A reprocessing for climate of sea surface temperature from the Along-Track Scanning Radiometers: basis in radiative transferEmbury, O. ORCID: https://orcid.org/0000-0002-1661-7828, Merchant, C.J. ORCID: https://orcid.org/0000-0003-4687-9850 and Filipiak, M.J. (2012) A reprocessing for climate of sea surface temperature from the Along-Track Scanning Radiometers: basis in radiative transfer. Remote Sensing of Environment, 116. pp. 32-46. ISSN 0034-4257 Full text not archived in this repository. It is advisable to refer to the publisher's version if you intend to cite from this work. See Guidance on citing. To link to this item DOI: 10.1016/j.rse.2010.10.016 Abstract/SummaryWe present new radiative transfer simulations to support determination of sea surface temperature (SST) from Along Track Scanning Radiometer (ATSR) imagery. The simulations are to be used within the ATSR Reprocessing for Climate project. The simulations are based on the “Reference Forward Model” line-by-line model linked with a sea surface emissivity model that accounts for wind speed and temperature, and with a discrete ordinates scattering model (DISORT). Input to the forward model is a revised atmospheric profile dataset, based on full resolution ERA-40, with a wider range of high-latitude profiles to address known retrieval biases in those regions. Analysis of the radiative impacts of atmospheric trace gases shows that geographical and temporal variation of N2O, CH4, HNO3, and CFC-11 and CFC-12 have effects of order 0.05, 0.2, 0.1 K on the 3.7, 11, 12 μm channels respectively. In addition several trace gases, neglected in previous studies, are included using fixed profiles contributing ~ 0.04 K to top-of-atmosphere BTs. Comparison against observations for ATSR2 and AATSR indicates that forward model biases have been reduced from 0.2 to 0.5 K for previous simulations to ~ 0.1 K.
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