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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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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