Effect of Cloud Fraction on Near-Cloud Aerosol Behavior in the MODIS Atmospheric Correction Ocean Color Product

Characterizing the way satellite-based aerosol statistics change near clouds is important for better understanding both aerosol-cloud interactions and aerosol direct radiative forcing. This study focuses on the question of whether the observed near-cloud increases in aerosol optical thickness and pa...

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Main Authors: Varnai, Tamas, Marshak, Alexander
Format: Other/Unknown Material
Language:unknown
Published: 2015
Subjects:
Online Access:http://hdl.handle.net/2060/20150007970
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spelling ftnasantrs:oai:casi.ntrs.nasa.gov:20150007970 2023-05-15T17:41:29+02:00 Effect of Cloud Fraction on Near-Cloud Aerosol Behavior in the MODIS Atmospheric Correction Ocean Color Product Varnai, Tamas Marshak, Alexander Unclassified, Unlimited, Publicly available April 27, 2015 application/pdf http://hdl.handle.net/2060/20150007970 unknown Document ID: 20150007970 http://hdl.handle.net/2060/20150007970 Copyright, Public use permitted CASI Earth Resources and Remote Sensing GSFC-E-DAA-TN20831 Remote Sensing (e-ISSN 2072-4292); 7; 5; 5283-5299 2015 ftnasantrs 2019-07-21T08:05:28Z Characterizing the way satellite-based aerosol statistics change near clouds is important for better understanding both aerosol-cloud interactions and aerosol direct radiative forcing. This study focuses on the question of whether the observed near-cloud increases in aerosol optical thickness and particle size may be explained by a combination of two factors: (i) Near-cloud data coming from areas with higher cloud fractions than far-from-cloud data and (ii) Cloud fraction being correlated with aerosol optical thickness and particle size. This question is addressed through a statistical analysis of aerosol parameters included in the MODIS (MODerate resolution Imaging Spectroradiometer) ocean color product. Results from ten Septembers (2002-2011) over part of the northeast Atlantic Ocean confirm that the combination of these two factors working together explains a significant but not dominant part (in our case, 15%-30%) of mean optical thickness changes near clouds. Overall, the findings show that cloud fraction plays a large role in shaping the way aerosol statistics change with distance to clouds. This implies that both cloud fraction and distance to clouds are important to consider when aerosol-cloud interactions or aerosol direct radiative effects are examined in satellite or modeling studies. Other/Unknown Material Northeast Atlantic NASA Technical Reports Server (NTRS)
institution Open Polar
collection NASA Technical Reports Server (NTRS)
op_collection_id ftnasantrs
language unknown
topic Earth Resources and Remote Sensing
spellingShingle Earth Resources and Remote Sensing
Varnai, Tamas
Marshak, Alexander
Effect of Cloud Fraction on Near-Cloud Aerosol Behavior in the MODIS Atmospheric Correction Ocean Color Product
topic_facet Earth Resources and Remote Sensing
description Characterizing the way satellite-based aerosol statistics change near clouds is important for better understanding both aerosol-cloud interactions and aerosol direct radiative forcing. This study focuses on the question of whether the observed near-cloud increases in aerosol optical thickness and particle size may be explained by a combination of two factors: (i) Near-cloud data coming from areas with higher cloud fractions than far-from-cloud data and (ii) Cloud fraction being correlated with aerosol optical thickness and particle size. This question is addressed through a statistical analysis of aerosol parameters included in the MODIS (MODerate resolution Imaging Spectroradiometer) ocean color product. Results from ten Septembers (2002-2011) over part of the northeast Atlantic Ocean confirm that the combination of these two factors working together explains a significant but not dominant part (in our case, 15%-30%) of mean optical thickness changes near clouds. Overall, the findings show that cloud fraction plays a large role in shaping the way aerosol statistics change with distance to clouds. This implies that both cloud fraction and distance to clouds are important to consider when aerosol-cloud interactions or aerosol direct radiative effects are examined in satellite or modeling studies.
format Other/Unknown Material
author Varnai, Tamas
Marshak, Alexander
author_facet Varnai, Tamas
Marshak, Alexander
author_sort Varnai, Tamas
title Effect of Cloud Fraction on Near-Cloud Aerosol Behavior in the MODIS Atmospheric Correction Ocean Color Product
title_short Effect of Cloud Fraction on Near-Cloud Aerosol Behavior in the MODIS Atmospheric Correction Ocean Color Product
title_full Effect of Cloud Fraction on Near-Cloud Aerosol Behavior in the MODIS Atmospheric Correction Ocean Color Product
title_fullStr Effect of Cloud Fraction on Near-Cloud Aerosol Behavior in the MODIS Atmospheric Correction Ocean Color Product
title_full_unstemmed Effect of Cloud Fraction on Near-Cloud Aerosol Behavior in the MODIS Atmospheric Correction Ocean Color Product
title_sort effect of cloud fraction on near-cloud aerosol behavior in the modis atmospheric correction ocean color product
publishDate 2015
url http://hdl.handle.net/2060/20150007970
op_coverage Unclassified, Unlimited, Publicly available
genre Northeast Atlantic
genre_facet Northeast Atlantic
op_source CASI
op_relation Document ID: 20150007970
http://hdl.handle.net/2060/20150007970
op_rights Copyright, Public use permitted
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