Near-Cloud Aerosol Properties from the 1 Km Resolution MODIS Ocean Product
This study examines aerosol properties in the vicinity of clouds by analyzing high-resolution atmospheric correction parameters provided in the MODIS (Moderate Resolution Imaging Spectroradiometer) ocean color product. The study analyzes data from a 2 week long period of September in 10 years, cover...
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ftnasantrs:oai:casi.ntrs.nasa.gov:20140010871 2023-05-15T17:41:32+02:00 Near-Cloud Aerosol Properties from the 1 Km Resolution MODIS Ocean Product Varnai, Tamas Marshak, Alexander Unclassified, Unlimited, Publicly available February 15, 2014 application/pdf http://hdl.handle.net/2060/20140010871 unknown Document ID: 20140010871 http://hdl.handle.net/2060/20140010871 Copyright, Distribution as joint owner in the copyright CASI Earth Resources and Remote Sensing GSFC-E-DAA-TN10928 Journal Geophysical Research-Atmospheres; 119; 3; 1546-1554 2014 ftnasantrs 2019-07-21T00:26:50Z This study examines aerosol properties in the vicinity of clouds by analyzing high-resolution atmospheric correction parameters provided in the MODIS (Moderate Resolution Imaging Spectroradiometer) ocean color product. The study analyzes data from a 2 week long period of September in 10 years, covering a large area in the northeast Atlantic Ocean. The results indicate that on the one hand, the Quality Assessment (QA) flags of the ocean color product successfully eliminate cloud-related uncertainties in ocean parameters such as chlorophyll content, but on the other hand, using the flags introduces a sampling bias in atmospheric products such as aerosol optical thickness (AOT) and Angstrom exponent. Therefore, researchers need to select QA flags by balancing the risks of increased retrieval uncertainties and sampling biases. Using an optimal set of QA flags, the results reveal substantial increases in optical thickness near clouds-on average the increase is 50% for the roughly half of pixels within 5 km from clouds and is accompanied by a roughly matching increase in particle size. Theoretical simulations show that the 50% increase in 550nm AOT changes instantaneous direct aerosol radiative forcing by up to 8W/m2 and that the radiative impact is significantly larger if observed near-cloud changes are attributed to aerosol particles as opposed to undetected cloud particles. These results underline that accounting for near-cloud areas and understanding the causes of near-cloud particle changes are critical for accurate calculations of direct aerosol radiative forcing. Other/Unknown Material Northeast Atlantic NASA Technical Reports Server (NTRS) |
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Open Polar |
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NASA Technical Reports Server (NTRS) |
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Earth Resources and Remote Sensing |
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Earth Resources and Remote Sensing Varnai, Tamas Marshak, Alexander Near-Cloud Aerosol Properties from the 1 Km Resolution MODIS Ocean Product |
topic_facet |
Earth Resources and Remote Sensing |
description |
This study examines aerosol properties in the vicinity of clouds by analyzing high-resolution atmospheric correction parameters provided in the MODIS (Moderate Resolution Imaging Spectroradiometer) ocean color product. The study analyzes data from a 2 week long period of September in 10 years, covering a large area in the northeast Atlantic Ocean. The results indicate that on the one hand, the Quality Assessment (QA) flags of the ocean color product successfully eliminate cloud-related uncertainties in ocean parameters such as chlorophyll content, but on the other hand, using the flags introduces a sampling bias in atmospheric products such as aerosol optical thickness (AOT) and Angstrom exponent. Therefore, researchers need to select QA flags by balancing the risks of increased retrieval uncertainties and sampling biases. Using an optimal set of QA flags, the results reveal substantial increases in optical thickness near clouds-on average the increase is 50% for the roughly half of pixels within 5 km from clouds and is accompanied by a roughly matching increase in particle size. Theoretical simulations show that the 50% increase in 550nm AOT changes instantaneous direct aerosol radiative forcing by up to 8W/m2 and that the radiative impact is significantly larger if observed near-cloud changes are attributed to aerosol particles as opposed to undetected cloud particles. These results underline that accounting for near-cloud areas and understanding the causes of near-cloud particle changes are critical for accurate calculations of direct aerosol radiative forcing. |
format |
Other/Unknown Material |
author |
Varnai, Tamas Marshak, Alexander |
author_facet |
Varnai, Tamas Marshak, Alexander |
author_sort |
Varnai, Tamas |
title |
Near-Cloud Aerosol Properties from the 1 Km Resolution MODIS Ocean Product |
title_short |
Near-Cloud Aerosol Properties from the 1 Km Resolution MODIS Ocean Product |
title_full |
Near-Cloud Aerosol Properties from the 1 Km Resolution MODIS Ocean Product |
title_fullStr |
Near-Cloud Aerosol Properties from the 1 Km Resolution MODIS Ocean Product |
title_full_unstemmed |
Near-Cloud Aerosol Properties from the 1 Km Resolution MODIS Ocean Product |
title_sort |
near-cloud aerosol properties from the 1 km resolution modis ocean product |
publishDate |
2014 |
url |
http://hdl.handle.net/2060/20140010871 |
op_coverage |
Unclassified, Unlimited, Publicly available |
genre |
Northeast Atlantic |
genre_facet |
Northeast Atlantic |
op_source |
CASI |
op_relation |
Document ID: 20140010871 http://hdl.handle.net/2060/20140010871 |
op_rights |
Copyright, Distribution as joint owner in the copyright |
_version_ |
1766143136833208320 |