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dc.contributor.authorClerbaux, N.
dc.contributor.authorBertrand, C.
dc.contributor.authorDewitte, S.
dc.contributor.authorGonzalez, L.
dc.contributor.authorIpe, A.
dc.contributor.authorNicula, B.
dc.coverage.temporal21st century
dc.date2002
dc.date.accessioned2016-03-07T17:14:22Z
dc.date.accessioned2021-12-09T09:53:21Z
dc.date.available2016-03-07T17:14:22Z
dc.date.available2021-12-09T09:53:21Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/8631
dc.descriptionThe analysis of one year of CERES{Terra data provides further evidence that the longwave radiation escaping from the atmosphere exhibits signi cant variability according to the azimuthal angle of observation. A regional analysis of this variability shows that the anisotropy in azimuth is maximum over mountain and desert areas and under cloud{free conditions. A relative di erence between North and South views of about 5% in annual average is observed over the Himalayan region in the 8 􀀀 14 m infrared window. We think that the remote sensing community should be aware of this variability, in particular when analyzing infrared data provided by instruments on geostationary orbits. Indeed, in this case, the azimuthal anisotropy may lead to systematic overestimation of the outgoing longwave radiation and to biases on retrieved quantities such as the surface temperature.
dc.languageeng
dc.publisherIRM
dc.publisherKMI
dc.publisherRMI
dc.relation.ispartofseriesIn Proceedings of The 2002 EUMETSAT Meteorological Satellite Conference, Dubin, Ireland, 2-6 September 2002
dc.title"Regional Bias in the OLR Estimated from the Geostationary Orbit"
dc.typeArticle
dc.subject.frascatiEarth and related Environmental sciences
dc.audienceGeneral Public
dc.audienceScientific
dc.subject.freeOLR Geostationary Orbit
dc.source.issueIn Proceedings of The 2002 EUMETSAT Meteorological Satellite Conference, Dubin, Ireland, 2-6 September 2002
dc.source.pagepp. 677-681
Orfeo.peerreviewedNot pertinent


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