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...

Full description

Bibliographic Details
Published in:Remote Sensing
Main Authors: Tamás Várnai, Alexander Marshak
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2015
Subjects:
Online Access:https://doi.org/10.3390/rs70505283
_version_ 1821659916467699712
author Tamás Várnai
Alexander Marshak
author_facet Tamás Várnai
Alexander Marshak
author_sort Tamás Várnai
collection MDPI Open Access Publishing
container_issue 5
container_start_page 5283
container_title Remote Sensing
container_volume 7
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 Text
genre Northeast Atlantic
genre_facet Northeast Atlantic
id ftmdpi:oai:mdpi.com:/2072-4292/7/5/5283/
institution Open Polar
language English
op_collection_id ftmdpi
op_container_end_page 5299
op_coverage agris
op_doi https://doi.org/10.3390/rs70505283
op_relation https://dx.doi.org/10.3390/rs70505283
op_rights https://creativecommons.org/licenses/by/4.0/
op_source Remote Sensing; Volume 7; Issue 5; Pages: 5283-5299
publishDate 2015
publisher Multidisciplinary Digital Publishing Institute
record_format openpolar
spelling ftmdpi:oai:mdpi.com:/2072-4292/7/5/5283/ 2025-01-16T23:51:03+00:00 Effect of Cloud Fraction on Near-Cloud Aerosol Behavior in the MODIS Atmospheric Correction Ocean Color Product Tamás Várnai Alexander Marshak agris 2015-04-27 application/pdf https://doi.org/10.3390/rs70505283 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/rs70505283 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 7; Issue 5; Pages: 5283-5299 cloud aerosol remote sensing satellite MODIS Text 2015 ftmdpi https://doi.org/10.3390/rs70505283 2023-07-31T20:43:16Z 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. Text Northeast Atlantic MDPI Open Access Publishing Remote Sensing 7 5 5283 5299
spellingShingle cloud
aerosol
remote sensing
satellite
MODIS
Tamás Várnai
Alexander Marshak
Effect of Cloud Fraction on Near-Cloud Aerosol Behavior in the MODIS Atmospheric Correction Ocean Color Product
title 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_short 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
topic cloud
aerosol
remote sensing
satellite
MODIS
topic_facet cloud
aerosol
remote sensing
satellite
MODIS
url https://doi.org/10.3390/rs70505283