<?xml version="1.0" encoding="UTF-8"?><?xml-stylesheet type="text/xsl" href="static/style.xsl"?><OAI-PMH xmlns="http://www.openarchives.org/OAI/2.0/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd"><responseDate>2026-04-17T01:00:39Z</responseDate><request verb="GetRecord" identifier="oai:www.recercat.cat:10256/20807" metadataPrefix="mets">https://recercat.cat/oai/request</request><GetRecord><record><header><identifier>oai:recercat.cat:10256/20807</identifier><datestamp>2024-06-18T11:51:28Z</datestamp><setSpec>com_2072_452955</setSpec><setSpec>com_2072_2054</setSpec><setSpec>col_2072_453063</setSpec></header><metadata><mets xmlns="http://www.loc.gov/METS/" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:doc="http://www.lyncode.com/xoai" ID="&#xa;&#x9;&#x9;&#x9;&#x9;DSpace_ITEM_10256-20807" TYPE="DSpace ITEM" PROFILE="DSpace METS SIP Profile 1.0" xsi:schemaLocation="http://www.loc.gov/METS/ http://www.loc.gov/standards/mets/mets.xsd" OBJID="&#xa;&#x9;&#x9;&#x9;&#x9;hdl:10256/20807">
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               <mods:name>
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                     <mods:roleTerm type="text">author</mods:roleTerm>
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                  <mods:namePart>Jahani, Babak</mods:namePart>
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               <mods:name>
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                  <mods:namePart>Andersen, Hendrik</mods:namePart>
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               <mods:name>
                  <mods:role>
                     <mods:roleTerm type="text">author</mods:roleTerm>
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                  <mods:namePart>Calbó Angrill, Josep</mods:namePart>
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               <mods:name>
                  <mods:role>
                     <mods:roleTerm type="text">author</mods:roleTerm>
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                  <mods:namePart>González Gutiérrez, Josep Abel</mods:namePart>
               </mods:name>
               <mods:name>
                  <mods:role>
                     <mods:roleTerm type="text">author</mods:roleTerm>
                  </mods:role>
                  <mods:namePart>Cermak, Jan</mods:namePart>
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               <mods:extension>
                  <mods:dateAccessioned encoding="iso8601">2024-06-18T11:51:28Z</mods:dateAccessioned>
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                  <mods:dateAvailable encoding="iso8601">2024-06-18T11:51:28Z</mods:dateAvailable>
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                  <mods:dateIssued encoding="iso8601">2022-01-31</mods:dateIssued>
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               <mods:identifier type="none"/>
               <mods:identifier type="uri">http://hdl.handle.net/10256/20807</mods:identifier>
               <mods:abstract>This study presents an approach for the quantification of cloud–aerosol transition-zone broadband&#xd;
longwave radiative effects at the top of the atmosphere (TOA) during daytime over the ocean, based on satellite&#xd;
observations and radiative transfer simulation. Specifically, we used several products from MODIS (MODerate&#xd;
Resolution Imaging Spectroradiometer) and CERES (Clouds and the Earth’s Radiant Energy System) sensors&#xd;
for the identification and selection of CERES footprints with a horizontally homogeneous transition-zone and&#xd;
clear-sky conditions. For the selected transition-zone footprints, radiative effect was calculated as the difference&#xd;
between the instantaneous CERES TOA upwelling broadband longwave radiance observations and corresponding clear-sky radiance simulations. The clear-sky radiances were simulated using the Santa Barbara DISORT&#xd;
(DIScrete Ordinates Radiative Transfer program for a multi-Layered plane-parallel medium) Atmospheric Radiative Transfer model fed by the hourly ERA5 reanalysis (fifth generation ECMWF ReAnalysis) atmospheric&#xd;
and surface data. The CERES radiance observations corresponding to the clear-sky footprints detected were also&#xd;
used for validating the simulated clear-sky radiances. We tested this approach using the radiative measurements&#xd;
made by the MODIS and CERES instruments on board the Aqua platform over the southeastern Atlantic Ocean&#xd;
during August 2010. For the studied period and domain, transition-zone radiative effect (given in flux units) is&#xd;
on average equal to 8.0 ± 3.7 W m−2&#xd;
(heating effect; median: 5.4 W m−2&#xd;
), although cases with radiative effects&#xd;
as large as 50 W m−2 were foundThis research has been supported by the Ministerio de Ciencia e Innovación (grant no. PID2019-105901RB-I00) and the Generalitat de Catalunya (grant no. 2018FI_B_00830).</mods:abstract>
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               <mods:accessCondition type="useAndReproduction">Attribution 4.0 International http://creativecommons.org/licenses/by/4.0/ info:eu-repo/semantics/openAccess</mods:accessCondition>
               <mods:subject>
                  <mods:topic>Radiació -- Mesurament</mods:topic>
               </mods:subject>
               <mods:subject>
                  <mods:topic>Radiation -- Measurement</mods:topic>
               </mods:subject>
               <mods:subject>
                  <mods:topic>Radiació atmosfèrica</mods:topic>
               </mods:subject>
               <mods:subject>
                  <mods:topic>Atmospheric radiation</mods:topic>
               </mods:subject>
               <mods:titleInfo>
                  <mods:title>Longwave radiative effect of the cloud–aerosol transition zone based on CERES observations</mods:title>
               </mods:titleInfo>
               <mods:genre>info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion peer-reviewed</mods:genre>
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