GOME aerosol optical depth retrieval over ocean: Correcting for the effects of residual cloud contamination

Aerosol optical depths (AODs) retrieved from GOME reflectances using a clear sky algorithm have been compared to AODs from ground-based sunphotometers. A systematic overestimation of GOME AOD was found, mainly due to the presence of clouds within the GOME field-of-view. In order to take the influenc...

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Main Author: Carboni, E
Format: Journal article
Language:English
Published: 2006
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author Carboni, E
author_facet Carboni, E
author_sort Carboni, E
collection OXFORD
description Aerosol optical depths (AODs) retrieved from GOME reflectances using a clear sky algorithm have been compared to AODs from ground-based sunphotometers. A systematic overestimation of GOME AOD was found, mainly due to the presence of clouds within the GOME field-of-view. In order to take the influence of clouds into account, a model which assumes a linear dependence of AOD on cloud fraction has been tested. This model was validated using independent measurements from different AERONET sites. The monthly averaged maps of corrected AOD show similar spatial behaviour to AVHRR and TOMS maps. The method proposed here produces monthly maps of AOD from GOME data. It is applicable on a statistical analysis (monthly) and is proved to be effective in regions with high AOD, but relatively large uncertainties remain for background marine conditions. © 2006 Elsevier Ltd. All rights reserved.
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spelling oxford-uuid:4939eccb-3486-4d99-9cec-b06892472d762022-03-26T15:30:24ZGOME aerosol optical depth retrieval over ocean: Correcting for the effects of residual cloud contaminationJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:4939eccb-3486-4d99-9cec-b06892472d76EnglishSymplectic Elements at Oxford2006Carboni, EAerosol optical depths (AODs) retrieved from GOME reflectances using a clear sky algorithm have been compared to AODs from ground-based sunphotometers. A systematic overestimation of GOME AOD was found, mainly due to the presence of clouds within the GOME field-of-view. In order to take the influence of clouds into account, a model which assumes a linear dependence of AOD on cloud fraction has been tested. This model was validated using independent measurements from different AERONET sites. The monthly averaged maps of corrected AOD show similar spatial behaviour to AVHRR and TOMS maps. The method proposed here produces monthly maps of AOD from GOME data. It is applicable on a statistical analysis (monthly) and is proved to be effective in regions with high AOD, but relatively large uncertainties remain for background marine conditions. © 2006 Elsevier Ltd. All rights reserved.
spellingShingle Carboni, E
GOME aerosol optical depth retrieval over ocean: Correcting for the effects of residual cloud contamination
title GOME aerosol optical depth retrieval over ocean: Correcting for the effects of residual cloud contamination
title_full GOME aerosol optical depth retrieval over ocean: Correcting for the effects of residual cloud contamination
title_fullStr GOME aerosol optical depth retrieval over ocean: Correcting for the effects of residual cloud contamination
title_full_unstemmed GOME aerosol optical depth retrieval over ocean: Correcting for the effects of residual cloud contamination
title_short GOME aerosol optical depth retrieval over ocean: Correcting for the effects of residual cloud contamination
title_sort gome aerosol optical depth retrieval over ocean correcting for the effects of residual cloud contamination
work_keys_str_mv AT carbonie gomeaerosolopticaldepthretrievaloveroceancorrectingfortheeffectsofresidualcloudcontamination