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    <dct:references>https://amt.copernicus.org/articles/18/3073/2025/amt-18-3073-2025.pdf</dct:references>
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    <dct:isPartOf>Atmospheric Measurement Techniques</dct:isPartOf>
    <dct:license>Open Access</dct:license>
    <dct:created>2025-07-11</dct:created>
    <dct:created>2025-02-24</dct:created>
    <dct:available>2025-02-24</dct:available>
    <dc:description>&lt;?xml version='1.0' encoding='UTF-8'?&gt;&lt;article&gt;&lt;p&gt;Abstract. A novel reference absorption instrument based on photothermal interferometry &#8211; the dual-wavelength photothermal aerosol absorption monitor PTAAM-2&#955; &#8211; and scattering measurements are used to characterize filter photometer artifacts in measurements of absorption coefficients of soot- and dust-dominated aerosol samples within laboratory and ambient campaigns. We provide, for different aerosol types, reference values of the multiple-scattering parameter, quantifying the artifact introduced by the interaction between the light, the particles, and the filter. The Aethalometer AE33 and the Continuous Light Absorption Photometer (CLAP) were characterized during a laboratory campaign where different soot and mineral dust samples were measured. Furthermore, ambient measurements during a campaign in Granada, Spain, were used to characterize the AE33 and MAAP (Multiangle Absorption Photometer), a pseudo-reference absorption instrument. The laboratory campaign showed significant wavelength dependence of the calibration parameter, the multiple-scattering parameter C. The C of the AE33 at 450 and 808&#8201;nm was 4.08 and 3.95 and 6.25 and 5.27 for propane soot and diesel soot, respectively. For the CLAP, the C was 5.10 and 4.26 and 6.79 and 5.80 for propane and diesel soot, respectively. For the different mineral dust samples analyzed in the laboratory, the C at 450&#8201;nm ranged between 2.74 and 3.03 for the AE33 and between 2.50 and 2.80 for the CLAP. The ambient measurements at Granada showed an overall C of 4.72 at 450&#8201;nm and of 3.90 at 808&#8201;nm for the AE33. The results for both the AE33 and the CLAP show a dependence with the particle size, with fine particles having the highest C values and with the C being reduced and leveling off for larger particles. Both the laboratory and the ambient measurements of the AE33 showed overlapping results. The cross-sensitivity to scattering was smaller for the CLAP than for the AE33. The values of the cross-sensitivity parameter ms at 450 and 808&#8201;nm were 3.0&#8201;% and 1.5&#8201;% for the AE33 and 2.4&#8201;% and 0.9&#8201;% for the CLAP. The intercomparison of the MAAP with the PTAAM-2&#955; during the ambient campaign in Granada showed that the MAAP overestimates the absorption coefficients for 47&#8201;% at 637&#8201;nm and features a cross-sensitivity to scattering of 2.4&#8201;%.&lt;/p&gt;&lt;/article&gt;</dc:description>
    <dc:subject>Make cities and human settlements inclusive, safe, resilient and sustainable</dc:subject>
    <dc:subject>Take urgent action to combat climate change and its impacts</dc:subject>
    <dc:subject>Build resilient infrastructure, promote inclusive and sustainable industrialization and foster innovation</dc:subject>
    <dc:subject>Earthwork. Foundations</dc:subject>
    <dc:subject>TA715-787</dc:subject>
    <dc:subject>Environmental engineering</dc:subject>
    <dc:subject>http://metadata.un.org/sdg/13</dc:subject>
    <dc:subject>http://metadata.un.org/sdg/3</dc:subject>
    <dc:subject>TA170-171</dc:subject>
    <dc:subject>Aerosol absorption</dc:subject>
    <dc:subject>http://metadata.un.org/sdg/11</dc:subject>
    <dc:subject>http://metadata.un.org/sdg/9</dc:subject>
    <dc:subject>Ensure healthy lives and promote well-being for all at all ages</dc:subject>
    <dc:creator rdf:resource="https://orcid.org/0000-0002-8124-1492"/>
    <dc:creator rdf:resource="https://orcid.org/0000-0003-3576-7167"/>
    <dc:creator rdf:resource="https://orcid.org/0000-0003-3630-5079"/>
    <dc:creator rdf:resource="https://orcid.org/0000-0003-1831-6874"/>
    <dc:creator rdf:resource="https://orcid.org/0000-0003-4341-7845"/>
    <dc:creator rdf:resource="https://orcid.org/0000-0002-6549-9899"/>
    <dc:creator rdf:resource="https://orcid.org/0000-0002-4456-0697"/>
    <dc:creator>J. Yus-D&#237;ez, L. Drinovec, L. Drinovec, L. Alados-Arboledas, G. Titos, E. Bazo, A. Casans, D. Patr&#243;n, X. Querol, A. Gonzalez-Romero, C. Perez Garc&#237;a-Pando, C. Perez Garc&#237;a-Pando, G. Mo&#269;nik, G. Mo&#269;nik, </dc:creator>
    <dc:date>2025-02-24</dc:date>
    <dc:type>journalpaper</dc:type>
    <dct:abstract>&lt;?xml version='1.0' encoding='UTF-8'?&gt;&lt;article&gt;&lt;p&gt;Abstract. A novel reference absorption instrument based on photothermal interferometry &#8211; the dual-wavelength photothermal aerosol absorption monitor PTAAM-2&#955; &#8211; and scattering measurements are used to characterize filter photometer artifacts in measurements of absorption coefficients of soot- and dust-dominated aerosol samples within laboratory and ambient campaigns. We provide, for different aerosol types, reference values of the multiple-scattering parameter, quantifying the artifact introduced by the interaction between the light, the particles, and the filter. The Aethalometer AE33 and the Continuous Light Absorption Photometer (CLAP) were characterized during a laboratory campaign where different soot and mineral dust samples were measured. Furthermore, ambient measurements during a campaign in Granada, Spain, were used to characterize the AE33 and MAAP (Multiangle Absorption Photometer), a pseudo-reference absorption instrument. The laboratory campaign showed significant wavelength dependence of the calibration parameter, the multiple-scattering parameter C. The C of the AE33 at 450 and 808&#8201;nm was 4.08 and 3.95 and 6.25 and 5.27 for propane soot and diesel soot, respectively. For the CLAP, the C was 5.10 and 4.26 and 6.79 and 5.80 for propane and diesel soot, respectively. For the different mineral dust samples analyzed in the laboratory, the C at 450&#8201;nm ranged between 2.74 and 3.03 for the AE33 and between 2.50 and 2.80 for the CLAP. The ambient measurements at Granada showed an overall C of 4.72 at 450&#8201;nm and of 3.90 at 808&#8201;nm for the AE33. The results for both the AE33 and the CLAP show a dependence with the particle size, with fine particles having the highest C values and with the C being reduced and leveling off for larger particles. Both the laboratory and the ambient measurements of the AE33 showed overlapping results. The cross-sensitivity to scattering was smaller for the CLAP than for the AE33. The values of the cross-sensitivity parameter ms at 450 and 808&#8201;nm were 3.0&#8201;% and 1.5&#8201;% for the AE33 and 2.4&#8201;% and 0.9&#8201;% for the CLAP. The intercomparison of the MAAP with the PTAAM-2&#955; during the ambient campaign in Granada showed that the MAAP overestimates the absorption coefficients for 47&#8201;% at 637&#8201;nm and features a cross-sensitivity to scattering of 2.4&#8201;%.&lt;/p&gt;&lt;/article&gt;</dct:abstract>
    <dc:title>Characterization of filter photometer artifacts in soot and dust measurements &#8211; laboratory and ambient experiments using a traceably calibrated aerosol absorption reference</dc:title>
    <dc:identifier>10261/401848</dc:identifier>
    <dct:relation>773051</dct:relation>
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