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dc.contributor.authorKruglanski, M.
dc.contributor.authorDe Mazière, M.
dc.contributor.authorVandaele, A.C.
dc.contributor.authorHurtmans, D.
dc.date2006
dc.date.accessioned2016-11-21T13:46:13Z
dc.date.available2016-11-21T13:46:13Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/4474
dc.descriptionA non-empirical algorithm is presented to retrieve the optical depth in the 750-1250 cm -1 spectral range, of aerosol located in the boundary layer over the ocean, from nadir high-resolution radiance spectra in the thermal infrared. The algorithm is based on a line-by-line radiative transfer forward model and used the Optimal Estimation Method for the retrieval. Its performance strongly depends on the quality of the a priori temperature and H 2O atmospheric profiles. To demonstrate the relevance of the algorithm, distributions of maritime aerosol parameters have been retrieved from IMG/ADEOS data for December 1996, using the algorithm with the LBLRTM radiative transfer code, and ERA40 (ECMWF) a priori atmospheric profiles and surface conditions.
dc.languageeng
dc.titleBoundary layer aerosol retrieval from thermal infrared nadir sounding - Preliminary results
dc.typeArticle
dc.subject.frascatiPhysical sciences
dc.audienceScientific
dc.subject.freeAlgorithms
dc.subject.freeInfrared radiation
dc.subject.freeOptical resolving power
dc.subject.freeRemote sensing
dc.subject.freeSatellites
dc.subject.freeRadiance spectra
dc.subject.freeRadiative transfer
dc.subject.freeRetrieval
dc.subject.freeThermal infrared
dc.subject.freeAerosols
dc.source.titleAdvances in Space Research
dc.source.volume37
dc.source.issue12
dc.source.page2160-2165
Orfeo.peerreviewedYes
dc.identifier.doi10.1016/j.asr.2005.08.032
dc.identifier.scopus2-s2.0-33745737199


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