MODIS 3 km aerosol product: algorithm and global perspective

After more than a decade of producing a nominal 10 km aerosol product based on the dark target method, the MODerate resolution Imaging Spectroradiometer (MODIS) aerosol team will be releasing a nominal 3 km product as part of their Collection 6 release. The new product differs from the original 10 k...

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Main Authors: L. A. Remer, S. Mattoo, R. C. Levy, L. A. Munchak
Format: Article
Language:English
Published: Copernicus Publications 2013-07-01
Series:Atmospheric Measurement Techniques
Online Access:http://www.atmos-meas-tech.net/6/1829/2013/amt-6-1829-2013.pdf
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spelling doaj-afe0d9644b2d4f779200d55af9cb434b2020-11-24T22:39:37ZengCopernicus PublicationsAtmospheric Measurement Techniques1867-13811867-85482013-07-01671829184410.5194/amt-6-1829-2013MODIS 3 km aerosol product: algorithm and global perspectiveL. A. RemerS. MattooR. C. LevyL. A. MunchakAfter more than a decade of producing a nominal 10 km aerosol product based on the dark target method, the MODerate resolution Imaging Spectroradiometer (MODIS) aerosol team will be releasing a nominal 3 km product as part of their Collection 6 release. The new product differs from the original 10 km product only in the manner in which reflectance pixels are ingested, organized and selected by the aerosol algorithm. Overall, the 3 km product closely mirrors the 10 km product. However, the finer resolution product is able to retrieve over the ocean closer to islands and coastlines, and is better able to resolve fine aerosol features such as smoke plumes over both ocean and land. In some situations, it provides retrievals over entire regions that the 10 km product barely samples. In situations traditionally difficult for the dark target algorithm such as over bright or urban surfaces, the 3 km product introduces isolated spikes of artificially high aerosol optical depth (AOD) that the 10 km algorithm avoids. Over land, globally, the 3 km product appears to be 0.01 to 0.02 higher than the 10 km product, while over ocean, the 3 km algorithm is retrieving a proportionally greater number of very low aerosol loading situations. Based on collocations with ground-based observations for only six months, expected errors associated with the 3 km land product are determined to be greater than that of the 10 km product: ± 0.05 ± 0.20 AOD. Over ocean, the suggestion is for expected errors to be the same as the 10 km product: ± 0.03 ± 0.05 AOD, but slightly less accurate in the coastal zone. The advantage of the product is on the local scale, which will require continued evaluation not addressed here. Nevertheless, the new 3 km product is expected to provide important information complementary to existing satellite-derived products and become an important tool for the aerosol community.http://www.atmos-meas-tech.net/6/1829/2013/amt-6-1829-2013.pdf
collection DOAJ
language English
format Article
sources DOAJ
author L. A. Remer
S. Mattoo
R. C. Levy
L. A. Munchak
spellingShingle L. A. Remer
S. Mattoo
R. C. Levy
L. A. Munchak
MODIS 3 km aerosol product: algorithm and global perspective
Atmospheric Measurement Techniques
author_facet L. A. Remer
S. Mattoo
R. C. Levy
L. A. Munchak
author_sort L. A. Remer
title MODIS 3 km aerosol product: algorithm and global perspective
title_short MODIS 3 km aerosol product: algorithm and global perspective
title_full MODIS 3 km aerosol product: algorithm and global perspective
title_fullStr MODIS 3 km aerosol product: algorithm and global perspective
title_full_unstemmed MODIS 3 km aerosol product: algorithm and global perspective
title_sort modis 3 km aerosol product: algorithm and global perspective
publisher Copernicus Publications
series Atmospheric Measurement Techniques
issn 1867-1381
1867-8548
publishDate 2013-07-01
description After more than a decade of producing a nominal 10 km aerosol product based on the dark target method, the MODerate resolution Imaging Spectroradiometer (MODIS) aerosol team will be releasing a nominal 3 km product as part of their Collection 6 release. The new product differs from the original 10 km product only in the manner in which reflectance pixels are ingested, organized and selected by the aerosol algorithm. Overall, the 3 km product closely mirrors the 10 km product. However, the finer resolution product is able to retrieve over the ocean closer to islands and coastlines, and is better able to resolve fine aerosol features such as smoke plumes over both ocean and land. In some situations, it provides retrievals over entire regions that the 10 km product barely samples. In situations traditionally difficult for the dark target algorithm such as over bright or urban surfaces, the 3 km product introduces isolated spikes of artificially high aerosol optical depth (AOD) that the 10 km algorithm avoids. Over land, globally, the 3 km product appears to be 0.01 to 0.02 higher than the 10 km product, while over ocean, the 3 km algorithm is retrieving a proportionally greater number of very low aerosol loading situations. Based on collocations with ground-based observations for only six months, expected errors associated with the 3 km land product are determined to be greater than that of the 10 km product: ± 0.05 ± 0.20 AOD. Over ocean, the suggestion is for expected errors to be the same as the 10 km product: ± 0.03 ± 0.05 AOD, but slightly less accurate in the coastal zone. The advantage of the product is on the local scale, which will require continued evaluation not addressed here. Nevertheless, the new 3 km product is expected to provide important information complementary to existing satellite-derived products and become an important tool for the aerosol community.
url http://www.atmos-meas-tech.net/6/1829/2013/amt-6-1829-2013.pdf
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