Assessment of tropospheric CALIPSO Version 4.2 aerosol types over the ocean using independent CALIPSO–SODA lidar ratios

<p>We assess the CALIPSO Version 4.2 (V4) aerosol typing and assigned lidar ratios over ocean using aerosol optical depth (AOD) retrievals from the Synergized Optical Depth of Aerosols (SODA) algorithm and retrieved columnar lidar ratio estimated by combining SODA AOD and CALIPSO attenuated ba...

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Main Authors: Z. Li, D. Painemal, G. Schuster, M. Clayton, R. Ferrare, M. Vaughan, D. Josset, J. Kar, C. Trepte
Format: Article
Language:English
Published: Copernicus Publications 2022-05-01
Series:Atmospheric Measurement Techniques
Online Access:https://amt.copernicus.org/articles/15/2745/2022/amt-15-2745-2022.pdf
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author Z. Li
Z. Li
D. Painemal
D. Painemal
G. Schuster
M. Clayton
M. Clayton
R. Ferrare
M. Vaughan
D. Josset
J. Kar
J. Kar
C. Trepte
author_facet Z. Li
Z. Li
D. Painemal
D. Painemal
G. Schuster
M. Clayton
M. Clayton
R. Ferrare
M. Vaughan
D. Josset
J. Kar
J. Kar
C. Trepte
author_sort Z. Li
collection DOAJ
description <p>We assess the CALIPSO Version 4.2 (V4) aerosol typing and assigned lidar ratios over ocean using aerosol optical depth (AOD) retrievals from the Synergized Optical Depth of Aerosols (SODA) algorithm and retrieved columnar lidar ratio estimated by combining SODA AOD and CALIPSO attenuated backscatter (CALIPSO–SODA). Six aerosol types – clean marine, dusty marine, dust, polluted continental/smoke, polluted dust, and elevated smoke – are characterized using CALIPSO–SODA over ocean and the results are compared against the prescribed V4 lidar ratios, when only one aerosol type is present in the atmospheric column. For samples detected at 5 or 20 km spatial resolutions and having AOD <span class="inline-formula">&gt;</span> 0.05, the CALIPSO–SODA lidar ratios are significantly different between different aerosol types, and are consistent with the type-specific values assigned in V4 to within 10 sr (except for polluted continental/smoke). This implies that the CALIPSO classification scheme generally categorizes specific aerosols types correctly over regions where they are abundant. We find remarkable daytime/nighttime regional agreement for clean marine aerosol over the open ocean (CALIPSO–SODA <span class="inline-formula">=</span> 20–25 sr, V4 <span class="inline-formula">=</span> 23 sr), elevated smoke over the southeast Atlantic (CALIPSO–SODA <span class="inline-formula">=</span> 65–75 sr, V4 <span class="inline-formula">=</span> 70 sr), and dust over the subtropical Atlantic adjacent to the African continent (CALIPSO–SODA <span class="inline-formula">=</span> 40–50 sr, V4 <span class="inline-formula">=</span> 44 sr). In contrast, daytime polluted continental/smoke lidar ratio is more than 20 sr smaller than the constant V4 value for that type, attributed in part to the challenge of classifying tenuous aerosol with low signal-to-noise ratio. Dust over most of the Atlantic Ocean features CALIPSO–SODA lidar ratios less than 40 sr, possibly suggesting the presence of dust mixed with marine aerosols or lidar ratio values that depend on source and evolution of the aerosol plume. The new dusty marine type introduced in V4 features similar magnitudes and spatial distribution as its clean marine counterpart with lidar ratio differences of less than 3 sr, and nearly identical values over the open ocean, implying that some modification of the classification scheme for the marine subtypes is warranted.</p>
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spelling doaj.art-3c0d58b0e4164e88b17e6f97c252c46e2022-12-22T02:01:17ZengCopernicus PublicationsAtmospheric Measurement Techniques1867-13811867-85482022-05-01152745276610.5194/amt-15-2745-2022Assessment of tropospheric CALIPSO Version 4.2 aerosol types over the ocean using independent CALIPSO–SODA lidar ratiosZ. Li0Z. Li1D. Painemal2D. Painemal3G. Schuster4M. Clayton5M. Clayton6R. Ferrare7M. Vaughan8D. Josset9J. Kar10J. Kar11C. Trepte12Science Systems and Applications Systems, Inc., Hampton, VA 23666, USA​​​​​​​NASA Langley Research Center, Hampton, VA 23681, USAScience Systems and Applications Systems, Inc., Hampton, VA 23666, USA​​​​​​​NASA Langley Research Center, Hampton, VA 23681, USANASA Langley Research Center, Hampton, VA 23681, USAScience Systems and Applications Systems, Inc., Hampton, VA 23666, USA​​​​​​​NASA Langley Research Center, Hampton, VA 23681, USANASA Langley Research Center, Hampton, VA 23681, USANASA Langley Research Center, Hampton, VA 23681, USAU.S. Naval Research Laboratory, Stennis Space Center, MS, 39529, USA​​​​​​​Science Systems and Applications Systems, Inc., Hampton, VA 23666, USA​​​​​​​NASA Langley Research Center, Hampton, VA 23681, USANASA Langley Research Center, Hampton, VA 23681, USA<p>We assess the CALIPSO Version 4.2 (V4) aerosol typing and assigned lidar ratios over ocean using aerosol optical depth (AOD) retrievals from the Synergized Optical Depth of Aerosols (SODA) algorithm and retrieved columnar lidar ratio estimated by combining SODA AOD and CALIPSO attenuated backscatter (CALIPSO–SODA). Six aerosol types – clean marine, dusty marine, dust, polluted continental/smoke, polluted dust, and elevated smoke – are characterized using CALIPSO–SODA over ocean and the results are compared against the prescribed V4 lidar ratios, when only one aerosol type is present in the atmospheric column. For samples detected at 5 or 20 km spatial resolutions and having AOD <span class="inline-formula">&gt;</span> 0.05, the CALIPSO–SODA lidar ratios are significantly different between different aerosol types, and are consistent with the type-specific values assigned in V4 to within 10 sr (except for polluted continental/smoke). This implies that the CALIPSO classification scheme generally categorizes specific aerosols types correctly over regions where they are abundant. We find remarkable daytime/nighttime regional agreement for clean marine aerosol over the open ocean (CALIPSO–SODA <span class="inline-formula">=</span> 20–25 sr, V4 <span class="inline-formula">=</span> 23 sr), elevated smoke over the southeast Atlantic (CALIPSO–SODA <span class="inline-formula">=</span> 65–75 sr, V4 <span class="inline-formula">=</span> 70 sr), and dust over the subtropical Atlantic adjacent to the African continent (CALIPSO–SODA <span class="inline-formula">=</span> 40–50 sr, V4 <span class="inline-formula">=</span> 44 sr). In contrast, daytime polluted continental/smoke lidar ratio is more than 20 sr smaller than the constant V4 value for that type, attributed in part to the challenge of classifying tenuous aerosol with low signal-to-noise ratio. Dust over most of the Atlantic Ocean features CALIPSO–SODA lidar ratios less than 40 sr, possibly suggesting the presence of dust mixed with marine aerosols or lidar ratio values that depend on source and evolution of the aerosol plume. The new dusty marine type introduced in V4 features similar magnitudes and spatial distribution as its clean marine counterpart with lidar ratio differences of less than 3 sr, and nearly identical values over the open ocean, implying that some modification of the classification scheme for the marine subtypes is warranted.</p>https://amt.copernicus.org/articles/15/2745/2022/amt-15-2745-2022.pdf
spellingShingle Z. Li
Z. Li
D. Painemal
D. Painemal
G. Schuster
M. Clayton
M. Clayton
R. Ferrare
M. Vaughan
D. Josset
J. Kar
J. Kar
C. Trepte
Assessment of tropospheric CALIPSO Version 4.2 aerosol types over the ocean using independent CALIPSO–SODA lidar ratios
Atmospheric Measurement Techniques
title Assessment of tropospheric CALIPSO Version 4.2 aerosol types over the ocean using independent CALIPSO–SODA lidar ratios
title_full Assessment of tropospheric CALIPSO Version 4.2 aerosol types over the ocean using independent CALIPSO–SODA lidar ratios
title_fullStr Assessment of tropospheric CALIPSO Version 4.2 aerosol types over the ocean using independent CALIPSO–SODA lidar ratios
title_full_unstemmed Assessment of tropospheric CALIPSO Version 4.2 aerosol types over the ocean using independent CALIPSO–SODA lidar ratios
title_short Assessment of tropospheric CALIPSO Version 4.2 aerosol types over the ocean using independent CALIPSO–SODA lidar ratios
title_sort assessment of tropospheric calipso version 4 2 aerosol types over the ocean using independent calipso soda lidar ratios
url https://amt.copernicus.org/articles/15/2745/2022/amt-15-2745-2022.pdf
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