random deviations of observed SEE from the mean observed  . The second method parameterizes   as a multi\uffe2\uff80\uff90linear regression of clay and sand percentages, and sets   to a constant mean value for all sites. The new model significantly outperformed the evaporation modules of ISBA (Interaction Sol\uffe2\uff80\uff90Biosph\uffc3\uffa8re\uffe2\uff80\uff90Atmosph\uffc3\uffa8re), H\uffe2\uff80\uff90TESSEL (Hydrology\uffe2\uff80\uff90Tiled ECMWF Scheme for Surface Exchange over Land), and CLM (Community Land Model). It has potential for integration in various land\uffe2\uff80\uff90surface schemes, and real calibration capabilities using combined thermal and microwave remote sensing data.</p", "keywords": ["550", "0207 environmental engineering", "modeling", "02 engineering and technology", "15. Life on land", "551", "01 natural sciences", "evaporation", "soil", "moisture", "[SDU.STU.HY] Sciences of the Universe [physics]/Earth Sciences/Hydrology", "[SDU.STU.HY]Sciences of the Universe [physics]/Earth Sciences/Hydrology", "texture", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2015WR018233"}, {"href": "https://doi.org/2336203031"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Water%20Resources%20Research", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "2336203031", "name": "item", "description": "2336203031", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/2336203031"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2016-05-01T00:00:00Z"}}, {"id": "1959.7/uws:76872", "type": "Feature", "geometry": null, "properties": {"updated": "2026-08-25T16:22:28Z", "type": "Journal Article", "created": "2024-01-08", "title": "Extreme drought impacts have been underestimated in grasslands and shrublands globally", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Climate change is increasing the frequency and severity of short-term (~1 y) drought events\u2014the most common duration of drought\u2014globally. Yet the impact of this intensification of drought on ecosystem functioning remains poorly resolved. This is due in part to the widely disparate approaches ecologists have employed to study drought, variation in the severity and duration of drought studied, and differences among ecosystems in vegetation, edaphic and climatic attributes that can mediate drought impacts. To overcome these problems and better identify the factors that modulate drought responses, we used a coordinated distributed experiment to quantify the impact of short-term drought on grassland and shrubland ecosystems. With a standardized approach, we imposed ~a single year of drought at 100 sites on six continents. Here we show that loss of a foundational ecosystem function\u2014aboveground net primary production (ANPP)\u2014was 60% greater at sites that experienced statistically extreme drought (1-in-100-y event) vs. those sites where drought was nominal (historically more common) in magnitude (35% vs. 21%, respectively). This reduction in a key carbon cycle process with a single year of extreme drought greatly exceeds previously reported losses for grasslands and shrublands. Our global experiment also revealed high variability in drought response but that relative reductions in ANPP were greater in drier ecosystems and those with fewer plant species. Overall, our results demonstrate with unprecedented rigor that the global impacts of projected increases in drought severity have been significantly underestimated and that drier and less diverse sites are likely to be most vulnerable to extreme drought.</p></article>", "keywords": ["[SDE] Environmental Sciences", "Medical Sciences", "Drought Severity", "550", "580 Plants (Botany)", "551", "Tierras de Matorral", "Medical Specialties", "Medicine and Health Sciences", "SDG 13 - Climate Action", "climate extreme | Drought-Net | International Drought Experiment | productivity", "Productividad Primaria Neta", "Net Primary Productivity", "Productivity", "2. Zero hunger", "Praderas", "Productividad", "Life Sciences", "Biological Sciences", "Grassland", "6. Clean water", "Droughts", "Grasslands", "[SDE]Environmental Sciences", "Drought-Net", "Public Health", "International Drought Experiment", "Ciclo del Carbono", "Severidad de la Sequ\u00eda", "Global Impacts", "productivity", "Climate Change", "climate extreme", "333", "Carbon Cycle", "Environmental Public Health", "XXXXXX - Unknown", "Impacto Global", "Scrublands", "General", "Biology", "Ecosystem", "Experimento internacional de Sequ\u00eda", "500", "Receptor Protein-Tyrosine Kinases", "15. Life on land", "Clima Extremo", "Climate Science", "13. Climate action", "Cambio Clim\u00e1tico", "Extreme Climate", "Climate extreme", "Klimatvetenskap"]}, "links": [{"href": "https://boris.unibe.ch/191349/1/smith-et-al-2024-extreme-drought-impacts-have-been-underestimated-in-grasslands-and-shrublands-globally.pdf"}, {"href": "https://escholarship.org/content/qt9b707158/qt9b707158.pdf"}, {"href": "https://doi.org/1959.7/uws:76872"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Proceedings%20of%20the%20National%20Academy%20of%20Sciences", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "1959.7/uws:76872", "name": "item", "description": "1959.7/uws:76872", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/1959.7/uws:76872"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-01-08T00:00:00Z"}}, {"id": "1805/19605", "type": "Feature", "geometry": null, "properties": {"updated": "2026-08-25T16:22:22Z", "type": "Journal Article", "created": "2018-10-19", "title": "Isotopic evidence for oligotrophication of terrestrial ecosystems", "description": "Human societies depend on an Earth system that operates within a constrained range of nutrient availability, yet the recent trajectory of terrestrial nitrogen (N) availability is uncertain. Examining patterns of foliar N concentrations and isotope ratios (\u03b415N) from more than 43,000 samples acquired over 37\u2009years, here we show that foliar N concentration declined by 9% and foliar \u03b415N declined by 0.6-1.6\u2030. Examining patterns across different climate spaces, foliar \u03b415N declined across the entire range of mean annual temperature and mean annual precipitation tested. These results suggest declines in N supply relative to plant demand at the global scale. In all, there are now multiple lines of evidence of declining N availability in many unfertilized terrestrial ecosystems, including declines in \u03b415N of tree rings and leaves from herbarium samples over the past 75-150\u2009years. These patterns are consistent with the proposed consequences of elevated atmospheric carbon dioxide and longer growing seasons. These declines will limit future terrestrial carbon uptake and increase nutritional stress for herbivores.", "keywords": ["0106 biological sciences", "570", "Nitrogen", "[SDV]Life Sciences [q-bio]", "577", "terrestrial nitrogen", "Nutritional stress", "551", "01 natural sciences", "oligotrophication", "Isotopes", "https://purl.org/becyt/ford/1.6", "Terrestrial carbon uptake", "https://purl.org/becyt/ford/1", "Ecosystem", "580", "2. Zero hunger", "Nitrogen Isotopes", "terrestrial ecosystems", "isotopic", "Eutrophication", "Plants", "15. Life on land", "sylviculture", "Nitrogen; Nitrogen Isotopes; Plants; Ecosystem; Eutrophication", "[SDV] Life Sciences [q-bio]", "element cycles", "foliar", "13. Climate action", "nutrient availability"]}, "links": [{"href": "https://cris.unibo.it/bitstream/11585/704621/3/Craine_2018_isotopic.pdf"}, {"href": "https://www.nature.com/articles/s41559-018-0694-0.pdf"}, {"href": "https://doi.org/1805/19605"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Nature%20Ecology%20%26amp%3B%20Evolution", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "1805/19605", "name": "item", "description": "1805/19605", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/1805/19605"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-10-22T00:00:00Z"}}, {"id": "1854/LU-8528923", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-08-25T16:22:23Z", "type": "Journal Article", "created": "2017-03-23", "title": "A review of spatial downscaling of satellite remotely sensed soil moisture", "description": "Abstract<p>Satellite remote sensing technology has been widely used to estimate surface soil moisture. Numerous efforts have been devoted to develop global soil moisture products. However, these global soil moisture products, normally retrieved from microwave remote sensing data, are typically not suitable for regional hydrological and agricultural applications such as irrigation management and flood predictions, due to their coarse spatial resolution. Therefore, various downscaling methods have been proposed to improve the coarse resolution soil moisture products. The purpose of this paper is to review existing methods for downscaling satellite remotely sensed soil moisture. These methods are assessed and compared in terms of their advantages and limitations. This review also provides the accuracy level of these methods based on published validation studies. In the final part, problems and future trends associated with these methods are analyzed.</p", "keywords": ["TIME-DOMAIN REFLECTOMETRY", "550", "IN-SITU", "downscaling", "MODIS TOA RADIANCES", "AMSR-E", "15. Life on land", "551", "01 natural sciences", "LAND-SURFACE TEMPERATURE", "REMEDHUS NETWORK SPAIN", "6. Clean water", "3. Good health", "[SDU] Sciences of the Universe [physics]", "L-BAND RADIOMETER", "remote sensing", "EVAPORATIVE FRACTION", "[SDU]Sciences of the Universe [physics]", "13. Climate action", "Earth and Environmental Sciences", "soil moisture", "SOUTHERN GREAT-PLAINS", "spatial resolution", "HIGH-RESOLUTION", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2016RG000543"}, {"href": "https://doi.org/1854/LU-8528923"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Reviews%20of%20Geophysics", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "1854/LU-8528923", "name": "item", "description": "1854/LU-8528923", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/1854/LU-8528923"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-04-18T00:00:00Z"}}, {"id": "1893/33794", "type": "Feature", "geometry": null, "properties": {"updated": "2026-08-25T16:22:25Z", "type": "Journal Article", "created": "2021-12-30", "title": "Global maps of soil temperature", "description": "Abstract<p>Research in global change ecology relies heavily on global climatic grids derived from estimates of air temperature in open areas at around 2\uffc2\uffa0m above the ground. These climatic grids do not reflect conditions below vegetation canopies and near the ground surface, where critical ecosystem functions occur and most terrestrial species reside. Here, we provide global maps of soil temperature and bioclimatic variables at a 1\uffe2\uff80\uff90km2resolution for 0\uffe2\uff80\uff935 and 5\uffe2\uff80\uff9315\uffc2\uffa0cm soil depth. These maps were created by calculating the difference (i.e. offset) between in situ soil temperature measurements, based on time series from over 1200 1\uffe2\uff80\uff90km2pixels (summarized from 8519 unique temperature sensors) across all the world's major terrestrial biomes, and coarse\uffe2\uff80\uff90grained air temperature estimates from ERA5\uffe2\uff80\uff90Land (an atmospheric reanalysis by the European Centre for Medium\uffe2\uff80\uff90Range Weather Forecasts). We show that mean annual soil temperature differs markedly from the corresponding gridded air temperature, by up to 10\uffc2\uffb0C (mean\uffc2\uffa0=\uffc2\uffa03.0\uffc2\uffa0\uffc2\uffb1\uffc2\uffa02.1\uffc2\uffb0C), with substantial variation across biomes and seasons. Over the year, soils in cold and/or dry biomes are substantially warmer (+3.6\uffc2\uffa0\uffc2\uffb1\uffc2\uffa02.3\uffc2\uffb0C) than gridded air temperature, whereas soils in warm and humid environments are on average slightly cooler (\uffe2\uff88\uff920.7\uffc2\uffa0\uffc2\uffb1\uffc2\uffa02.3\uffc2\uffb0C). The observed substantial and biome\uffe2\uff80\uff90specific offsets emphasize that the projected impacts of climate and climate change on near\uffe2\uff80\uff90surface biodiversity and ecosystem functioning are inaccurately assessed when air rather than soil temperature is used, especially in cold environments. The global soil\uffe2\uff80\uff90related bioclimatic variables provided here are an important step forward for any application in ecology and related disciplines. Nevertheless, we highlight the need to fill remaining geographic gaps by collecting more in situ measurements of microclimate conditions to further enhance the spatiotemporal resolution of global soil temperature products for ecological applications.</p", "keywords": ["0106 biological sciences", "Bioclimatic variables; Global maps; Microclimate; Near-surface temperatures; Soil temperature; Soil-dwelling organisms; Temperature offset; Weather stations; Climate change; Temperature; Ecosystem; Soil", "791", "550", ":Zoology and botany: 480 [VDP]", "VDP::Zoologiske og botaniske fag: 480", "551", "Q1", "7. Clean energy", "01 natural sciences", "41 Environmental sciences", "Global map", "SDG 13 - Climate Action", "Soil temperature", "MICROCLIMATE", "bepress|Physical Sciences and Mathematics|Environmental Sciences", "soil-dwelling organism", "bioclimatic variables; global maps; microclimate; near-surface temperatures; soil temperature; soil-dwelling organisms; temperature offset; weather stations", "weather station", "GB", "http://aims.fao.org/aos/agrovoc/c_34836", "Geology", "16. Peace & justice", "Settore BIOS-01/C - Botanica ambientale e applicata", "6. Clean water", "Near-surface soil temperature", "international", "[SDE]Environmental Sciences", "551: Geologie und Hydrologie", "Near-surface temperature", "Near-surface temperatures", "soil temperature", "P40 - M\u00e9t\u00e9orologie et climatologie", "577", "bepress|Physical Sciences and Mathematics|Earth Sciences", "MITIGATION", "bepress|Life Sciences|Ecology and Evolutionary Biology", "12. Responsible consumption", "near-surface temperatures", "bepress|Physical Sciences and Mathematics|Oceanography and Atmospheric Sciences and Meteorology|Climate", "bioclimatic variables", "Bioclimatic variables", "Settore BIO/07 - ECOLOGIA", "temperature offset", "global maps", "http://aims.fao.org/aos/agrovoc/c_1344", "577: \u00d6kologie", "global map", "Biology", "Ecosystem", "Ekologi", "http://aims.fao.org/aos/agrovoc/c_24894", "Science & Technology", "ddc:550", "9. Industry and infrastructure", "31 Biological sciences", "Biology and Life Sciences", "Microclimate", "06 Biological Sciences", "15. Life on land", "weather stations", "bepress|Physical Sciences and Mathematics|Environmental Sciences|Environmental Monitoring", "900", "cartographie", "microclimate", "Klimatvetenskap", "[SDE] Environmental Sciences", "Biodiversity & Conservation", "05 Environmental Sciences", "Weather stations", "Temperature offset", "Plan_S-Compliant-OA", "Soil", "bepress|Life Sciences", "Geolog\u00eda", "Research Articles", "info:eu-repo/classification/ddc/570", "changement climatique", "Ecology", "zone climatique", "4. Education", "Temperature", "Biological Sciences", "bioclimatologie", "FOREST", "Weather station", "Chemistry", "Biodiversity Conservation", "Life Sciences & Biomedicine", "bepress|Physical Sciences and Mathematics", "Technology and Engineering", "http://aims.fao.org/aos/agrovoc/c_1669", "bioclimatic variable", "Climate Change", "soil-dwelling organisms", "Environmental Sciences & Ecology", "MOISTURE", "LITTER DECOMPOSITION", "PERMAFROST", "near-surface temperature", "temp\u00e9rature du sol", "bepress|Physical Sciences and Mathematics|Oceanography and Atmospheric Sciences and Meteorology", "SUITABILITY", "G1", "VDP::Mathematics and natural scienses: 400::Zoology and botany: 480", "Global maps", "http://aims.fao.org/aos/agrovoc/c_1666", ":Zoologiske og botaniske fag: 480 [VDP]", "Soil-dwelling organisms", "0105 earth and related environmental sciences", "info:eu-repo/classification/ddc/550", "r\u00e9chauffement global", "Climate Change; Ecosystem; Microclimate; Soil; Temperature; bioclimatic variables; global maps; microclimate; near-surface temperatures; soil temperature; soil-dwelling organisms; temperature offset; weather stations", "http://aims.fao.org/aos/agrovoc/c_9260", "P30 - Sciences et am\u00e9nagement du sol", "Aquatic Ecology", "Bioclimatic variable", "SNOW-COVER", "Climate Science", "37 Earth sciences", "Climate Action", "bepress|Physical Sciences and Mathematics|Earth Sciences|Soil Science", "[SDE.BE] Environmental Sciences/Biodiversity and Ecology", "Earth sciences", "variation saisonni\u00e8re", "PLANT-RESPONSES", "CLIMATIC CONTROLS", "Soil-dwelling organism", "Settore BIOS-05/A - Ecologia", "13. Climate action", "Earth and Environmental Sciences", "VDP::Matematikk og naturvitenskap: 400::Zoologiske og botaniske fag: 480", "VDP::Zoology and botany: 480", "[SDE.BE]Environmental Sciences/Biodiversity and Ecology", "CBCE", "http://aims.fao.org/aos/agrovoc/c_7197", "Environmental Sciences"]}, "links": [{"href": "https://ray.yorksj.ac.uk/id/eprint/5803/1/20211222_SoilTemp_maps_preformatted.pdf"}, {"href": "http://dspace.stir.ac.uk/bitstream/1893/33794/1/Lembrechts-etal-GCB-2022.pdf"}, {"href": "https://eprints.whiterose.ac.uk/183991/1/Global%20Change%20Biology%20-%202022%20-%20Lembrechts%20-%20Global%20maps%20of%20soil%20temperature.pdf"}, {"href": "https://iris.cnr.it/bitstream/20.500.14243/445619/1/prod_462419-doc_189996.pdf"}, {"href": "https://openpub.fmach.it/bitstream/10449/74200/1/Global%20Change%20Biology%20-%202022%20-%20Lembrechts%20-%20Global%20maps%20of%20soil%20temperature.pdf"}, {"href": "https://iris.unica.it/bitstream/11584/332967/1/2022_Global_maps_soil_temperature_GlobalChangeBiology.pdf"}, {"href": "https://ricerca.univaq.it/bitstream/11697/178559/2/Global%20Change%20Biology%20-%202022%20-%20Lembrechts%20-%20Global%20maps%20of%20soil%20temperature.pdf"}, {"href": "https://vb.gamtc.lt/object/elaba:126634244/126634244.pdf"}, {"href": "https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.16060"}, {"href": "https://escholarship.org/content/qt6hg3313z/qt6hg3313z.pdf"}, {"href": "https://doi.org/1893/33794"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Global%20Change%20Biology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "1893/33794", "name": "item", "description": "1893/33794", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/1893/33794"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-03-21T00:00:00Z"}}, {"id": "1912/29772", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-08-25T16:22:26Z", "type": "Journal Article", "created": "2021-11-08", "title": "Radium inputs into the Arctic Ocean from rivers: a basin-wide estimate", "description": "Abstract<p>Radium isotopes have been used to trace nutrient, carbon, and trace metal fluxes inputs from ocean margins. However, these approaches require a full accounting of radium sources to the coastal ocean including rivers. Here, we aim to quantify river radium inputs into the Arctic Ocean for the first time for 226Ra and to refine the estimates for 228Ra. Using new and existing data, we find that the estimated combined (dissolved plus desorbed) annual 226Ra and 228Ra fluxes to the Arctic Ocean are [7.0\uffe2\uff80\uff939.4] \uffc3\uff97 1014 dpm y\uffe2\uff88\uff921 and [15\uffe2\uff80\uff9318] \uffc3\uff97 1014 dpm y\uffe2\uff88\uff921, respectively. Of these totals, 44% and 60% of the river 226Ra and 228Ra, respectively are from suspended sediment desorption, which were estimated from laboratory incubation experiments. Using Ra isotope data from 20 major rivers around the world, we derived global annual 226Ra and 228Ra fluxes of [7.4\uffe2\uff80\uff9317] \uffc3\uff97 1015 and [15\uffe2\uff80\uff9327] \uffc3\uff97 1015 dpm y\uffe2\uff88\uff921, respectively. As climate change spurs rapid Arctic warming, hydrological cycles are intensifying and coastal ice cover and permafrost are diminishing. These river radium inputs to the Arctic Ocean will serve as a valuable baseline as we attempt to understand the changes that warming temperatures are having on fluxes of biogeochemically important elements to the Arctic coastal zone.</p", "keywords": ["550", "Radium isotopes", "F700", "15. Life on land", "551", "01 natural sciences", "river fluxes", "River fluxes", "radium isotopes", "13. Climate action", "Arctic Ocean", "SDG 14 - Life Below Water", "14. Life underwater", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://nrl.northumbria.ac.uk/id/eprint/50000/9/JGR%20Oceans%20-%202022%20-%20Bullock%20-%20Radium%20Inputs%20Into%20the%20Arctic%20Ocean%20From%20Rivers%20%20A%20Basin%E2%80%90Wide%20Estimate.pdf"}, {"href": "https://doi.org/1912/29772"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Goldschmidt2021%20abstracts", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "1912/29772", "name": "item", "description": "1912/29772", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/1912/29772"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-01-01T00:00:00Z"}}, {"id": "1959.7/uws:77264", "type": "Feature", "geometry": null, "properties": {"updated": "2026-08-25T16:22:28Z", "type": "Journal Article", "created": "2024-06-07", "title": "Increasing numbers of global change stressors reduce soil carbon worldwide", "description": "Open AccessF.T.M. was supported by European Research Council grant number 647038 (BIODESERT), Generalitat Valenciana grant number CIDEGENT/2018/041, by the Spanish Ministry of Science and Innovation (grant numbers EUR2022-134048 and PID2020-116578RB-I00) and by the contract between ETH Zurich and University of Alicante \u201cMapping terrestrial ecosystem structure at the global scale\u201d. E.G. acknowledges funding from Generalitat Valenciana and Europen Social Fund (grant number APOSTD/2021/188). F.T.M. also acknowledges support from the King Abdullah University of Science and Technology (KAUST) and the KAUST Climate and Livability Initiative. T.S.-S., A.G. and M.D.-B. are supported by grant number TED2021-130908B-C41 (URBANCHANGE). M.D.-B. was also supported by the European Research Council (ERC) grant number 647038 (BIODESERT), BES grant agreement number LRB17 1019 (MUSGONET), the innovation programme under Marie Sklodowska-Curie grant agreement number 702057 (CLIMIFUN), Ram\u00f3n y Cajal grant number RYC2018-025483-I, a project from the Spanish Ministry of Science and Innovation (grant number PID2020-115813RA-I00; SOIL4GROWTH) and project PAIDI 2020 from the Junta de Andaluc\u00eda (grant number P20_00879). C.W.M. acknowledges funding for the research provided by the NSF Postdoctoral Fellowship in Polar Regions Research (grant number 0852036), the German Science Foundation (DFG) for financial support in the frame of the \u201cInitiation of International Collaboration\u201d (grant number MU 3021/2-1) and funding within the DFG Priority Programme 1158 \u201cAntarctic Research with Comparable Investigations in Arctic Sea Ice Areas\u201d (grant number MU 3021/8-1). M.B. acknowledges funding from Spanish Ministry of Science and Innovation through a Ram\u00f3n y Cajal Fellowship (# RYC2021-031797-I).", "keywords": ["Ecolog\u00eda (Biolog\u00eda)", "550", "Global change stressors", "2410.05 Ecolog\u00eda Humana", "Climate-change ecology", "500", "551.588.7", "Edafolog\u00eda (Biolog\u00eda)", "Soil carbon", "631.4", "2511 Ciencias del Suelo (Edafolog\u00eda)", "Climate change", "2511.02 Biolog\u00eda de Suelos", "310308 - Terrestrial ecology", "502.1"]}, "links": [{"href": "https://doi.org/1959.7/uws:77264"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Nature%20Climate%20Change", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "1959.7/uws:77264", "name": "item", "description": "1959.7/uws:77264", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/1959.7/uws:77264"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-06-07T00:00:00Z"}}, {"id": "1983/38cb9066-8784-4005-9693-98996b291220", "type": "Feature", "geometry": null, "properties": {"updated": "2026-08-25T16:22:28Z", "type": "Journal Article", "created": "2021-03-12", "title": "Editorial: Novel Isotope Systems and Biogeochemical Cycling During Cryospheric Weathering in Polar Environments", "description": "Cryospheric weathering processes in permafrost and glaciated environments play an essential role in carbon cycling within the Earth system. Chemical weathering of silicate, carbonate and sulfidebearing rocks releases cations and anions that can consume (or release) atmospheric carbon dioxide (CO2), as well as biologically important nutrients such as phosphorous, iron and silicon, which can impact downstream ecosystems (Figure 1). How these cryospheric weathering processes will respond to future climate-driven changes in permafrost thaw and glacial melt is difficult to predict due to the role of complex forcing mechanisms and feedbacks. Isotope geochemistry utilizes changes in the relative abundance of different isotopes due to physical, chemical and biological reactions, allowing some of the complexities of cryospheric weathering processes to be unpicked. In recent years, there has been an explosion in the range of stable and radiogenic isotope systems used for the study of high-latitude environments, including isotopes of major elements such as carbon, oxygen, and silicon (e.g., Opfergelt et al., 2013; Kutscher et al., 2017), and trace metal isotopes such as strontium (Hindshaw et al., 2014), lithium (Murphy et al., 2019), iron (Zhang et al., 2015), uranium-series (e.g., Arendt et al., 2018) and rare earth elements (e.g., Clinger et al., 2016). This research topic explores some of the developments in high-latitude field and experimental studies that utilize such geochemical tools to trace the degree and nature of weathering reactions that play a critical role in carbon cycling. The nine contributions to the research topic involve the analysis of traditional (C, N, S, O) and non-traditional (Mg, Li, Si, Ge) isotopes from different samples types such as river waters, lake waters, rocks, sediments, or mineral separates from locations both in the Northern (Greenland, Iceland, Canada, Svalbard) and Southern Hemisphere (Patagonia, Antarctica). Two papers use isotope geochemistry to explore organic and inorganic carbon cycling within permafrost and active layer soils. Jones et al. show that biogeochemical processes and decomposition pathways of organic carbon in ice-wedge polygons in Svalbard are dependent upon water and organic carbon content. Sulfur (\u03b434S) and oxygen (\u03b418O) isotopes show that iron and sulfate reduction processes dominate in water saturated, high organic carbon environments, whereas sulfide oxidation dominates in drier areas with less organic carbon. Zolkos and Tank use an experimental approach in combination with stable carbon isotopes (\u03b413CO2) to show that carbonate weathering coupled with sulfide oxidation in recently or previously unthawed Canadian permafrost sediments is a net source of inorganic CO2 to the atmosphere, albeit partly counterbalanced by carbonate buffering.", "keywords": ["glacier", "550", "Science", "Q", "551", "cryosphere", "01 natural sciences", "7. Clean energy", "13. Climate action", "14. Life underwater", "isotope", "permafrost", "geochemistry", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/1983/38cb9066-8784-4005-9693-98996b291220"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Frontiers%20in%20Earth%20Science", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "1983/38cb9066-8784-4005-9693-98996b291220", "name": "item", "description": "1983/38cb9066-8784-4005-9693-98996b291220", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/1983/38cb9066-8784-4005-9693-98996b291220"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-03-11T00:00:00Z"}}, {"id": "1983/a9ecd79e-9249-4f29-b8fd-05f3f4442b8c", "type": "Feature", "geometry": null, "properties": {"updated": "2026-08-25T16:22:28Z", "type": "Journal Article", "created": "2020-06-26", "title": "Silicon Isotopes Reveal a Non-glacial Source of Silicon to Crescent Stream, McMurdo Dry Valleys, Antarctica", "description": "In high latitude environments, silicon is supplied to river waters by both glacial and non-glacial chemical weathering. The signal of these two end-members is often obscured by biological uptake and/or groundwater input in the river catchment. McMurdo Dry Valleys streams in Antarctica have no deep groundwater input, no connectivity between streams and no surface vegetation cover, and thus provide a simplified system for us to constrain the supply of dissolved silicon (DSi) to rivers from chemical weathering in a glacial environment. Here we report dissolved Si concentrations, germanium/silicon ratios (Ge/Si) and silicon isotope compositions (\u03b430SiDSi) in Crescent Stream, McMurdo Dry Valleys for samples collected between December and February in the 2014\u22122015, 2015\u22122016, and 2016\u22122017 austral seasons. The \u03b430SiDSi compositions and DSi concentrations are higher than values reported in wet-based glacial meltwaters, and form a narrow cluster within the range of values reported for permafrost dominated Arctic Rivers. High \u03b430SiDSi compositions, ranging from +0.90\u2030 to +1.39\u2030, are attributed to (i) the precipitation of amorphous silica during freezing of waters in isolated pockets of the hyporheic zone in the winter and the release of Si from unfrozen pockets during meltwater-hyporheic zone exchange in the austral summer, and (ii) additional Si isotope fractionation via long-term Si uptake in clay minerals and seasonal Si uptake into diatoms superimposed on this winter-derived isotope signal. There is no relationship between \u03b430SiDSi compositions and DSi concentrations with seasonal and daily discharge, showing that stream waters contain DSi that is in equilibrium with the formation of secondary Si minerals in the hyporheic zone. We show that \u03b430SiDSi compositions can be used as tracers of silicate weathering in the hyporheic zone and possible tracers of freeze-thaw conditions in the hyporheic zone. This is important in the context of the ongoing warming in McMurdo Dry Valleys and the supply of more meltwaters to the hyporheic zone of McMurdo Dry Valley streams.", "keywords": ["550", "Science", "Q", "silicon", "Antartica", "15. Life on land", "551", "01 natural sciences", "hyporheic zone", "silicon isotopes", "13. Climate action", "weathering", "Antarctica", "isotopes", "permafrost", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/1983/a9ecd79e-9249-4f29-b8fd-05f3f4442b8c"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Frontiers%20in%20Earth%20Science", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "1983/a9ecd79e-9249-4f29-b8fd-05f3f4442b8c", "name": "item", "description": "1983/a9ecd79e-9249-4f29-b8fd-05f3f4442b8c", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/1983/a9ecd79e-9249-4f29-b8fd-05f3f4442b8c"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2020-06-26T00:00:00Z"}}, {"id": "1983/b92f4977-b482-4b57-9710-09413462ccde", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-08-25T16:22:28Z", "type": "Journal Article", "created": "2020-09-02", "title": "Assessing the Potential for Mobilization of Old Soil Carbon After Permafrost Thaw: A Synthesis of 14C Measurements From the Northern Permafrost Region", "description": "Abstract<p>The magnitude of future emissions of greenhouse gases from the northern permafrost region depends crucially on the mineralization of soil organic carbon (SOC) that has accumulated over millennia in these perennially frozen soils. Many recent studies have used radiocarbon (14C) to quantify the release of this \uffe2\uff80\uff9cold\uffe2\uff80\uff9d SOC as CO2 or CH4 to the atmosphere or as dissolved and particulate organic carbon (DOC and POC) to surface waters. We compiled ~1,900 14C measurements from 51 sites in the northern permafrost region to assess the vulnerability of thawing SOC in tundra, forest, peatland, lake, and river ecosystems. We found that growing season soil 14C\uffe2\uff80\uff90CO2 emissions generally had a modern (post\uffe2\uff80\uff901950s) signature, but that well\uffe2\uff80\uff90drained, oxic soils had increased CO2 emissions derived from older sources following recent thaw. The age of CO2 and CH4 emitted from lakes depended primarily on the age and quantity of SOC in sediments and on the mode of emission, and indicated substantial losses of previously frozen SOC from actively expanding thermokarst lakes. Increased fluvial export of aged DOC and POC occurred from sites where permafrost thaw caused soil thermal erosion. There was limited evidence supporting release of previously frozen SOC as CO2, CH4, and DOC from thawing peatlands with anoxic soils. This synthesis thus suggests widespread but not universal release of permafrost SOC following thaw. We show that different definitions of \uffe2\uff80\uff9cold\uffe2\uff80\uff9d sources among studies hamper the comparison of vulnerability of permafrost SOC across ecosystems and disturbances. We also highlight opportunities for future 14C studies in the permafrost region.</p", "keywords": ["[SDE] Environmental Sciences", "particulate organic carbon", "0301 basic medicine", "550", "permafrost thaw", "methane", "500", "carbon dioxide", "15. Life on land", "551", "dissolved organic carbon", "01 natural sciences", "[SDE.MCG] Environmental Sciences/Global Changes", "03 medical and health sciences", "13. Climate action", "ddc:551.9", "radiocarbon", "0105 earth and related environmental sciences"]}, "links": [{"href": "http://livrepository.liverpool.ac.uk/3106184/1/2020%20Estop%E2%80%90Aragon%C3%A9s%20et%20al%2C%20GBC%20-%20Arctic%2014C%20synthesis.pdf"}, {"href": "https://eprints.gla.ac.uk/222767/13/222767.pdf"}, {"href": "https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2020GB006672"}, {"href": "https://doi.org/1983/b92f4977-b482-4b57-9710-09413462ccde"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Global%20Biogeochemical%20Cycles", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "1983/b92f4977-b482-4b57-9710-09413462ccde", "name": "item", "description": "1983/b92f4977-b482-4b57-9710-09413462ccde", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/1983/b92f4977-b482-4b57-9710-09413462ccde"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2020-09-01T00:00:00Z"}}, {"id": "20.500.11850/631341", "type": "Feature", "geometry": null, "properties": {"updated": "2026-08-25T16:22:33Z", "type": "Journal Article", "created": "2023-09-08", "title": "Upper Bounds of Maximum Land Surface Temperatures in a Warming Climate and Limits to Plant Growth", "description": "Abstract<p>Extremely high land surface temperatures affect soil ecological processes, alter land\uffe2\uff80\uff90atmosphere interactions, and may limit some forms of life. Extreme surface temperature hotspots are presently identified using satellite observations or deduced from complex Earth system models. We introduce a simple, yet physically based analytical approach that incorporates salient land characteristics and atmospheric conditions to globally identify locations of extreme surface temperatures and their upper bounds. We then provide a predictive tool for delineating the spatial extent of land hotspots at the limits to biological adaptability. The model is in good agreement with satellite observations showing that temperature hotspots are associated with high radiation and low wind speed and occur primarily in Middle East and North Africa, with maximum temperatures exceeding 85\uffc2\uffb0C during the study period from 2005 to 2020. We observed an increasing trend in maximum surface temperatures at a rate of 0.17\uffc2\uffb0C/decade. The model allows quantifying how upper bounds of extreme temperatures can increase in a warming climate in the future for which we do not have satellite observations and offers new insights on potential impacts of future warming on limits to plant growth and biological adaptability.</p", "keywords": ["0301 basic medicine", "Ecology", "LST hotspots", "maximum land surface temperature (LST)", "15. Life on land", "01 natural sciences", "Environmental sciences", "atmospheric conditions", "03 medical and health sciences", "ddc:551.5", "land conditions", "13. Climate action", "GE1-350", "QH540-549.5", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/20.500.11850/631341"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Earth%27s%20Future", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "20.500.11850/631341", "name": "item", "description": "20.500.11850/631341", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/20.500.11850/631341"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2023-09-01T00:00:00Z"}}, {"id": "2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/292778", "type": "Feature", "geometry": null, "properties": {"updated": "2026-08-25T16:22:37Z", "type": "Journal Article", "created": "2019-08-12", "title": "ORCHIDEE MICT-LEAK (r5459), a global model for the production, transport, and transformation of dissolved organic carbon from Arctic permafrost regions \u2013 Part 1: Rationale, model description, and simulation protocol", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Abstract. Few Earth system models adequately represent the unique permafrost soil biogeochemistry and its respective processes; this significantly contributes to uncertainty in estimating their responses, and that of the planet at large, to warming. Likewise, the riverine component of what is known as the \u201cboundless carbon cycle\u201d is seldom recognised in Earth system modelling. The hydrological mobilisation of organic material from a \u223c1330\u20131580\u2009PgC carbon stock to the river network results in either sedimentary settling or atmospheric \u201cevasion\u201d, processes widely expected to increase with amplified Arctic climate warming. Here, the production, transport, and atmospheric release of dissolved organic carbon (DOC) from high-latitude permafrost soils into inland waters and the ocean are explicitly represented for the first time in the land surface component (ORCHIDEE) of a CMIP6 global climate model (Institut Pierre Simon Laplace \u2013 IPSL). The model, ORCHIDEE MICT-LEAK, which represents the merger of previously described ORCHIDEE versions MICT and LEAK, mechanistically represents (a)\u00a0vegetation and soil physical processes for high-latitude snow, ice, and soil phenomena and (b)\u00a0the cycling of DOC and CO2, including atmospheric evasion, along the terrestrial\u2013aquatic continuum from soils through the river network to the coast at 0.5 to 2\u2218 resolution. This paper, the first in a two-part study, presents the rationale for including these processes in a high-latitude-specific land surface model, then describes the model with a focus on novel process implementations, followed by a summary of the model configuration and simulation protocol. The results of these simulation runs, conducted for the Lena River basin, are evaluated against observational data in the second part of this study.</p></article>", "keywords": ["QE1-996.5", "550", "Geology", "15. Life on land", "551", "01 natural sciences", "6. Clean water", "Sciences de la terre et du cosmos", "[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry", "13. Climate action", "[SDU.STU.GC] Sciences of the Universe [physics]/Earth Sciences/Geochemistry", "[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology", "Sciences pharmaceutiques", "[SDU.STU.GL] Sciences of the Universe [physics]/Earth Sciences/Glaciology", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://dipot.ulb.ac.be/dspace/bitstream/2013/292778/1/doi_276405.pdf"}, {"href": "https://doi.org/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/292778"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Geoscientific%20Model%20Development", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/292778", "name": "item", "description": "2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/292778", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/292778"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-03-25T00:00:00Z"}}, {"id": "21.11116/0000-000A-E334-B", "type": "Feature", "geometry": null, "properties": {"updated": "2026-08-25T16:22:39Z", "type": "Journal Article", "created": "2022-08-17", "title": "Lowering water table reduces carbon sink strength and carbon stocks in northern peatlands", "description": "Abstract<p>Peatlands at high latitudes have accumulated &gt;400\uffe2\uff80\uff89Pg carbon (C) because saturated soil and cold temperatures suppress C decomposition. This substantial amount of C in Arctic and Boreal peatlands is potentially subject to increased decomposition if the water table (WT) decreases due to climate change, including permafrost thaw\uffe2\uff80\uff90related drying. Here, we optimize a version of the Organizing Carbon and Hydrology In Dynamic Ecosystems model (ORCHIDEE\uffe2\uff80\uff90PCH4) using site\uffe2\uff80\uff90specific observations to investigate changes in CO2 and CH4 fluxes as well as C stock responses to an experimentally manipulated decrease of WT at six northern peatlands. The unmanipulated control peatlands, with the WT &lt;20\uffe2\uff80\uff89cm on average (seasonal max up to 45\uffe2\uff80\uff89cm) below the surface, currently act as C sinks in most years (58\uffe2\uff80\uff89\uffc2\uffb1\uffe2\uff80\uff8934\uffe2\uff80\uff89g C\uffe2\uff80\uff89m\uffe2\uff88\uff922\uffc2\uffa0year\uffe2\uff88\uff921; including 6\uffe2\uff80\uff89\uffc2\uffb1\uffe2\uff80\uff897\uffe2\uff80\uff89g C\uffe2\uff80\uff93CH4 m\uffe2\uff88\uff922\uffc2\uffa0year\uffe2\uff88\uff921 emission). We found, however, that lowering the WT by 10\uffe2\uff80\uff89cm reduced the CO2 sink by 13\uffe2\uff80\uff89\uffc2\uffb1\uffe2\uff80\uff8915\uffe2\uff80\uff89g\uffe2\uff80\uff89C\uffe2\uff80\uff89m\uffe2\uff88\uff922\uffc2\uffa0year\uffe2\uff88\uff921 and decreased CH4 emission by 4\uffe2\uff80\uff89\uffc2\uffb1\uffe2\uff80\uff894\uffe2\uff80\uff89g CH4 m\uffe2\uff88\uff922\uffc2\uffa0year\uffe2\uff88\uff921, thus accumulating less C over 100\uffe2\uff80\uff89years (0.2\uffe2\uff80\uff89\uffc2\uffb1\uffe2\uff80\uff890.2\uffe2\uff80\uff89kg\uffe2\uff80\uff89C\uffe2\uff80\uff89m\uffe2\uff88\uff922). Yet, the reduced emission of CH4, which has a larger greenhouse warming potential, resulted in a net decrease in greenhouse gas balance by 310\uffe2\uff80\uff89\uffc2\uffb1\uffe2\uff80\uff89360\uffe2\uff80\uff89g\uffe2\uff80\uff89CO2\uffe2\uff80\uff90eq\uffc2\uffa0m\uffe2\uff88\uff922\uffc2\uffa0year\uffe2\uff88\uff921. Peatlands with the initial WT close to the soil surface were more vulnerable to C loss: Non\uffe2\uff80\uff90permafrost peatlands lost &gt;2\uffe2\uff80\uff89kg\uffe2\uff80\uff89C\uffe2\uff80\uff89m\uffe2\uff88\uff922 over 100\uffe2\uff80\uff89years when WT is lowered by 50\uffe2\uff80\uff89cm, while permafrost peatlands temporally switched from C sinks to sources. These results highlight that reductions in C storage capacity in response to drying of northern peatlands are offset in part by reduced CH4 emissions, thus slightly reducing the positive carbon climate feedbacks of peatlands under a warmer and drier future climate scenario.</p", "keywords": ["570", "Carbon Sequestration", "permafrost thaw", "land surface model", "551", "01 natural sciences", "manipulation experiment", "Greenhouse Gases", "Soil", "Groundwater", "Research Articles", "Ecosystem", "0105 earth and related environmental sciences", "[SDU.OCEAN]Sciences of the Universe [physics]/Ocean", "Atmosphere", "[SDU.OCEAN] Sciences of the Universe [physics]/Ocean", " Atmosphere", "carbon stock", "high latitude", "Carbon Dioxide", "15. Life on land", "[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces", " environment", "Carbon", "carbon flux", "13. Climate action", "[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces", "environment", "Methane", "drainage"]}, "links": [{"href": "https://eprints.whiterose.ac.uk/190653/1/Global%20Change%20Biology%20-%202022%20-%20Kwon%20-%20Lowering%20water%20table%20reduces%20carbon%20sink%20strength%20and%20carbon%20stocks%20in%20northern.pdf"}, {"href": "https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.16394"}, {"href": "https://doi.org/21.11116/0000-000A-E334-B"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Global%20Change%20Biology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "21.11116/0000-000A-E334-B", "name": "item", "description": "21.11116/0000-000A-E334-B", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/21.11116/0000-000A-E334-B"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-08-30T00:00:00Z"}}, {"id": "2078.1/293942", "type": "Feature", "geometry": null, "properties": {"updated": "2026-08-25T16:22:38Z", "type": "Journal Article", "created": "2024-09-09", "title": "Rainfall Impacts Dissolved Organic Matter and Cation Export From Permafrost Catchments and a Glacial River During Late Summer in Northeast Greenland", "description": "ABSTRACT<p>Ongoing and amplified climate change in the Arctic is leading to glacier retreat and to the exposure of an ever\uffe2\uff80\uff90larger portion of non\uffe2\uff80\uff90glaciated permafrost\uffe2\uff80\uff90dominated landscapes. Warming will also cause more precipitation to fall as rain, further enhancing the thaw of previously frozen ground. Yet, the impact of those perturbations on the geochemistry of Arctic rivers remains a subject of debate. Here, we determined the geochemical composition of waters from various contrasting non\uffe2\uff80\uff90glacial permafrost catchments and investigated their impact on a glacially dominated river, the Zackenberg River (Northeast Greenland), during late summer (August 2019). We also studied the effect of rainfall on the geochemistry of the Zackenberg River, its non\uffe2\uff80\uff90glacial tributaries, and a nearby independent non\uffe2\uff80\uff90glacial headwater stream Gr\uffc3\uffa6nse. We analyzed water properties, quantified and characterized dissolved organic matter (DOM) using absorbance and fluorescence spectroscopy and radiocarbon isotopes, and set this alongside analyses of the major cations (Ca, Mg, Na, and K), dissolved silicon (Si), and germanium/silicon ratios (Ge/Si). The glacier\uffe2\uff80\uff90fed Zackenberg River contained low concentrations of major cations, dissolved Si and dissolved organic carbon (DOC), and a Ge/Si ratio typical of bulk rock. Glacial DOM was enriched in protein\uffe2\uff80\uff90like fluorescent DOM and displayed relatively depleted radiocarbon values (i.e., old DOM). Non\uffe2\uff80\uff90glacial streams (i.e., tributaries and Gr\uffc3\uffa6nse) had higher concentrations of major cations and DOC and DOM enriched in aromatic compounds. They showed a wide range of values for radiocarbon, Si and Ge/Si ratios associated with variable contributions of surface runoff relative to deep active layer leaching. Before the rain event, Zackenberg tributaries did not contribute notably to the solute export of the Zackenberg River, and supra\uffe2\uff80\uff90permafrost ground waters governed the supply of solutes in Zackenberg tributaries and Gr\uffc3\uffa6nse stream. After the rain event, surface runoff modified the composition of Gr\uffc3\uffa6nse stream, and non\uffe2\uff80\uff90glacial tributaries strongly increased their contribution to the Zackenberg River solute export. Our results show that summer rainfall events provide an additional source of DOM and Si\uffe2\uff80\uff90rich waters from permafrost\uffe2\uff80\uff90underlain catchments to the discharge of glacially dominated rivers. This suggests that the magnitude and composition of solute exports from Arctic rivers are modulated by permafrost thaw and summer rain events. This event\uffe2\uff80\uff90driven solute supply will likely impact the carbon cycle in rivers, estuaries, and oceans and should be included into future predictions of carbon balance in these vulnerable Arctic systems.</p", "keywords": ["[SDV] Life Sciences [q-bio]", "550", "[SDV]Life Sciences [q-bio]", "supra-permafrost groundwater", "Zackenberg", "dissolved silicon", "dissolved organic matter", "551", "PARAFAC"]}, "links": [{"href": "https://doi.org/2078.1/293942"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Permafrost%20and%20Periglacial%20Processes", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "2078.1/293942", "name": "item", "description": "2078.1/293942", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/2078.1/293942"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-09-09T00:00:00Z"}}, {"id": "2164/10082", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-08-25T16:22:41Z", "type": "Journal Article", "created": "2018-02-15", "title": "Rhizosphere\u2010Scale Quantification of Hydraulic and Mechanical Properties of Soil Impacted by Root and Seed Exudates", "description": "Core Ideas                     <p>                                                                           <p>We hypothesized that plant exudates gel soil particles and on drying enhance water repellency.</p>                                                                             <p>This has been carried out using rhizosphere\uffe2\uff80\uff90scale mechanical and hydraulic measurements.</p>                                                                             <p>Plant exudates enhanced soil hardness and modulus of elasticity as chia seed &gt; maize root &gt; barley root.</p>                                                                             <p>Plant exudates caused measureable decreases in soil wetting rates through water repellency.</p>                                                                     </p>                     <p>                       Using rhizosphere\uffe2\uff80\uff90scale physical measurements, we tested the hypothesis that plant exudates gel together soil particles and, on drying, enhance soil water repellency. Barley (                       Hordeum vulgare                       L. cv. Optic) and maize (                       Zea mays                       L. cv. Freya) root exudates were compared with chia (                       Salvia hispanica                       L.) seed exudate, a commonly used root exudate analog. Sandy loam and clay loam soils were treated with root exudates at 0.46 and 4.6 mg exudate g                       \uffe2\uff88\uff921                       dry soil and chia seed exudate at 0.046, 0.46, 0.92, 2.3 and 4.6 mg exudate g                       \uffe2\uff88\uff921                       dry soil. Soil hardness and modulus of elasticity were measured at \uffe2\uff88\uff9210 kPa matric potential using a 3\uffe2\uff80\uff90mm\uffe2\uff80\uff90diameter spherical indenter. The water sorptivity and repellency index of air\uffe2\uff80\uff90dry soil were measured using a miniaturized infiltrometer device with a 1\uffe2\uff80\uff90mm tip radius. Soil hardness increased by 28% for barley root exudate, 62% for maize root exudate, and 86% for chia seed exudate at 4.6 mg g                       \uffe2\uff88\uff921                       concentration in the sandy loam soil. For the clay loam soil, root exudates did not affect soil hardness, whereas chia seed exudate increased soil hardness by 48% at 4.6 mg g                       \uffe2\uff88\uff921                       concentration. Soil water repellency increased by 48% for chia seed exudate and 23% for maize root exudate but not for barley root exudate at 4.6 mg g                       \uffe2\uff88\uff921                       concentration in the sandy loam soil. For the clay loam soil, chia seed exudate increased water repellency by 45%, whereas root exudates did not affect water repellency at 4.6 mg g                       \uffe2\uff88\uff921                       concentration. Water sorptivity and repellency were both correlated with hardness, presumably due to the combined influence of exudates on the hydrological and mechanical properties of the soils.                     </p>", "keywords": ["/dk/atira/pure/subjectarea/asjc/1100/1111", "550", "EP/M020355/1", "seed exudate", "QH301 Biology", "551", "630", "QH301", "DIMR 646809", "GE1-350", "2. Zero hunger", "soil mechanical stability", "QE1-996.5", "BB/J000868/1", "Civil_env_eng", "name=Soil Science", "Root exudate", "Geology", "04 agricultural and veterinary sciences", "15. Life on land", "6. Clean water", "Environmental sciences", "BB/J011460/1", "BB/L026058/1", "Engineering and Physical Sciences Research Council (EPSRC)", "rhizosphere-scale indenter and infiltrometer", "soil water repellency", "Biotechnology and Biological Sciences Research Council (BBSRC)", "0401 agriculture", " forestry", " and fisheries", "European Research Council"]}, "links": [{"href": "https://repository.uwl.ac.uk/id/eprint/4977/1/vzj-17-1-170083-1.pdf"}, {"href": "https://eprints.soton.ac.uk/415075/1/vzj2017.04.0083_1.pdf"}, {"href": "https://eprints.soton.ac.uk/415075/2/vzj_17_1_170083_1_.pdf"}, {"href": "https://onlinelibrary.wiley.com/doi/pdf/10.2136/vzj2017.04.0083"}, {"href": "https://doi.org/2164/10082"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Vadose%20Zone%20Journal", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "2164/10082", "name": "item", "description": "2164/10082", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/2164/10082"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-01-01T00:00:00Z"}}, {"id": "2164/19435", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-08-25T16:22:42Z", "type": "Journal Article", "created": "2022-03-17", "title": "Structure and function of the soil microbiome underlying N2O emissions from global wetlands", "description": "Abstract<p>Wetland soils are the greatest source of nitrous oxide (N2O), a critical greenhouse gas and ozone depleter released by microbes. Yet, microbial players and processes underlying the N2O emissions from wetland soils are poorly understood. Using in situ N2O measurements and by determining the structure and potential functional of microbial communities in 645 wetland soil samples globally, we examined the potential role of archaea, bacteria, and fungi in nitrogen (N) cycling and N2O emissions. We show that N2O emissions are higher in drained and warm wetland soils, and are correlated with functional diversity of microbes. We further provide evidence that despite their much lower abundance compared to bacteria, nitrifying archaeal abundance is a key factor explaining N2O emissions from wetland soils globally. Our data suggest that ongoing global warming and intensifying environmental change may boost archaeal nitrifiers, collectively transforming wetland soils to a greater source of N2O.</p", "keywords": ["0301 basic medicine", "570", "571", "Supplementary Data", "QH301 Biology", "Science", "General Biochemistry", "Genetics and Molecular Biology", "Nitrous Oxide", "General Physics and Astronomy", "Soil Science", "551", "852993", "Article", "DH150187", "QH301", "Greenhouse Gases", "Soil", "03 medical and health sciences", "948219", "General", "Soil Microbiology", "0303 health sciences", "Microbiota", "Q", "General Chemistry", "15. Life on land", "6. Clean water", "BBS/e/F/000Pr10355", "13. Climate action", "BB/r012490/1", "Wetlands", "Biotechnology and Biological Sciences Research Council (BBSRC)", "Other", "European Research Council"]}, "links": [{"href": "https://pub.epsilon.slu.se/27540/1/bahram-m-et-al-220412.pdf"}, {"href": "https://ueaeprints.uea.ac.uk/id/eprint/84269/1/Published_Version.pdf"}, {"href": "https://www.nature.com/articles/s41467-022-29161-3.pdf"}, {"href": "https://doi.org/2164/19435"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Nature%20Communications", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "2164/19435", "name": "item", "description": "2164/19435", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/2164/19435"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-03-17T00:00:00Z"}}, {"id": "2164/20152", "type": "Feature", "geometry": null, "properties": {"updated": "2026-08-25T16:22:42Z", "type": "Journal Article", "created": "2022-11-10", "title": "Management-induced changes in soil organic carbon  on global croplands", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Abstract. Soil organic carbon (SOC), one of the largest terrestrial carbon (C) stocks on Earth, has been depleted by anthropogenic land cover change and agricultural management. However, the latter has so far not been well represented in global C stock assessments. While SOC models often simulate detailed biochemical processes that lead to the accumulation and decay of SOC, the management decisions driving these biophysical processes are still little investigated at the global scale. Here we develop a spatially explicit data set for agricultural management on cropland, considering crop production levels, residue returning rates, manure application, and the adoption of irrigation and tillage practices. We combine it with a reduced-complexity model based on the Intergovernmental Panel on Climate Change (IPCC) tier\u00a02 method to create a half-degree resolution data set of SOC stocks and SOC stock changes for the first 30\u2009cm of mineral soils. We estimate that, due to arable farming, soils have lost around 34.6\u2009GtC relative to a counterfactual hypothetical natural state in 1975. Within the period 1975\u20132010, this SOC debt continued to expand by 5\u2009GtC (0.14\u2009GtC\u2009yr\u22121) to around 39.6\u2009GtC. However, accounting for historical management led to 2.1\u2009GtC fewer (0.06\u2009GtC\u2009yr\u22121) emissions than under the assumption of constant management. We also find that management decisions have influenced the historical SOC trajectory most strongly by residue returning, indicating that SOC enhancement by biomass retention may be a promising negative emissions technique. The reduced-complexity SOC model may allow us to simulate management-induced SOC enhancement \u2013 also within computationally demanding integrated (land use) assessment modeling.</p></article>", "keywords": ["570", "AGRICULTURE", "550", "Supplementary Data", "QH301 Biology", "agricultural management", "crop production", "SEQUESTRATION", "551", "01 natural sciences", "630", "NITROGEN-CYCLE", "QH301", "Life", "land cover", "QH501-531", "SDG 13 - Climate Action", "soil carbon", "SDG 2 - Zero Hunger", "EMISSIONS", "CROPS", "QH540-549.5", "global change", "SDG 15 - Life on Land", "0105 earth and related environmental sciences", "2. Zero hunger", "QE1-996.5", "Ecology", "INTENSIFICATION", "VEGETATION MODEL", "Geology", "LAND-USE CHANGE", "15. Life on land", "carbon sequestration", "CLIMATE", "COVER CHANGE", "agricultural land", "13. Climate action", "trajectory", "Intergovernmental Panel on Climate Change"]}, "links": [{"href": "https://bg.copernicus.org/articles/19/5125/2022/bg-19-5125-2022.pdf"}, {"href": "https://doi.org/2164/20152"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Biogeosciences", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "2164/20152", "name": "item", "description": "2164/20152", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/2164/20152"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2020-12-22T00:00:00Z"}}, {"id": "2164/21392", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-08-25T16:22:42Z", "type": "Journal Article", "created": "2023-03-14", "title": "Trade\u2010offs in carbon\u2010degrading enzyme activities limit long\u2010term soil carbon sequestration with biochar addition", "description": "ABSTRACT<p>Biochar amendment is one of the most promising agricultural approaches to tackle climate change by enhancing soil carbon (C) sequestration. Microbial\uffe2\uff80\uff90mediated decomposition processes are fundamental for the fate and persistence of sequestered C in soil, but the underlying mechanisms are uncertain. Here, we synthesise 923 observations regarding the effects of biochar addition (over periods ranging from several weeks to several years) on soil C\uffe2\uff80\uff90degrading enzyme activities from 130 articles across five continents worldwide. Our results showed that biochar addition increased soil ligninase activity targeting complex phenolic macromolecules by 7.1%, but suppressed cellulase activity degrading simpler polysaccharides by 8.3%. These shifts in enzyme activities explained the most variation of changes in soil C sequestration across a wide range of climatic, edaphic and experimental conditions, with biochar\uffe2\uff80\uff90induced shift in ligninase:cellulase ratio correlating negatively with soil C sequestration. Specifically, short\uffe2\uff80\uff90term (&lt;1\uffc2\uffa0year) biochar addition significantly reduced cellulase activity by 4.6% and enhanced soil organic C sequestration by 87.5%, whereas no significant responses were observed for ligninase activity and ligninase:cellulase ratio. However, long\uffe2\uff80\uff90term (\uffe2\uff89\uffa51\uffc2\uffa0year) biochar addition significantly enhanced ligninase activity by 5.2% and ligninase:cellulase ratio by 36.1%, leading to a smaller increase in soil organic C sequestration (25.1%). These results suggest that shifts in enzyme activities increased ligninase:cellulase ratio with time after biochar addition, limiting long\uffe2\uff80\uff90term soil C sequestration with biochar addition. Our work provides novel evidence to explain the diminished soil C sequestration with long\uffe2\uff80\uff90term biochar addition and suggests that earlier studies may have overestimated soil C sequestration with biochar addition by failing to consider the physiological acclimation of soil microorganisms over time.</p", "keywords": ["Carbon Sequestration", "Supplementary Data", "QH301 Biology", "General Biochemistry", "Genetics and Molecular Biology", "soil microorganism", "551", "QH301", "Soil", "soil carbon sequestration", "SDG 13 - Climate Action", "Cellulases", "Biochar addition", "European Commission", "2. Zero hunger", "GE", "15. Life on land", "Carbon", "enzyme activity", "meta-analysis", "enzyme activities", "13. Climate action", "experimental duration", "839806", "Other", "figshare", "General Agricultural and Biological Sciences", "biochar addition", "GE Environmental Sciences", "European Research Council"]}, "links": [{"href": "https://doi.org/2164/21392"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Biological%20Reviews", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "2164/21392", "name": "item", "description": "2164/21392", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/2164/21392"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2023-03-13T00:00:00Z"}}, {"id": "2263/91312", "type": "Feature", "geometry": null, "properties": {"updated": "2026-08-25T16:22:43Z", "type": "Journal Article", "created": "2022-11-24", "title": "Grazing and ecosystem service delivery in global drylands", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Grazing represents the most extensive use of land worldwide. Yet its impacts on ecosystem services remain uncertain because pervasive interactions between grazing pressure, climate, soil properties, and biodiversity may occur but have never been addressed simultaneously. Using a standardized survey at 98 sites across six continents, we show that interactions between grazing pressure, climate, soil, and biodiversity are critical to explain the delivery of fundamental ecosystem services across drylands worldwide. Increasing grazing pressure reduced ecosystem service delivery in warmer and species-poor drylands, whereas positive effects of grazing were observed in colder and species-rich areas. Considering interactions between grazing and local abiotic and biotic factors is key for understanding the fate of dryland ecosystems under climate change and increasing human pressure.</p></article>", "keywords": ["[SDE] Environmental Sciences", "Climate", "Edafolog\u00eda (Biolog\u00eda)", "630", "3104 Producci\u00f3n Animal", "Dryland", "Soil", "636", "2511.06 Conservaci\u00f3n de Suelos", "591.5", "Climate change", "3104.90 Sistemas de Producci\u00f3n Ganadera", "biodiversity", "2. Zero hunger", "2417.13 Ecolog\u00eda Vegetal", "Qu\u00edmica", "Biodiversity", "2502 Climatolog\u00eda", "Grazing", "2401.06 Ecolog\u00eda Animal", "[SDE]Environmental Sciences", "ddc:570", "Rangeland", "581.5", "Ecolog\u00eda (Biolog\u00eda)", "570", "632.11", "Ecosystem services (ES)", "Livestock", "Climate Change", "631.45", "Wild", "SDG-02: Zero hunger", "XXXXXX - Unknown", "Humans", "Ecosystem services", "grazing", "Herbivory", "14. Life underwater", "climate", "Institut f\u00fcr Biochemie und Biologie", "631.585", "Ecosystem", "551.583", "SDG-15: Life on land", "3103.10 Pastos", "Systems", "Drylands", "15. Life on land", "13. Climate action", "58.032.3", "Veterinaria", "ecosystem services"]}, "links": [{"href": "https://repositorio.ulisboa.pt/bitstream/10451/56169/1/abq4062_CombinedPDF_v4.pdf"}, {"href": "https://doi.org/2263/91312"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Science", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "2263/91312", "name": "item", "description": "2263/91312", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/2263/91312"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-11-25T00:00:00Z"}}, {"id": "2809132863", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-08-25T16:22:51Z", "type": "Journal Article", "created": "2018-06-19", "title": "Combining a Two Source Energy Balance Model Driven by MODIS and MSG-SEVIRI Products with an Aggregation Approach to Estimate Turbulent Fluxes over Sparse and Heterogeneous Vegetation in Sahel Region (Niger)", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Estimates of turbulent fluxes (i.e., sensible and latent heat fluxes H and LE) over heterogeneous surfaces is not an easy task. The heterogeneity caused by the contrast in vegetation, hydric and soil conditions can generate a large spatial variability in terms of surface\u2013atmosphere interactions. This study considered the issue of using a thermal-based two-source energy model (TSEB) driven by MODIS (Moderate resolution Imaging Spectroradiometer) and MSG (Meteosat Second Generation) observations in conjunction with an aggregation scheme to derive area-averaged H and LE over a heterogeneous watershed in Niamey, Niger (Wankama catchment). Data collected in the context of the African Monsoon Multidisciplinary Analysis (AMMA) program, including a scintillometry campaign, were used to test the proposed approach. The model predictions of area-averaged turbulent fluxes were compared to data acquired by a Large Aperture Scintillometer (LAS) set up over a transect about 3.2 km-long and spanning three vegetation types (millet, fallow and degraded shrubs). First, H and LE fluxes were estimated at the MSG-SEVIRI grid scale by neglecting explicitly the subpixel heterogeneity. Moreover, the impact of upscaling the model\u2019s inputs was investigated using in-situ input data and three aggregation schemes of increasing complexity based on MODIS products: a simple averaging of inputs at the MODIS resolution scale, another simple averaging scheme that considers scintillometer footprint extent, and the weighted average of inputs based on the footprint weighting function. The H and LE simulated using the footprint weighted method were more accurate than for the two other aggregation rules despite the heterogeneity of the landscape. The statistical values are: correlation coefficient (R) = 0.71, root mean square error (RMSE) = 63 W/m2 and mean bias error (MBE) = \u221223 W/m2 for H and an R = 0.82, RMSE = 88 W/m2 and MBE = 45 W/m2 for LE. This study opens perspectives for the monitoring of convective and evaporative fluxes over heterogeneous landscape based on medium resolution satellite products.</p></article>", "keywords": ["550", "Science", "0207 environmental engineering", "02 engineering and technology", "551", "01 natural sciences", "7. Clean energy", "TSEB model", "aggregation schemes", "scintillometry", "non-uniform and heterogeneous surfaces", "11. Sustainability", "heterogeneous surfaces", "0105 earth and related environmental sciences", "Q", "SEVIRI", "15. Life on land", "[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces", " environment", "6. Clean water", "3. Good health", "non-uniform and", "MODIS", "13. Climate action", "[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces", "regional surfaces fluxes", "environment"]}, "links": [{"href": "http://www.mdpi.com/2072-4292/10/6/974/pdf"}, {"href": "https://doi.org/2809132863"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Remote%20Sensing", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "2809132863", "name": "item", "description": "2809132863", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/2809132863"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-06-19T00:00:00Z"}}, {"id": "3163216605", "type": "Feature", "geometry": null, "properties": {"updated": "2026-08-25T16:23:08Z", "type": "Journal Article", "created": "2021-05-17", "title": "Estimating lockdown-induced European NO2 changes using satellite and surface observations and air quality models", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Abstract. This study provides a comprehensive assessment of NO2 changes across the main European urban areas induced by COVID-19 lockdowns using satellite retrievals from the Tropospheric Monitoring Instrument (TROPOMI) onboard the Sentinel-5p satellite, surface site measurements, and simulations from the Copernicus Atmosphere Monitoring Service (CAMS) regional ensemble of air quality models. Some recent TROPOMI-based estimates of changes in atmospheric NO2 concentrations have neglected the influence of weather variability between the reference and lockdown periods. Here we provide weather-normalized estimates based on a machine learning method (gradient boosting) along with an assessment of the biases that can be expected from methods that omit the influence of weather. We also compare the weather-normalized satellite-estimated NO2 column changes with weather-normalized surface NO2 concentration changes and the CAMS regional ensemble, composed of 11 models, using recently published estimates of emission reductions induced by the lockdown. All estimates show similar NO2 reductions. Locations where the lockdown measures were stricter show stronger reductions, and, conversely, locations where softer measures were implemented show milder reductions in NO2 pollution levels. Average reduction estimates based on either satellite observations (\u221223\u2009%), surface stations (\u221243\u2009%), or models (\u221232\u2009%) are presented, showing the importance of vertical sampling but also the horizontal representativeness. Surface station estimates are significantly changed when sampled to the TROPOMI overpasses (\u221237\u2009%), pointing out the importance of the variability in time of such estimates. Observation-based machine learning estimates show a stronger temporal variability than model-based estimates.                     </p></article>", "keywords": ["[SDE] Environmental Sciences", "550", "QC1-999", "551", "COVID-19 (Malaltia)", "01 natural sciences", "COVID-19 (Malaltia) -- Aspectes ambientals", "COVID-19 (Disease)", "Lockdown", "11. Sustainability", "Satellite images", "QD1-999", "0105 earth and related environmental sciences", "info:eu-repo/classification/ddc/550", "Air quality models", "Physics", "Aire -- Qualitat", "COVID-19", "Surface observations", "Satellite observations", "Chemistry", "Meteorology and Atmospheric Sciences", "13. Climate action", "[SDE]Environmental Sciences", "Air quality", "Meteorologi och atmosf\u00e4rsvetenskap", "\u00c0rees tem\u00e0tiques de la UPC::Desenvolupament hum\u00e0 i sostenible::Degradaci\u00f3 ambiental::Contaminaci\u00f3 atmosf\u00e8rica", ":Desenvolupament hum\u00e0 i sostenible::Degradaci\u00f3 ambiental::Contaminaci\u00f3 atmosf\u00e8rica [\u00c0rees tem\u00e0tiques de la UPC]"]}, "links": [{"href": "https://doi.org/3163216605"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Atmospheric%20Chemistry%20and%20Physics", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "3163216605", "name": "item", "description": "3163216605", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/3163216605"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-05-17T00:00:00Z"}}, {"id": "3210439835", "type": "Feature", "geometry": null, "properties": {"updated": "2026-08-25T16:23:11Z", "type": "Journal Article", "created": "2021-11-03", "title": "Improved global-scale predictions of soil carbon stocks with Millennial Version 2", "description": "Abstract   Soil carbon (C) models are used to predict C sequestration responses to climate and land use change. Yet, the soil models embedded in Earth system models typically do not represent processes that reflect our current understanding of soil C cycling, such as microbial decomposition, mineral association, and aggregation. Rather, they rely on conceptual pools with turnover times that are fit to bulk C stocks and/or fluxes. As measurements of soil fractions become increasingly available, it is necessary for soil C models to represent these measurable quantities so that model processes can be evaluated more accurately. Here we present Version 2 (V2) of the Millennial model, a soil model developed to simulate C pools that can be measured by extraction or fractionation, including particulate organic C, mineral-associated organic C, aggregate C, microbial biomass, and low molecular weight C. Model processes have been updated to reflect the current understanding of mineral-association, temperature sensitivity and reaction kinetics, and different model structures were tested within an open-source framework. We evaluated the ability of Millennial V2 to simulate total soil organic C (SOC), as well as the mineral-associated and particulate fractions, using three independent data sets of soil fractionation measurements spanning a range of climate and geochemistry in Australia (N\u00a0=\u00a0495), Europe (N\u00a0=\u00a0175), and across the globe (N\u00a0=\u00a0659). When using all the data together (N\u00a0=\u00a01329), the Millennial V2 model predicted SOC (RMSE\u00a0=\u00a03.3\u00a0kg\u00a0C m\u22122, AIC\u00a0=\u00a0675,      R   i  n   2     \u00a0=\u00a00.31,      R   o  u  t   2     \u00a0=\u00a00.26) better than the widely-used first-order decomposition model Century (RMSE\u00a0=\u00a03.4\u00a0kg\u00a0C m\u22122, AIC\u00a0=\u00a0696,      R   i  n   2     \u00a0=\u00a00.21,      R   o  u  t   2     \u00a0=\u00a00.18) across sites, despite the fact that Millennial V2 has an increase in process complexity and number of parameters compared to Century. Millennial V2 also reproduced the observed fraction of C in MAOM and larger particle size fractions for most latitudes and biomes, and allows for a more detailed understanding of the pools and processes that affect model performance. It is important to note that this study evaluates the spatial variation in C stock only, and that the temporal dynamics of Millennial V2 remain to be tested. The Millennial V2 model updates the conceptual Century model pools and processes and represents our current understanding of the roles that microbial activity, mineral association and aggregation play in soil C sequestration.", "keywords": ["2. Zero hunger", "[SDU.OCEAN]Sciences of the Universe [physics]/Ocean", "550", "Mineral association", "Atmosphere", "Soil organic carbon stocks", "[SDU.OCEAN] Sciences of the Universe [physics]/Ocean", " Atmosphere", "15. Life on land", "551", "Microbial decomposition", "01 natural sciences", "[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces", " environment", "13. Climate action", "Soil carbon modeling", "[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces", "environment", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/3210439835"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20Biology%20and%20Biochemistry", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "3210439835", "name": "item", "description": "3210439835", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/3210439835"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-01-01T00:00:00Z"}}, {"id": "39561539", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-08-25T16:23:21Z", "type": "Journal Article", "created": "2024-11-17", "title": "Mobilization of poly- and perfluoroalkyl substances (PFAS) from heterogeneous soils: Desorption by ethanol/xanthan gum mixture", "description": "Remediating soils contaminated by per- and polyfluoroalkyl substances (PFAS) is a challenging task due to the unique properties of these compounds, such as variable solubility and resistance to degradation. In-situ soil flushing with solvents has been considered as a remediation technique for PFAS-contaminated soils. The use of non-Newtonian fluids, displaying variable viscosity depending on the applied shear rate, can offer certain advantages in improving the efficiency of the process, particularly in heterogeneous porous media. In this work, the efficacy of ethanol/xanthan mixture (XE) in the recovery of a mixture of perfluorooctane sulfonate (PFOS), perfluorooctanoic acid (PFOA), perfluorohexane sulfonate (PFHxS), and perfluorobutane sulfonate (PFBS) from soil has been tested at lab-scale. XE's non-Newtonian behavior was examined through rheological measurements, confirming that ethanol did not affect xanthan gum's (XG) shear-thinning behavior. The recovery of PFAS in batch-desorption exceeded 95\u00a0% in ethanol, and 99\u00a0% in XE, except for PFBS which reached 94\u00a0%. 1D-column experiments revealed overshoots in PFAS breakthrough curves during ethanol and XE injection, due to over-solubilization. XE, (XG 0.05\u00a0% w/w) could recover 99\u00a0% PFOA, 98\u00a0% PFBS, 97\u00a0% PFHxS, and 92\u00a0% PFOS. Numerical modeling successfully reproduces breakthrough curves for PFOA, PFHxS, and PFBS with the convection-dispersion-sorption equation and Langmuir sorption isotherm.", "keywords": ["Heterogeneity of porous media", "628", "[SDU.STU] Sciences of the Universe [physics]/Earth Sciences", "[SDU.STU]Sciences of the Universe [physics]/Earth Sciences", "Desorption", "551", "Alcohol", "Poly- and perfluoroalkyl substances (PFAS)", "Non-Newtonian fluids (NNF)"]}, "links": [{"href": "https://doi.org/39561539"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Hazardous%20Materials", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "39561539", "name": "item", "description": "39561539", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/39561539"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2025-01-01T00:00:00Z"}}, {"id": "699cce7b36d2cdfbbf190e86cca42533", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-08-25T16:23:52Z", "type": "Report", "title": "Multi-modelling predictions show high uncertainty of required carbon input changes to reach a 4 parts per thousand target", "description": "Soils store vast amounts of carbon (C) on land, and increasing soil organic carbon (SOC) stocks in already managed soils such as croplands may be one way to remove C from the atmosphere, thereby limiting subsequent warming. The main objective of this study was to estimate the amount of additional C input needed to annually increase SOC stocks by 4%(0) at 16 long-term agricultural experiments in Europe, including exogenous organic matter (EOM) additions. We used an ensemble of six SOC models and ran them under two configurations: (1) with default parametrization and (2) with parameters calibrated site-by-site to fit the evolution of SOC stocks in the control treatments (without EOM). We compared model simulations and analysed the factors generating variability across models. The calibrated ensemble was able to reproduce the SOC stock evolution in the unfertilised control treatments. We found that, on average, the experimental sites needed an additional 1.5 +/- 1.2 Mg C ha(-)(1) year(-1) to increase SOC stocks by 4%(0) per year over 30 years, compared to the C input in the control treatments (multi-model median +/- median standard deviation across sites). That is, a 119% increase compared to the control. While mean annual temperature, initial SOC stocks and initial C input had a significant effect on the variability of the predicted C input in the default configuration (i.e., the relative standard deviation of the predicted C input from the mean), only water-related variables (i.e., mean annual precipitation and potential evapotranspiration) explained the divergence between models when calibrated. Our work highlights the challenge of increasing SOC stocks in agriculture and accentuates the need to increasingly lean on multi-model ensembles when predicting SOC stock trends and related processes. To increase the reliability of SOC models under future climate change, we suggest model developers to better constrain the effect of water-related variables on SOC decomposition.", "keywords": ["2. Zero hunger", "13. Climate action", "Soil Science", "15. Life on land", "551"], "contacts": [{"organization": "Bruni, Elisa, Chenu, Claire, Abramoff, Rose Z., Baldoni, Guido, Barkusky, Dietmar, Clivot, Hugues, Huang, Yuanyuan, K\u00e4tterer, Thomas, Pikula, Dorota, Virto, Inigo, Guenet, Bertrand,", "roles": ["creator"]}]}, "links": [{"href": "https://pub.epsilon.slu.se/31490/1/bruni-e-et-al-20230810.pdf"}, {"href": "https://doi.org/699cce7b36d2cdfbbf190e86cca42533"}, {"rel": "self", "type": "application/geo+json", "title": "699cce7b36d2cdfbbf190e86cca42533", "name": "item", "description": "699cce7b36d2cdfbbf190e86cca42533", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/699cce7b36d2cdfbbf190e86cca42533"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-01-01T00:00:00Z"}}, {"id": "oai:pub.epsilon.slu.se:31490", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-08-25T16:28:15Z", "type": "Report", "title": "Multi-modelling predictions show high uncertainty of required carbon input changes to reach a 4 parts per thousand target", "description": "Soils store vast amounts of carbon (C) on land, and increasing soil organic carbon (SOC) stocks in already managed soils such as croplands may be one way to remove C from the atmosphere, thereby limiting subsequent warming. The main objective of this study was to estimate the amount of additional C input needed to annually increase SOC stocks by 4%(0) at 16 long-term agricultural experiments in Europe, including exogenous organic matter (EOM) additions. We used an ensemble of six SOC models and ran them under two configurations: (1) with default parametrization and (2) with parameters calibrated site-by-site to fit the evolution of SOC stocks in the control treatments (without EOM). We compared model simulations and analysed the factors generating variability across models. The calibrated ensemble was able to reproduce the SOC stock evolution in the unfertilised control treatments. We found that, on average, the experimental sites needed an additional 1.5 +/- 1.2 Mg C ha(-)(1) year(-1) to increase SOC stocks by 4%(0) per year over 30 years, compared to the C input in the control treatments (multi-model median +/- median standard deviation across sites). That is, a 119% increase compared to the control. While mean annual temperature, initial SOC stocks and initial C input had a significant effect on the variability of the predicted C input in the default configuration (i.e., the relative standard deviation of the predicted C input from the mean), only water-related variables (i.e., mean annual precipitation and potential evapotranspiration) explained the divergence between models when calibrated. Our work highlights the challenge of increasing SOC stocks in agriculture and accentuates the need to increasingly lean on multi-model ensembles when predicting SOC stock trends and related processes. To increase the reliability of SOC models under future climate change, we suggest model developers to better constrain the effect of water-related variables on SOC decomposition.", "keywords": ["2. Zero hunger", "13. Climate action", "Soil Science", "15. 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