<rdf:RDF xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:dcat="http://www.w3.org/ns/dcat#" xmlns:dct="http://purl.org/dc/terms/" xmlns:rdf="http://www.w3.org/1999/02/22-rdf-syntax-ns#">
  <rdf:Description rdf:about="https://doi.org/10.1098/rstb.2017.0302">
    <dct:isReferencedBy>CORDIS</dct:isReferencedBy>
    <dct:isReferencedBy>OpenAire</dct:isReferencedBy>
    <dct:isReferencedBy>Research@WUR</dct:isReferencedBy>
    <dct:isReferencedBy>Sygma</dct:isReferencedBy>
    <dct:isReferencedBy>Bielefeld Academic Search Engine (BASE)</dct:isReferencedBy>
    <dct:isReferencedBy>OPUS Augsburg</dct:isReferencedBy>
    <dct:isReferencedBy>HAL-INSU</dct:isReferencedBy>
    <dct:isReferencedBy>Crossref</dct:isReferencedBy>
    <dct:isReferencedBy>Microsoft Academic Graph</dct:isReferencedBy>
    <dct:isReferencedBy>Europe PubMed Central</dct:isReferencedBy>
    <dct:isReferencedBy>CORE (RIOXX-UK Aggregator)</dct:isReferencedBy>
    <dct:isReferencedBy>UnpayWall</dct:isReferencedBy>
    <dct:isReferencedBy>e-space at Manchester Metropolitan University</dct:isReferencedBy>
    <dct:isReferencedBy>PubMed Central</dct:isReferencedBy>
    <dct:isReferencedBy>HAL-CEA</dct:isReferencedBy>
    <dct:isReferencedBy>European Union Open Data Portal</dct:isReferencedBy>
    <dct:references>https://eprints.whiterose.ac.uk/135234/8/Tropical%20land%20carbon%20cycle%20responses%20to%202015/16%20El%20Ni%C3%B1o%20as%20recorded%20by%20atmospheric%20greenhouse%20gas%20and%20remote%20sensing%20data.pdf</dct:references>
    <dct:references>https://royalsocietypublishing.org/doi/pdf/10.1098/rstb.2017.0302</dct:references>
    <dct:references>https://doi.org/10.1098/rstb.2017.0302</dct:references>
    <dcat:downloadURL rdf:resource="https://eprints.whiterose.ac.uk/135234/8/Tropical%20land%20carbon%20cycle%20responses%20to%202015/16%20El%20Ni%C3%B1o%20as%20recorded%20by%20atmospheric%20greenhouse%20gas%20and%20remote%20sensing%20data.pdf"/>
    <dcat:downloadURL rdf:resource="https://royalsocietypublishing.org/doi/pdf/10.1098/rstb.2017.0302"/>
    <dct:isPartOf>Philosophical Transactions of the Royal Society B: Biological Sciences</dct:isPartOf>
    <dct:license>Open Access</dct:license>
    <dct:created>2018-10-08</dct:created>
    <dct:available>2021-07-01</dct:available>
    <dc:description>&lt;p&gt;             The outstanding tropical land climate characteristic over the past decades is rapid warming, with no significant large-scale precipitation trends. This warming is expected to continue but the effects on tropical vegetation are unknown. El Ni&#65475;&#65457;o-related heat peaks may provide a test bed for a future hotter world. Here we analyse tropical land carbon cycle responses to the 2015/16 El Ni&#65475;&#65457;o heat and drought anomalies using an atmospheric transport inversion. Based on the global atmospheric CO             2             and fossil fuel emission records, we find no obvious signs of anomalously large carbon release compared with earlier El Ni&#65475;&#65457;o events, suggesting resilience of tropical vegetation. We find roughly equal net carbon release anomalies from Amazonia and tropical Africa, approximately 0.5 PgC each, and smaller carbon release anomalies from tropical East Asia and southern Africa. Atmospheric CO anomalies reveal substantial fire carbon release from tropical East Asia peaking in October 2015 while fires contribute only a minor amount to the Amazonian carbon flux anomaly. Anomalously large Amazonian carbon flux release is consistent with downregulation of primary productivity during peak negative near-surface water anomaly (October 2015 to March 2016) as diagnosed by solar-induced fluorescence. Finally, we find an unexpected anomalous positive flux to the atmosphere from tropical Africa early in 2016, coincident with substantial CO release.           &lt;/p&gt;           &lt;p&gt;This article is part of a discussion meeting issue &#65506;&#65408;&#65432;The impact of the 2015/2016 El Ni&#65475;&#65457;o on the terrestrial tropical carbon cycle: patterns, mechanisms and implications&#65506;&#65408;&#65433;.&lt;/p&gt;</dc:description>
    <dc:subject>Life Sciences &amp; Biomedicine - Other Topics</dc:subject>
    <dc:subject>FLUX</dc:subject>
    <dc:subject>0301 basic medicine</dc:subject>
    <dc:subject>Hot Temperature</dc:subject>
    <dc:subject>550</dc:subject>
    <dc:subject>551</dc:subject>
    <dc:subject>global warming</dc:subject>
    <dc:subject>01 natural sciences</dc:subject>
    <dc:subject>Carbon Cycle</dc:subject>
    <dc:subject>Greenhouse Gases</dc:subject>
    <dc:subject>03 medical and health sciences</dc:subject>
    <dc:subject>[SDU.STU.CL] Sciences of the Universe [physics]/Earth Sciences/Climatology</dc:subject>
    <dc:subject>CHEMICAL-TRANSPORT MODEL</dc:subject>
    <dc:subject>carbon cycle</dc:subject>
    <dc:subject>INVERSION</dc:subject>
    <dc:subject>Biology</dc:subject>
    <dc:subject>TEMPERATURE</dc:subject>
    <dc:subject>11 Medical and Health Sciences</dc:subject>
    <dc:subject>0105 earth and related environmental sciences</dc:subject>
    <dc:subject>tropical forests</dc:subject>
    <dc:subject>El Nino-Southern Oscillation</dc:subject>
    <dc:subject>Evolutionary Biology</dc:subject>
    <dc:subject>Tropical Climate</dc:subject>
    <dc:subject>Science &amp; Technology</dc:subject>
    <dc:subject>Atmosphere</dc:subject>
    <dc:subject>PHOTOSYNTHESIS</dc:subject>
    <dc:subject>EQUATORIAL PACIFIC</dc:subject>
    <dc:subject>Articles</dc:subject>
    <dc:subject>06 Biological Sciences</dc:subject>
    <dc:subject>15. Life on land</dc:subject>
    <dc:subject>[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces, environment</dc:subject>
    <dc:subject>6. Clean water</dc:subject>
    <dc:subject>Droughts</dc:subject>
    <dc:subject>[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology</dc:subject>
    <dc:subject>13. Climate action</dc:subject>
    <dc:subject>PRECIPITATION</dc:subject>
    <dc:subject>Remote Sensing Technology</dc:subject>
    <dc:subject>INDUCED CHLOROPHYLL FLUORESCENCE</dc:subject>
    <dc:subject>CO2</dc:subject>
    <dc:subject>[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces</dc:subject>
    <dc:subject>SENSITIVITY</dc:subject>
    <dc:subject>environment</dc:subject>
    <dc:subject>Life Sciences &amp; Biomedicine</dc:subject>
    <dc:subject>fire</dc:subject>
    <dc:creator rdf:resource="https://orcid.org/0000-0002-0801-0831"/>
    <dc:creator rdf:resource="https://orcid.org/0000-0002-5858-8471"/>
    <dc:creator rdf:resource="https://orcid.org/0000-0003-4908-8974"/>
    <dc:creator rdf:resource="https://orcid.org/0000-0001-8494-0697"/>
    <dc:creator rdf:resource="https://orcid.org/0000-0001-8630-1610"/>
    <dc:creator rdf:resource="https://orcid.org/0000-0002-5955-0483"/>
    <dc:creator rdf:resource="https://orcid.org/0000-0003-3944-9879"/>
    <dc:creator rdf:resource="https://orcid.org/0000-0002-4327-3813"/>
    <dc:creator>Caio S. C. Correia, Lucas G. Domingues, Merritt N. Deeter, Robert J. Parker, Wolfgang Buermann, Peter Somkuti, Luciana V. Gatti, Emanuel Gloor, Chris Wilson, Chris Wilson, Martyn P. Chipperfield, Martyn P. Chipperfield, Wouter Peters, John B. Miller, Martin J. P. Sullivan, Hartmut Boesch, Fr&#233;d&#233;ric Chevallier, </dc:creator>
    <dc:date>2018-10-08</dc:date>
    <dc:type>journalpaper</dc:type>
    <dct:abstract>&lt;p&gt;             The outstanding tropical land climate characteristic over the past decades is rapid warming, with no significant large-scale precipitation trends. This warming is expected to continue but the effects on tropical vegetation are unknown. El Ni&#65475;&#65457;o-related heat peaks may provide a test bed for a future hotter world. Here we analyse tropical land carbon cycle responses to the 2015/16 El Ni&#65475;&#65457;o heat and drought anomalies using an atmospheric transport inversion. Based on the global atmospheric CO             2             and fossil fuel emission records, we find no obvious signs of anomalously large carbon release compared with earlier El Ni&#65475;&#65457;o events, suggesting resilience of tropical vegetation. We find roughly equal net carbon release anomalies from Amazonia and tropical Africa, approximately 0.5 PgC each, and smaller carbon release anomalies from tropical East Asia and southern Africa. Atmospheric CO anomalies reveal substantial fire carbon release from tropical East Asia peaking in October 2015 while fires contribute only a minor amount to the Amazonian carbon flux anomaly. Anomalously large Amazonian carbon flux release is consistent with downregulation of primary productivity during peak negative near-surface water anomaly (October 2015 to March 2016) as diagnosed by solar-induced fluorescence. Finally, we find an unexpected anomalous positive flux to the atmosphere from tropical Africa early in 2016, coincident with substantial CO release.           &lt;/p&gt;           &lt;p&gt;This article is part of a discussion meeting issue &#65506;&#65408;&#65432;The impact of the 2015/2016 El Ni&#65475;&#65457;o on the terrestrial tropical carbon cycle: patterns, mechanisms and implications&#65506;&#65408;&#65433;.&lt;/p&gt;</dct:abstract>
    <dc:title>Tropical land carbon cycle responses to 2015/16 El Ni&#241;o as recorded by atmospheric greenhouse gas and remote sensing data</dc:title>
    <dc:identifier>10.1098/rstb.2017.0302</dc:identifier>
  </rdf:Description>
</rdf:RDF>