Aerosol Optical Properties Above Opaque Water Clouds Derived From The Caliop Version 4 Level 1 Data

In a previous study we evaluated the above-cloud aerosol optical depth (AOD) retrieval at 532 nm in the CALIOP version 3 (V3) data products for two selected spatial domains along the Saharan dust transport pathway and African smoke transport pathway. In that study we rescaled the V3 level-1 (L1) dat...

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Main Authors: Liu Zhaoyan, Winker David, Omar Ali, Vaughan Mark, Kar Jayanta, Trepte Charles, Hu Yongxiang, Schuster Gregory, Young Stuart
Format: Article
Language:English
Published: EDP Sciences 2016-01-01
Series:EPJ Web of Conferences
Online Access:http://dx.doi.org/10.1051/epjconf/201611904010
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spelling doaj-c8d7df594e614a1db88fdbd1288616042021-08-02T12:42:50ZengEDP SciencesEPJ Web of Conferences2100-014X2016-01-011190401010.1051/epjconf/201611904010epjconf_ilrc2016_04010Aerosol Optical Properties Above Opaque Water Clouds Derived From The Caliop Version 4 Level 1 DataLiu ZhaoyanWinker David0Omar Ali1Vaughan Mark2Kar JayantaTrepte Charles3Hu Yongxiang4Schuster Gregory5Young Stuart6NASA Langley Research CenterNASA Langley Research CenterScience Systems and Applications Inc.NASA Langley Research CenterNASA Langley Research CenterNASA Langley Research CenterCSIRO Oceans and AtmosphereIn a previous study we evaluated the above-cloud aerosol optical depth (AOD) retrieval at 532 nm in the CALIOP version 3 (V3) data products for two selected spatial domains along the Saharan dust transport pathway and African smoke transport pathway. In that study we rescaled the V3 level-1 (L1) data to compensate for known V3 calibration biases, and then derived aerosol intrinsic properties such as lidar ratio (Sa) and particulate depolarization ratio (PDR) for comparison with the CALIOP dust and smoke aerosol models. The calibration of the recently released version 4 (V4) CALIPSO L1 data product is significantly improved over V3. So in this paper we repeat our previous analysis using the new V4 L1 data. A comparison shows that our rescaled V3 and the new V4 data are different only by ~1% in the two selected spatial domains. The retrieved AOD values decrease by ~2.6% in both domains from V3 to V4. When the data is screened to exclude weakly scattering layers, the median Sa retrieved from the V4 L1 data in the dust transport region is reduced by 1.4 sr to 43.0±8.3 sr. The median Sa value in the smoke transport region is increased by 0.8 sr to 71.2±15.1 sr. The PDR values remain almost unchanged for the screened data.http://dx.doi.org/10.1051/epjconf/201611904010
collection DOAJ
language English
format Article
sources DOAJ
author Liu Zhaoyan
Winker David
Omar Ali
Vaughan Mark
Kar Jayanta
Trepte Charles
Hu Yongxiang
Schuster Gregory
Young Stuart
spellingShingle Liu Zhaoyan
Winker David
Omar Ali
Vaughan Mark
Kar Jayanta
Trepte Charles
Hu Yongxiang
Schuster Gregory
Young Stuart
Aerosol Optical Properties Above Opaque Water Clouds Derived From The Caliop Version 4 Level 1 Data
EPJ Web of Conferences
author_facet Liu Zhaoyan
Winker David
Omar Ali
Vaughan Mark
Kar Jayanta
Trepte Charles
Hu Yongxiang
Schuster Gregory
Young Stuart
author_sort Liu Zhaoyan
title Aerosol Optical Properties Above Opaque Water Clouds Derived From The Caliop Version 4 Level 1 Data
title_short Aerosol Optical Properties Above Opaque Water Clouds Derived From The Caliop Version 4 Level 1 Data
title_full Aerosol Optical Properties Above Opaque Water Clouds Derived From The Caliop Version 4 Level 1 Data
title_fullStr Aerosol Optical Properties Above Opaque Water Clouds Derived From The Caliop Version 4 Level 1 Data
title_full_unstemmed Aerosol Optical Properties Above Opaque Water Clouds Derived From The Caliop Version 4 Level 1 Data
title_sort aerosol optical properties above opaque water clouds derived from the caliop version 4 level 1 data
publisher EDP Sciences
series EPJ Web of Conferences
issn 2100-014X
publishDate 2016-01-01
description In a previous study we evaluated the above-cloud aerosol optical depth (AOD) retrieval at 532 nm in the CALIOP version 3 (V3) data products for two selected spatial domains along the Saharan dust transport pathway and African smoke transport pathway. In that study we rescaled the V3 level-1 (L1) data to compensate for known V3 calibration biases, and then derived aerosol intrinsic properties such as lidar ratio (Sa) and particulate depolarization ratio (PDR) for comparison with the CALIOP dust and smoke aerosol models. The calibration of the recently released version 4 (V4) CALIPSO L1 data product is significantly improved over V3. So in this paper we repeat our previous analysis using the new V4 L1 data. A comparison shows that our rescaled V3 and the new V4 data are different only by ~1% in the two selected spatial domains. The retrieved AOD values decrease by ~2.6% in both domains from V3 to V4. When the data is screened to exclude weakly scattering layers, the median Sa retrieved from the V4 L1 data in the dust transport region is reduced by 1.4 sr to 43.0±8.3 sr. The median Sa value in the smoke transport region is increased by 0.8 sr to 71.2±15.1 sr. The PDR values remain almost unchanged for the screened data.
url http://dx.doi.org/10.1051/epjconf/201611904010
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