Aerosol‐radiation interaction in the cloudless atmosphere during LACE 98 1. Measured and calculated broadband solar and spectral surface insolations
Identifieur interne : 001555 ( Main/Corpus ); précédent : 001554; suivant : 001556Aerosol‐radiation interaction in the cloudless atmosphere during LACE 98 1. Measured and calculated broadband solar and spectral surface insolations
Auteurs : Manfred Wendisch ; Andreas Keil ; Dörthe Müller ; Ulla Wandinger ; Peter Wendling ; Armin Stifter ; Andreas Petzold ; Markus Fiebig ; Matthias Wiegner ; Volker Freudenthaler ; Wolfgang Armbruster ; Wolfgang Von Hoyningen Uene ; Ulrich LeitererSource :
- Journal of Geophysical Research: Atmospheres [ 0148-0227 ] ; 2002-11-16.
Abstract
Vertical profile measurements of aerosol particle size distributions and of meteorological parameters (obtained from aircraft, radiosondes, and lidar) are used as input to a spectral radiative transfer model to calculate broadband solar and spectral surface insolations. The calculated values are compared to measured ones gathered with broadband solar pyranometers and pyrheliometers, and a fixed‐grating photodiode array spectroradiometer with 512 spectral channels between 500 and 920 nm wavelength. The measurements were obtained during the joint field campaign Lindenberg Aerosol Characterization Experiment (LACE) 98 near Berlin/Germany in the summer of 1998. Two cases (days with high and low aerosol loading, respectively) are investigated in detail. Furthermore, a measurement‐based sensitivity analysis was carried out focusing on the influence of particle composition (complex refractive index) and of microphysical and humidity growth uncertainties on the calculated surface insolations. Assuming a spectral refractive index of ammonium sulfate for the aerosol particles, on average the global component of the broadband solar surface insolations is 11–20 W m−2 (2–3%) greater than the measured values; the direct portion is 17–28 W m−2 (4–5%) higher, and its diffuse component is 6–7 W m−2 (4–10%) lower in comparison to the measurements. The measured and calculated spectral surface insolations (global portion) agree well in the central visible spectral region (500–600 nm wavelength). Toward larger wavelengths (near infrared) the calculated spectral surface insolations are increasingly higher than the measured ones.
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DOI: 10.1029/2000JD000226
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Measured and calculated broadband solar and spectral surface insolations</title><author><name sortKey="Wendisch, Manfred" sort="Wendisch, Manfred" uniqKey="Wendisch M" first="Manfred" last="Wendisch">Manfred Wendisch</name><affiliation><mods:affiliation>Institute for Tropospheric Research, Leipzig, Germany</mods:affiliation></affiliation></author><author><name sortKey="Keil, Andreas" sort="Keil, Andreas" uniqKey="Keil A" first="Andreas" last="Keil">Andreas Keil</name><affiliation><mods:affiliation>Institute for Tropospheric Research, Leipzig, Germany</mods:affiliation></affiliation><affiliation><mods:affiliation>Now at Met Office, Farnborough, UK.</mods:affiliation></affiliation></author><author><name sortKey="Muller, Dorthe" sort="Muller, Dorthe" uniqKey="Muller D" first="Dörthe" last="Müller">Dörthe Müller</name><affiliation><mods:affiliation>Institute for Tropospheric Research, Leipzig, Germany</mods:affiliation></affiliation></author><author><name sortKey="Wandinger, Ulla" sort="Wandinger, Ulla" uniqKey="Wandinger U" first="Ulla" last="Wandinger">Ulla Wandinger</name><affiliation><mods:affiliation>Institute for Tropospheric Research, Leipzig, Germany</mods:affiliation></affiliation></author><author><name sortKey="Wendling, Peter" sort="Wendling, Peter" uniqKey="Wendling P" first="Peter" last="Wendling">Peter Wendling</name><affiliation><mods:affiliation>Institute for Physics of the Atmosphere, Oberpfaffenhofen, Germany</mods:affiliation></affiliation></author><author><name sortKey="Stifter, Armin" sort="Stifter, Armin" uniqKey="Stifter A" first="Armin" last="Stifter">Armin Stifter</name><affiliation><mods:affiliation>Institute for Physics of the Atmosphere, Oberpfaffenhofen, Germany</mods:affiliation></affiliation></author><author><name sortKey="Petzold, Andreas" sort="Petzold, Andreas" uniqKey="Petzold A" first="Andreas" last="Petzold">Andreas Petzold</name><affiliation><mods:affiliation>Institute for Physics of the Atmosphere, Oberpfaffenhofen, Germany</mods:affiliation></affiliation></author><author><name sortKey="Fiebig, Markus" sort="Fiebig, Markus" uniqKey="Fiebig M" first="Markus" last="Fiebig">Markus Fiebig</name><affiliation><mods:affiliation>Institute for Physics of the Atmosphere, Oberpfaffenhofen, Germany</mods:affiliation></affiliation></author><author><name sortKey="Wiegner, Matthias" sort="Wiegner, Matthias" uniqKey="Wiegner M" first="Matthias" last="Wiegner">Matthias Wiegner</name><affiliation><mods:affiliation>Meteorological Institute, University of Munich, Munich, Germany</mods:affiliation></affiliation></author><author><name sortKey="Freudenthaler, Volker" sort="Freudenthaler, Volker" uniqKey="Freudenthaler V" first="Volker" last="Freudenthaler">Volker Freudenthaler</name><affiliation><mods:affiliation>Meteorological Institute, University of Munich, Munich, Germany</mods:affiliation></affiliation></author><author><name sortKey="Armbruster, Wolfgang" sort="Armbruster, Wolfgang" uniqKey="Armbruster W" first="Wolfgang" last="Armbruster">Wolfgang Armbruster</name><affiliation><mods:affiliation>Institute for Space Research, Free University of Berlin, Berlin, Germany</mods:affiliation></affiliation><affiliation><mods:affiliation>Now at Department of Optics of the Atmosphere and Meteorology. 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Measured and calculated broadband solar and spectral surface insolations</title><author><name sortKey="Wendisch, Manfred" sort="Wendisch, Manfred" uniqKey="Wendisch M" first="Manfred" last="Wendisch">Manfred Wendisch</name><affiliation><mods:affiliation>Institute for Tropospheric Research, Leipzig, Germany</mods:affiliation></affiliation></author><author><name sortKey="Keil, Andreas" sort="Keil, Andreas" uniqKey="Keil A" first="Andreas" last="Keil">Andreas Keil</name><affiliation><mods:affiliation>Institute for Tropospheric Research, Leipzig, Germany</mods:affiliation></affiliation><affiliation><mods:affiliation>Now at Met Office, Farnborough, UK.</mods:affiliation></affiliation></author><author><name sortKey="Muller, Dorthe" sort="Muller, Dorthe" uniqKey="Muller D" first="Dörthe" last="Müller">Dörthe Müller</name><affiliation><mods:affiliation>Institute for Tropospheric Research, Leipzig, Germany</mods:affiliation></affiliation></author><author><name sortKey="Wandinger, Ulla" sort="Wandinger, Ulla" uniqKey="Wandinger U" first="Ulla" last="Wandinger">Ulla Wandinger</name><affiliation><mods:affiliation>Institute for Tropospheric Research, Leipzig, Germany</mods:affiliation></affiliation></author><author><name sortKey="Wendling, Peter" sort="Wendling, Peter" uniqKey="Wendling P" first="Peter" last="Wendling">Peter Wendling</name><affiliation><mods:affiliation>Institute for Physics of the Atmosphere, Oberpfaffenhofen, Germany</mods:affiliation></affiliation></author><author><name sortKey="Stifter, Armin" sort="Stifter, Armin" uniqKey="Stifter A" first="Armin" last="Stifter">Armin Stifter</name><affiliation><mods:affiliation>Institute for Physics of the Atmosphere, Oberpfaffenhofen, Germany</mods:affiliation></affiliation></author><author><name sortKey="Petzold, Andreas" sort="Petzold, Andreas" uniqKey="Petzold A" first="Andreas" last="Petzold">Andreas Petzold</name><affiliation><mods:affiliation>Institute for Physics of the Atmosphere, Oberpfaffenhofen, Germany</mods:affiliation></affiliation></author><author><name sortKey="Fiebig, Markus" sort="Fiebig, Markus" uniqKey="Fiebig M" first="Markus" last="Fiebig">Markus Fiebig</name><affiliation><mods:affiliation>Institute for Physics of the Atmosphere, Oberpfaffenhofen, Germany</mods:affiliation></affiliation></author><author><name sortKey="Wiegner, Matthias" sort="Wiegner, Matthias" uniqKey="Wiegner M" first="Matthias" last="Wiegner">Matthias Wiegner</name><affiliation><mods:affiliation>Meteorological Institute, University of Munich, Munich, Germany</mods:affiliation></affiliation></author><author><name sortKey="Freudenthaler, Volker" sort="Freudenthaler, Volker" uniqKey="Freudenthaler V" first="Volker" last="Freudenthaler">Volker Freudenthaler</name><affiliation><mods:affiliation>Meteorological Institute, University of Munich, Munich, Germany</mods:affiliation></affiliation></author><author><name sortKey="Armbruster, Wolfgang" sort="Armbruster, Wolfgang" uniqKey="Armbruster W" first="Wolfgang" last="Armbruster">Wolfgang Armbruster</name><affiliation><mods:affiliation>Institute for Space Research, Free University of Berlin, Berlin, Germany</mods:affiliation></affiliation><affiliation><mods:affiliation>Now at Department of Optics of the Atmosphere and Meteorology. Research Society for Applied Natural Sciences, Ettlingen, Germany.</mods:affiliation></affiliation></author><author><name sortKey="Von Hoyningen Uene, Wolfgang" sort="Von Hoyningen Uene, Wolfgang" uniqKey="Von Hoyningen Uene W" first="Wolfgang" last="Von Hoyningen Uene">Wolfgang Von Hoyningen Uene</name><affiliation><mods:affiliation>Institute for Remote Sensing, University of Bremen, Bremen, Germany</mods:affiliation></affiliation></author><author><name sortKey="Leiterer, Ulrich" sort="Leiterer, Ulrich" uniqKey="Leiterer U" first="Ulrich" last="Leiterer">Ulrich Leiterer</name><affiliation><mods:affiliation>Meteorological Observatory, German Weather Service, Lindenberg, Germany</mods:affiliation></affiliation></author></analytic><monogr></monogr><series><title level="j">Journal of Geophysical Research: Atmospheres</title><title level="j" type="abbrev">J. Geophys. Res.</title><idno type="ISSN">0148-0227</idno><idno type="eISSN">2156-2202</idno><imprint><publisher>Blackwell Publishing Ltd</publisher><date type="published" when="2002-11-16">2002-11-16</date><biblScope unit="volume">107</biblScope><biblScope unit="issue">D21</biblScope><biblScope unit="page" from="LAC 6-1">LAC 6-1</biblScope><biblScope unit="page" to="LAC 6-20">LAC 6-20</biblScope></imprint><idno type="ISSN">0148-0227</idno></series><idno type="istex">E56D5E66F1B57EC4A80FBA5AD64DA2EE12767F47</idno><idno type="DOI">10.1029/2000JD000226</idno><idno type="ArticleID">2000JD000226</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0148-0227</idno></seriesStmt></fileDesc><profileDesc><textClass></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract">Vertical profile measurements of aerosol particle size distributions and of meteorological parameters (obtained from aircraft, radiosondes, and lidar) are used as input to a spectral radiative transfer model to calculate broadband solar and spectral surface insolations. The calculated values are compared to measured ones gathered with broadband solar pyranometers and pyrheliometers, and a fixed‐grating photodiode array spectroradiometer with 512 spectral channels between 500 and 920 nm wavelength. The measurements were obtained during the joint field campaign Lindenberg Aerosol Characterization Experiment (LACE) 98 near Berlin/Germany in the summer of 1998. Two cases (days with high and low aerosol loading, respectively) are investigated in detail. Furthermore, a measurement‐based sensitivity analysis was carried out focusing on the influence of particle composition (complex refractive index) and of microphysical and humidity growth uncertainties on the calculated surface insolations. Assuming a spectral refractive index of ammonium sulfate for the aerosol particles, on average the global component of the broadband solar surface insolations is 11–20 W m−2 (2–3%) greater than the measured values; the direct portion is 17–28 W m−2 (4–5%) higher, and its diffuse component is 6–7 W m−2 (4–10%) lower in comparison to the measurements. The measured and calculated spectral surface insolations (global portion) agree well in the central visible spectral region (500–600 nm wavelength). Toward larger wavelengths (near infrared) the calculated spectral surface insolations are increasingly higher than the measured ones.</div></front></TEI><istex><corpusName>wiley</corpusName><author><json:item><name>Manfred Wendisch</name><affiliations><json:string>Institute for Tropospheric Research, Leipzig, Germany</json:string></affiliations></json:item><json:item><name>Andreas Keil</name><affiliations><json:string>Institute for Tropospheric Research, Leipzig, Germany</json:string><json:string>Now at Met Office, Farnborough, UK.</json:string></affiliations></json:item><json:item><name>Dörthe Müller</name><affiliations><json:string>Institute for Tropospheric Research, Leipzig, Germany</json:string></affiliations></json:item><json:item><name>Ulla Wandinger</name><affiliations><json:string>Institute for Tropospheric Research, Leipzig, Germany</json:string></affiliations></json:item><json:item><name>Peter Wendling</name><affiliations><json:string>Institute for Physics of the Atmosphere, Oberpfaffenhofen, Germany</json:string></affiliations></json:item><json:item><name>Armin Stifter</name><affiliations><json:string>Institute for Physics of the Atmosphere, Oberpfaffenhofen, Germany</json:string></affiliations></json:item><json:item><name>Andreas Petzold</name><affiliations><json:string>Institute for Physics of the Atmosphere, Oberpfaffenhofen, Germany</json:string></affiliations></json:item><json:item><name>Markus Fiebig</name><affiliations><json:string>Institute for Physics of the Atmosphere, Oberpfaffenhofen, Germany</json:string></affiliations></json:item><json:item><name>Matthias Wiegner</name><affiliations><json:string>Meteorological Institute, University of Munich, Munich, Germany</json:string></affiliations></json:item><json:item><name>Volker Freudenthaler</name><affiliations><json:string>Meteorological Institute, University of Munich, Munich, Germany</json:string></affiliations></json:item><json:item><name>Wolfgang Armbruster</name><affiliations><json:string>Institute for Space Research, Free University of Berlin, Berlin, Germany</json:string><json:string>Now at Department of Optics of the Atmosphere and Meteorology. Research Society for Applied Natural Sciences, Ettlingen, Germany.</json:string></affiliations></json:item><json:item><name>Wolfgang von Hoyningen‐Huene</name><affiliations><json:string>Institute for Remote Sensing, University of Bremen, Bremen, Germany</json:string></affiliations></json:item><json:item><name>Ulrich Leiterer</name><affiliations><json:string>Meteorological Observatory, German Weather Service, Lindenberg, Germany</json:string></affiliations></json:item></author><language><json:string>eng</json:string></language><abstract>Vertical profile measurements of aerosol particle size distributions and of meteorological parameters (obtained from aircraft, radiosondes, and lidar) are used as input to a spectral radiative transfer model to calculate broadband solar and spectral surface insolations. The calculated values are compared to measured ones gathered with broadband solar pyranometers and pyrheliometers, and a fixed‐grating photodiode array spectroradiometer with 512 spectral channels between 500 and 920 nm wavelength. The measurements were obtained during the joint field campaign Lindenberg Aerosol Characterization Experiment (LACE) 98 near Berlin/Germany in the summer of 1998. Two cases (days with high and low aerosol loading, respectively) are investigated in detail. Furthermore, a measurement‐based sensitivity analysis was carried out focusing on the influence of particle composition (complex refractive index) and of microphysical and humidity growth uncertainties on the calculated surface insolations. Assuming a spectral refractive index of ammonium sulfate for the aerosol particles, on average the global component of the broadband solar surface insolations is 11–20 W m−2 (2–3%) greater than the measured values; the direct portion is 17–28 W m−2 (4–5%) higher, and its diffuse component is 6–7 W m−2 (4–10%) lower in comparison to the measurements. The measured and calculated spectral surface insolations (global portion) agree well in the central visible spectral region (500–600 nm wavelength). Toward larger wavelengths (near infrared) the calculated spectral surface insolations are increasingly higher than the measured ones.</abstract><qualityIndicators><score>8.224</score><pdfVersion>1.4</pdfVersion><pdfPageSize>592 x 807 pts</pdfPageSize><refBibsNative>true</refBibsNative><keywordCount>0</keywordCount><abstractCharCount>1634</abstractCharCount><pdfWordCount>14046</pdfWordCount><pdfCharCount>90680</pdfCharCount><pdfPageCount>20</pdfPageCount><abstractWordCount>227</abstractWordCount></qualityIndicators><title>Aerosol‐radiation interaction in the cloudless atmosphere during LACE 98 1. Measured and calculated broadband solar and spectral surface insolations</title><genre><json:string>article</json:string></genre><host><volume>107</volume><pages><total>20</total><last>LAC 6-20</last><first>LAC 6-1</first></pages><issn><json:string>0148-0227</json:string></issn><issue>D21</issue><subject><json:item><value>Lindenberg Aerosol Characterization Experiments (LACE)</value></json:item><json:item><value>Aerosol and Clouds</value></json:item><json:item><value>ATMOSPHERIC COMPOSITION AND STRUCTURE</value></json:item><json:item><value>Aerosols and particles</value></json:item><json:item><value>Pollution: urban and regional</value></json:item><json:item><value>Troposphere: composition and chemistry</value></json:item><json:item><value>Troposphere: constituent transport and chemistry</value></json:item><json:item><value>Pollution: urban and regional</value></json:item><json:item><value>Aerosols and particles</value></json:item><json:item><value>BIOGEOSCIENCES</value></json:item><json:item><value>Pollution: urban, regional and global</value></json:item><json:item><value>OCEANOGRAPHY: GENERAL</value></json:item><json:item><value>Marine pollution</value></json:item><json:item><value>NATURAL HAZARDS</value></json:item><json:item><value>Megacities and urban environment</value></json:item><json:item><value>OCEANOGRAPHY: BIOLOGICAL AND CHEMICAL</value></json:item><json:item><value>Aerosols</value></json:item><json:item><value>PALEOCEANOGRAPHY</value></json:item><json:item><value>Aerosols</value></json:item><json:item><value>Aerosol and Clouds</value></json:item></subject><genre></genre><language><json:string>unknown</json:string></language><eissn><json:string>2156-2202</json:string></eissn><title>Journal of Geophysical Research: Atmospheres</title><doi><json:string>10.1002/(ISSN)2156-2202d</json:string></doi></host><publicationDate>2002</publicationDate><copyrightDate>2002</copyrightDate><doi><json:string>10.1029/2000JD000226</json:string></doi><id>E56D5E66F1B57EC4A80FBA5AD64DA2EE12767F47</id><fulltext><json:item><original>true</original><mimetype>application/pdf</mimetype><extension>pdf</extension><uri>https://api.istex.fr/document/E56D5E66F1B57EC4A80FBA5AD64DA2EE12767F47/fulltext/pdf</uri></json:item><json:item><original>false</original><mimetype>application/zip</mimetype><extension>zip</extension><uri>https://api.istex.fr/document/E56D5E66F1B57EC4A80FBA5AD64DA2EE12767F47/fulltext/zip</uri></json:item><istex:fulltextTEI uri="https://api.istex.fr/document/E56D5E66F1B57EC4A80FBA5AD64DA2EE12767F47/fulltext/tei"><teiHeader><fileDesc><titleStmt><title level="a" type="main" xml:lang="en">Aerosol‐radiation interaction in the cloudless atmosphere during LACE 98 1. 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Measured and calculated broadband solar and spectral surface insolations</title><author><persName><forename type="first">Manfred</forename><surname>Wendisch</surname></persName><affiliation>Institute for Tropospheric Research, Leipzig, Germany</affiliation></author><author><persName><forename type="first">Andreas</forename><surname>Keil</surname></persName><affiliation>Institute for Tropospheric Research, Leipzig, Germany</affiliation><affiliation>Now at Met Office, Farnborough, UK.</affiliation></author><author><persName><forename type="first">Dörthe</forename><surname>Müller</surname></persName><affiliation>Institute for Tropospheric Research, Leipzig, Germany</affiliation></author><author><persName><forename type="first">Ulla</forename><surname>Wandinger</surname></persName><affiliation>Institute for Tropospheric Research, Leipzig, Germany</affiliation></author><author><persName><forename type="first">Peter</forename><surname>Wendling</surname></persName><affiliation>Institute for Physics of the Atmosphere, Oberpfaffenhofen, Germany</affiliation></author><author><persName><forename type="first">Armin</forename><surname>Stifter</surname></persName><affiliation>Institute for Physics of the Atmosphere, Oberpfaffenhofen, Germany</affiliation></author><author><persName><forename type="first">Andreas</forename><surname>Petzold</surname></persName><affiliation>Institute for Physics of the Atmosphere, Oberpfaffenhofen, Germany</affiliation></author><author><persName><forename type="first">Markus</forename><surname>Fiebig</surname></persName><affiliation>Institute for Physics of the Atmosphere, Oberpfaffenhofen, Germany</affiliation></author><author><persName><forename type="first">Matthias</forename><surname>Wiegner</surname></persName><affiliation>Meteorological Institute, University of Munich, Munich, Germany</affiliation></author><author><persName><forename type="first">Volker</forename><surname>Freudenthaler</surname></persName><affiliation>Meteorological Institute, University of Munich, Munich, Germany</affiliation></author><author><persName><forename type="first">Wolfgang</forename><surname>Armbruster</surname></persName><affiliation>Institute for Space Research, Free University of Berlin, Berlin, Germany</affiliation><affiliation>Now at Department of Optics of the Atmosphere and Meteorology. Research Society for Applied Natural Sciences, Ettlingen, Germany.</affiliation></author><author><persName><forename type="first">Wolfgang</forename><surname>von Hoyningen‐Huene</surname></persName><affiliation>Institute for Remote Sensing, University of Bremen, Bremen, Germany</affiliation></author><author><persName><forename type="first">Ulrich</forename><surname>Leiterer</surname></persName><affiliation>Meteorological Observatory, German Weather Service, Lindenberg, Germany</affiliation></author></analytic><monogr><title level="j">Journal of Geophysical Research: Atmospheres</title><title level="j" type="abbrev">J. Geophys. Res.</title><idno type="pISSN">0148-0227</idno><idno type="eISSN">2156-2202</idno><idno type="DOI">10.1002/(ISSN)2156-2202d</idno><imprint><publisher>Blackwell Publishing Ltd</publisher><date type="published" when="2002-11-16"></date><biblScope unit="volume">107</biblScope><biblScope unit="issue">D21</biblScope><biblScope unit="page" from="LAC 6-1">LAC 6-1</biblScope><biblScope unit="page" to="LAC 6-20">LAC 6-20</biblScope></imprint></monogr><idno type="istex">E56D5E66F1B57EC4A80FBA5AD64DA2EE12767F47</idno><idno type="DOI">10.1029/2000JD000226</idno><idno type="ArticleID">2000JD000226</idno></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>2002</date></creation><langUsage><language ident="en">en</language></langUsage><abstract><p>Vertical profile measurements of aerosol particle size distributions and of meteorological parameters (obtained from aircraft, radiosondes, and lidar) are used as input to a spectral radiative transfer model to calculate broadband solar and spectral surface insolations. The calculated values are compared to measured ones gathered with broadband solar pyranometers and pyrheliometers, and a fixed‐grating photodiode array spectroradiometer with 512 spectral channels between 500 and 920 nm wavelength. The measurements were obtained during the joint field campaign Lindenberg Aerosol Characterization Experiment (LACE) 98 near Berlin/Germany in the summer of 1998. Two cases (days with high and low aerosol loading, respectively) are investigated in detail. Furthermore, a measurement‐based sensitivity analysis was carried out focusing on the influence of particle composition (complex refractive index) and of microphysical and humidity growth uncertainties on the calculated surface insolations. Assuming a spectral refractive index of ammonium sulfate for the aerosol particles, on average the global component of the broadband solar surface insolations is 11–20 W m−2 (2–3%) greater than the measured values; the direct portion is 17–28 W m−2 (4–5%) higher, and its diffuse component is 6–7 W m−2 (4–10%) lower in comparison to the measurements. The measured and calculated spectral surface insolations (global portion) agree well in the central visible spectral region (500–600 nm wavelength). Toward larger wavelengths (near infrared) the calculated spectral surface insolations are increasingly higher than the measured ones.</p></abstract><textClass><keywords scheme="Journal Subject"><list><head>Index Terms</head><item><term>Lindenberg Aerosol Characterization Experiments (LACE)</term></item><item><term>Aerosol and Clouds</term></item><item><term>ATMOSPHERIC COMPOSITION AND STRUCTURE</term></item><item><term>Aerosols and particles</term></item><item><term>Pollution: urban and regional</term></item><item><term>Troposphere: composition and chemistry</term></item><item><term>Troposphere: constituent transport and chemistry</term></item><item><term>Pollution: urban and regional</term></item><item><term>Aerosols and particles</term></item><item><term>BIOGEOSCIENCES</term></item><item><term>Pollution: urban, regional and global</term></item><item><term>OCEANOGRAPHY: GENERAL</term></item><item><term>Marine pollution</term></item><item><term>NATURAL HAZARDS</term></item><item><term>Megacities and urban environment</term></item><item><term>OCEANOGRAPHY: BIOLOGICAL AND CHEMICAL</term></item><item><term>Aerosols</term></item><item><term>PALEOCEANOGRAPHY</term></item><item><term>Aerosols</term></item></list></keywords></textClass><textClass><keywords scheme="Journal Subject"><list><head>article category</head><item><term>Aerosol and Clouds</term></item></list></keywords></textClass></profileDesc><revisionDesc><change when="2000-12-06">Received</change><change when="2001-11-01">Registration</change><change when="2002-11-16">Published</change></revisionDesc></teiHeader></istex:fulltextTEI><json:item><original>false</original><mimetype>text/plain</mimetype><extension>txt</extension><uri>https://api.istex.fr/document/E56D5E66F1B57EC4A80FBA5AD64DA2EE12767F47/fulltext/txt</uri></json:item></fulltext><metadata><istex:metadataXml wicri:clean="Wiley, elements deleted: body"><istex:xmlDeclaration>version="1.0" encoding="UTF-8" standalone="yes"</istex:xmlDeclaration><istex:document><component type="serialArticle" version="2.0" xml:lang="en" xml:id="jgrd8698"><header><publicationMeta level="product"><doi>10.1002/(ISSN)2156-2202d</doi><issn type="print">0148-0227</issn><issn type="electronic">2156-2202</issn><idGroup><id type="product" value="JGRD"></id><id type="coden" value="JGREA2"></id></idGroup><titleGroup><title type="main" xml:lang="en" sort="JOURNAL OF GEOPHYSICAL RESEARCH: ATMOSPHERES">Journal of Geophysical Research: Atmospheres</title><title type="short">J. Geophys. Res.</title></titleGroup></publicationMeta><publicationMeta level="part" position="210"><doi>10.1002/jgrd.v107.D21</doi><idGroup><id type="focusSection" value="4"></id></idGroup><titleGroup><title type="focusSection" xml:lang="en">Journal of Geophysical Research: Atmospheres</title></titleGroup><numberingGroup><numbering type="journalVolume" number="107">107</numbering><numbering type="journalIssue">D21</numbering></numberingGroup><coverDate startDate="2002-11-16">16 November 2002</coverDate></publicationMeta><publicationMeta level="unit" position="780" type="article" status="forIssue"><doi>10.1029/2000JD000226</doi><idGroup><id type="editorialOffice" value="2000JD000226"></id><id type="society" value="8124"></id><id type="unit" value="JGRD8698"></id></idGroup><countGroup><count type="pageTotal" number="20"></count></countGroup><titleGroup><title type="articleCategory">Aerosol and Clouds</title><title type="tocHeading1">Aerosol and Clouds</title></titleGroup><copyright ownership="thirdParty">Copyright 2002 by the American Geophysical Union.</copyright><eventGroup><event type="manuscriptReceived" date="2000-12-06"></event><event type="manuscriptRevised" date="2001-10-29"></event><event type="manuscriptAccepted" date="2001-11-01"></event><event type="firstOnline" date="2002-09-13"></event><event type="publishedOnlineFinalForm" date="2002-09-13"></event><event type="xmlConverted" agent="SPi Global Converter:AGUv3.21_TO_WileyML3Gv1.0.3 version:1.1; 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Measured and calculated broadband solar and spectral surface insolations</articleTitle>, <journalTitle>J. Geophys. Res.</journalTitle>, <vol>107</vol>(<issue>D21</issue>), 8124, doi:<accessionId ref="info:doi/10.1029/2000JD000226">10.1029/2000JD000226</accessionId>, <pubYear year="2002">2002</pubYear>.</citation></selfCitationGroup><linkGroup><link type="toTypesetVersion" href="file:JGRD.JGRD8698.pdf"></link></linkGroup></publicationMeta><contentMeta><countGroup><count type="figureTotal" number="6"></count><count type="tableTotal" number="4"></count></countGroup><titleGroup><title type="main">Aerosol‐radiation interaction in the cloudless atmosphere during LACE 98 1. Measured and calculated broadband solar and spectral surface insolations</title><title type="short">MEASURED AND CALCULATED SURFACE INSOLATIONS</title><title type="shortAuthors">Wendisch <i>et al</i>.</title></titleGroup><creators><creator creatorRole="author" xml:id="jgrd8698-cr-0001" affiliationRef="#jgrd8698-aff-0001"><personName><givenNames>Manfred</givenNames> <familyName>Wendisch</familyName></personName></creator><creator creatorRole="author" xml:id="jgrd8698-cr-0002" affiliationRef="#jgrd8698-aff-0001 #jgrd8698-aff-0007"><personName><givenNames>Andreas</givenNames> <familyName>Keil</familyName></personName></creator><creator creatorRole="author" xml:id="jgrd8698-cr-0003" affiliationRef="#jgrd8698-aff-0001"><personName><givenNames>Dörthe</givenNames> <familyName>Müller</familyName></personName></creator><creator creatorRole="author" xml:id="jgrd8698-cr-0004" affiliationRef="#jgrd8698-aff-0001"><personName><givenNames>Ulla</givenNames> <familyName>Wandinger</familyName></personName></creator><creator creatorRole="author" xml:id="jgrd8698-cr-0005" affiliationRef="#jgrd8698-aff-0002"><personName><givenNames>Peter</givenNames> <familyName>Wendling</familyName></personName></creator><creator creatorRole="author" xml:id="jgrd8698-cr-0006" affiliationRef="#jgrd8698-aff-0002"><personName><givenNames>Armin</givenNames> <familyName>Stifter</familyName></personName></creator><creator creatorRole="author" xml:id="jgrd8698-cr-0007" affiliationRef="#jgrd8698-aff-0002"><personName><givenNames>Andreas</givenNames> <familyName>Petzold</familyName></personName></creator><creator creatorRole="author" xml:id="jgrd8698-cr-0008" affiliationRef="#jgrd8698-aff-0002"><personName><givenNames>Markus</givenNames> <familyName>Fiebig</familyName></personName></creator><creator creatorRole="author" xml:id="jgrd8698-cr-0009" affiliationRef="#jgrd8698-aff-0003"><personName><givenNames>Matthias</givenNames> <familyName>Wiegner</familyName></personName></creator><creator creatorRole="author" xml:id="jgrd8698-cr-0010" affiliationRef="#jgrd8698-aff-0003"><personName><givenNames>Volker</givenNames> <familyName>Freudenthaler</familyName></personName></creator><creator creatorRole="author" xml:id="jgrd8698-cr-0011" affiliationRef="#jgrd8698-aff-0004 #jgrd8698-aff-0008"><personName><givenNames>Wolfgang</givenNames> <familyName>Armbruster</familyName></personName></creator><creator creatorRole="author" xml:id="jgrd8698-cr-0012" affiliationRef="#jgrd8698-aff-0005"><personName><givenNames>Wolfgang</givenNames> <familyName>von Hoyningen‐Huene</familyName></personName></creator><creator creatorRole="author" xml:id="jgrd8698-cr-0013" affiliationRef="#jgrd8698-aff-0006"><personName><givenNames>Ulrich</givenNames> <familyName>Leiterer</familyName></personName></creator></creators><affiliationGroup><affiliation countryCode="DE" type="organization" xml:id="jgrd8698-aff-0001"><orgName>Institute for Tropospheric Research</orgName><address><city>Leipzig</city><country>Germany</country></address></affiliation><affiliation countryCode="DE" type="organization" xml:id="jgrd8698-aff-0002"><orgName>Institute for Physics of the Atmosphere</orgName><address><city>Oberpfaffenhofen</city><country>Germany</country></address></affiliation><affiliation countryCode="DE" type="organization" xml:id="jgrd8698-aff-0003"><orgDiv>Meteorological Institute</orgDiv><orgName>University of Munich</orgName><address><city>Munich</city><country>Germany</country></address></affiliation><affiliation countryCode="DE" type="organization" xml:id="jgrd8698-aff-0004"><orgDiv>Institute for Space Research</orgDiv><orgName>Free University of Berlin</orgName><address><city>Berlin</city><country>Germany</country></address></affiliation><affiliation countryCode="DE" type="organization" xml:id="jgrd8698-aff-0005"><orgDiv>Institute for Remote Sensing</orgDiv><orgName>University of Bremen</orgName><address><city>Bremen</city><country>Germany</country></address></affiliation><affiliation countryCode="DE" type="organization" xml:id="jgrd8698-aff-0006"><orgDiv>Meteorological Observatory</orgDiv><orgName>German Weather Service</orgName><address><city>Lindenberg</city><country>Germany</country></address></affiliation><affiliation type="organization" xml:id="jgrd8698-aff-0007"><unparsedAffiliation>Now at Met Office, Farnborough, UK.</unparsedAffiliation></affiliation><affiliation type="organization" xml:id="jgrd8698-aff-0008"><unparsedAffiliation>Now at Department of Optics of the Atmosphere and Meteorology. Research Society for Applied Natural Sciences, Ettlingen, Germany.</unparsedAffiliation></affiliation></affiliationGroup><abstractGroup><abstract type="main"><p xml:id="jgrd8698-para-0001" label="1">Vertical profile measurements of aerosol particle size distributions and of meteorological parameters (obtained from aircraft, radiosondes, and lidar) are used as input to a spectral radiative transfer model to calculate broadband solar and spectral surface insolations. The calculated values are compared to measured ones gathered with broadband solar pyranometers and pyrheliometers, and a fixed‐grating photodiode array spectroradiometer with 512 spectral channels between 500 and 920 nm wavelength. The measurements were obtained during the joint field campaign Lindenberg Aerosol Characterization Experiment (LACE) 98 near Berlin/Germany in the summer of 1998. Two cases (days with high and low aerosol loading, respectively) are investigated in detail. Furthermore, a measurement‐based sensitivity analysis was carried out focusing on the influence of particle composition (complex refractive index) and of microphysical and humidity growth uncertainties on the calculated surface insolations. Assuming a spectral refractive index of ammonium sulfate for the aerosol particles, on average the global component of the broadband solar surface insolations is 11–20 W m<sup>−2</sup> (2–3%) greater than the measured values; the direct portion is 17–28 W m<sup>−2</sup> (4–5%) higher, and its diffuse component is 6–7 W m<sup>−2</sup> (4–10%) lower in comparison to the measurements. The measured and calculated spectral surface insolations (global portion) agree well in the central visible spectral region (500–600 nm wavelength). Toward larger wavelengths (near infrared) the calculated spectral surface insolations are increasingly higher than the measured ones.</p></abstract></abstractGroup></contentMeta></header></component></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>Aerosol‐radiation interaction in the cloudless atmosphere during LACE 98 1. Measured and calculated broadband solar and spectral surface insolations</title></titleInfo><titleInfo type="abbreviated"><title>MEASURED AND CALCULATED SURFACE INSOLATIONS</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>Aerosol‐radiation interaction in the cloudless atmosphere during LACE 98 1. Measured and calculated broadband solar and spectral surface insolations</title></titleInfo><name type="personal"><namePart type="given">Manfred</namePart><namePart type="family">Wendisch</namePart><affiliation>Institute for Tropospheric Research, Leipzig, Germany</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Andreas</namePart><namePart type="family">Keil</namePart><affiliation>Institute for Tropospheric Research, Leipzig, Germany</affiliation><affiliation>Now at Met Office, Farnborough, UK.</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Dörthe</namePart><namePart type="family">Müller</namePart><affiliation>Institute for Tropospheric Research, Leipzig, Germany</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Ulla</namePart><namePart type="family">Wandinger</namePart><affiliation>Institute for Tropospheric Research, Leipzig, Germany</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Peter</namePart><namePart type="family">Wendling</namePart><affiliation>Institute for Physics of the Atmosphere, Oberpfaffenhofen, Germany</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Armin</namePart><namePart type="family">Stifter</namePart><affiliation>Institute for Physics of the Atmosphere, Oberpfaffenhofen, Germany</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Andreas</namePart><namePart type="family">Petzold</namePart><affiliation>Institute for Physics of the Atmosphere, Oberpfaffenhofen, Germany</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Markus</namePart><namePart type="family">Fiebig</namePart><affiliation>Institute for Physics of the Atmosphere, Oberpfaffenhofen, Germany</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Matthias</namePart><namePart type="family">Wiegner</namePart><affiliation>Meteorological Institute, University of Munich, Munich, Germany</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Volker</namePart><namePart type="family">Freudenthaler</namePart><affiliation>Meteorological Institute, University of Munich, Munich, Germany</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Wolfgang</namePart><namePart type="family">Armbruster</namePart><affiliation>Institute for Space Research, Free University of Berlin, Berlin, Germany</affiliation><affiliation>Now at Department of Optics of the Atmosphere and Meteorology. Research Society for Applied Natural Sciences, Ettlingen, Germany.</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Wolfgang</namePart><namePart type="family">von Hoyningen‐Huene</namePart><affiliation>Institute for Remote Sensing, University of Bremen, Bremen, Germany</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Ulrich</namePart><namePart type="family">Leiterer</namePart><affiliation>Meteorological Observatory, German Weather Service, Lindenberg, Germany</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="article" displayLabel="article"></genre><originInfo><publisher>Blackwell Publishing Ltd</publisher><dateIssued encoding="w3cdtf">2002-11-16</dateIssued><dateCaptured encoding="w3cdtf">2000-12-06</dateCaptured><dateValid encoding="w3cdtf">2001-11-01</dateValid><edition>Wendisch, M., A. Keil, D. Mueller, U. Wandinger, P. Wendling, A. Stifter, A. Petzold, M. Fiebig, M. Wiegner, V. Freudenthaler, W. Armbruster, W. von Hoyningen‐Huene, and U. Leiterer, Aerosol‐radiation interaction in the cloudless atmosphere during LACE 98, 1. Measured and calculated broadband solar and spectral surface insolations, J. Geophys. Res., 107(D21), 8124, doi:10.1029/2000JD000226, 2002.</edition><copyrightDate encoding="w3cdtf">2002</copyrightDate></originInfo><language><languageTerm type="code" authority="rfc3066">en</languageTerm><languageTerm type="code" authority="iso639-2b">eng</languageTerm></language><physicalDescription><internetMediaType>text/html</internetMediaType><extent unit="figures">6</extent><extent unit="tables">4</extent></physicalDescription><abstract>Vertical profile measurements of aerosol particle size distributions and of meteorological parameters (obtained from aircraft, radiosondes, and lidar) are used as input to a spectral radiative transfer model to calculate broadband solar and spectral surface insolations. The calculated values are compared to measured ones gathered with broadband solar pyranometers and pyrheliometers, and a fixed‐grating photodiode array spectroradiometer with 512 spectral channels between 500 and 920 nm wavelength. The measurements were obtained during the joint field campaign Lindenberg Aerosol Characterization Experiment (LACE) 98 near Berlin/Germany in the summer of 1998. Two cases (days with high and low aerosol loading, respectively) are investigated in detail. Furthermore, a measurement‐based sensitivity analysis was carried out focusing on the influence of particle composition (complex refractive index) and of microphysical and humidity growth uncertainties on the calculated surface insolations. Assuming a spectral refractive index of ammonium sulfate for the aerosol particles, on average the global component of the broadband solar surface insolations is 11–20 W m−2 (2–3%) greater than the measured values; the direct portion is 17–28 W m−2 (4–5%) higher, and its diffuse component is 6–7 W m−2 (4–10%) lower in comparison to the measurements. The measured and calculated spectral surface insolations (global portion) agree well in the central visible spectral region (500–600 nm wavelength). Toward larger wavelengths (near infrared) the calculated spectral surface insolations are increasingly higher than the measured ones.</abstract><relatedItem type="host"><titleInfo><title>Journal of Geophysical Research: Atmospheres</title></titleInfo><titleInfo type="abbreviated"><title>J. Geophys. Res.</title></titleInfo><genre type="Journal">journal</genre><subject><genre>Index Terms</genre><topic authorityURI="http://psi.agu.org/specialSection/LACE1">Lindenberg Aerosol Characterization Experiments (LACE)</topic><topic authorityURI="http://psi.agu.org/subset/AAC">Aerosol and Clouds</topic><topic authorityURI="http://psi.agu.org/taxonomy5/0300">ATMOSPHERIC COMPOSITION AND STRUCTURE</topic><topic authorityURI="http://psi.agu.org/taxonomy5/0305">Aerosols and particles</topic><topic authorityURI="http://psi.agu.org/taxonomy5/0345">Pollution: urban and regional</topic><topic authorityURI="http://psi.agu.org/taxonomy5/0365">Troposphere: composition and chemistry</topic><topic authorityURI="http://psi.agu.org/taxonomy5/0368">Troposphere: constituent transport and chemistry</topic><topic authorityURI="http://psi.agu.org/taxonomy5/0345">Pollution: urban and regional</topic><topic authorityURI="http://psi.agu.org/taxonomy5/0305">Aerosols and particles</topic><topic authorityURI="http://psi.agu.org/taxonomy5/0400">BIOGEOSCIENCES</topic><topic authorityURI="http://psi.agu.org/taxonomy5/0478">Pollution: urban, regional and global</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4200">OCEANOGRAPHY: GENERAL</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4251">Marine pollution</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4300">NATURAL HAZARDS</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4325">Megacities and urban environment</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4800">OCEANOGRAPHY: BIOLOGICAL AND CHEMICAL</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4801">Aerosols</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4900">PALEOCEANOGRAPHY</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4906">Aerosols</topic></subject><subject><genre>article category</genre><topic>Aerosol and Clouds</topic></subject><identifier type="ISSN">0148-0227</identifier><identifier type="eISSN">2156-2202</identifier><identifier type="DOI">10.1002/(ISSN)2156-2202d</identifier><identifier type="CODEN">JGREA2</identifier><identifier type="PublisherID">JGRD</identifier><part><date>2002</date><detail type="volume"><caption>vol.</caption><number>107</number></detail><detail type="issue"><caption>no.</caption><number>D21</number></detail><extent unit="pages"><start>LAC 6-1</start><end>LAC 6-20</end><total>20</total></extent></part></relatedItem><identifier type="istex">E56D5E66F1B57EC4A80FBA5AD64DA2EE12767F47</identifier><identifier type="DOI">10.1029/2000JD000226</identifier><identifier type="ArticleID">2000JD000226</identifier><accessCondition type="use and reproduction" contentType="copyright">Copyright 2002 by the American Geophysical Union.</accessCondition><recordInfo><recordContentSource>WILEY</recordContentSource></recordInfo></mods></metadata><serie></serie></istex></record>Pour manipuler ce document sous Unix (Dilib)
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