Aerosol retrieval over snow using the RemoTAP algorithm

In order to conduct accurate aerosol retrieval over snow, the Remote Sensing of Trace Gases and Aerosol Products (RemoTAP) algorithm developed by SRON Netherlands Institute for Space Research is extended with a bi-directional reflection distribution function (BRDF) for snow surfaces. The capability...

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Published in:Atmospheric Measurement Techniques
Main Authors: Zhang, Zihan, Fu, Guangliang, Hasekamp, Otto
Format: Text
Language:English
Published: 2023
Subjects:
Online Access:https://doi.org/10.5194/amt-16-6051-2023
https://amt.copernicus.org/articles/16/6051/2023/
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spelling ftcopernicus:oai:publications.copernicus.org:amt112512 2024-09-15T17:35:15+00:00 Aerosol retrieval over snow using the RemoTAP algorithm Zhang, Zihan Fu, Guangliang Hasekamp, Otto 2023-12-19 application/pdf https://doi.org/10.5194/amt-16-6051-2023 https://amt.copernicus.org/articles/16/6051/2023/ eng eng doi:10.5194/amt-16-6051-2023 https://amt.copernicus.org/articles/16/6051/2023/ eISSN: 1867-8548 Text 2023 ftcopernicus https://doi.org/10.5194/amt-16-6051-2023 2024-08-28T05:24:15Z In order to conduct accurate aerosol retrieval over snow, the Remote Sensing of Trace Gases and Aerosol Products (RemoTAP) algorithm developed by SRON Netherlands Institute for Space Research is extended with a bi-directional reflection distribution function (BRDF) for snow surfaces. The capability of the extended algorithm is validated with both synthetic measurements and real satellite measurements from the Polarization & Anisotropy of Reflectances for Atmospheric Sciences coupled with Observations from a Lidar (PARASOL), and a comparison has been made to retrievals with the baseline RemoTAP (without a snow kernel). For retrievals with real PARASOL observations, we use pixels over Aerosol Robotic Network (AERONET) stations for validation and we use the MODIS snow cover products to identify pixels over snow. We evaluate the retrieved aerosol optical thickness (AOT) at 550 nm ( τ 550 ) , single-scattering albedo (SSA) at 550 nm ( ω 550 ) and Ångström exponent (AE) for 440–870 nm ( AE 440−870 ) . The experiments with both synthetic and real data show that the extended RemoTAP maintains capability for snow-free pixels and has obvious advantages in accuracy and the fraction of successful retrievals for retrieval over snow, especially over surfaces with snow cover >75 %. According to the real-data experiment, we find that the retrieval algorithm has difficulty in fitting the PARASOL 1020 nm band, where snow reflectance is significantly lower than that for the visible bands. When we perform a four-band retrieval (490, 565, 670, 865 nm) with the extended RemoTAP, we obtain a good retrieval result for τ 550 , ω 550 and AE 440−870 . Therefore, the four-band retrieval with the extended RemoTAP is recommended for aerosol retrieval over snow. Text Aerosol Robotic Network Copernicus Publications: E-Journals Atmospheric Measurement Techniques 16 24 6051 6063
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description In order to conduct accurate aerosol retrieval over snow, the Remote Sensing of Trace Gases and Aerosol Products (RemoTAP) algorithm developed by SRON Netherlands Institute for Space Research is extended with a bi-directional reflection distribution function (BRDF) for snow surfaces. The capability of the extended algorithm is validated with both synthetic measurements and real satellite measurements from the Polarization & Anisotropy of Reflectances for Atmospheric Sciences coupled with Observations from a Lidar (PARASOL), and a comparison has been made to retrievals with the baseline RemoTAP (without a snow kernel). For retrievals with real PARASOL observations, we use pixels over Aerosol Robotic Network (AERONET) stations for validation and we use the MODIS snow cover products to identify pixels over snow. We evaluate the retrieved aerosol optical thickness (AOT) at 550 nm ( τ 550 ) , single-scattering albedo (SSA) at 550 nm ( ω 550 ) and Ångström exponent (AE) for 440–870 nm ( AE 440−870 ) . The experiments with both synthetic and real data show that the extended RemoTAP maintains capability for snow-free pixels and has obvious advantages in accuracy and the fraction of successful retrievals for retrieval over snow, especially over surfaces with snow cover >75 %. According to the real-data experiment, we find that the retrieval algorithm has difficulty in fitting the PARASOL 1020 nm band, where snow reflectance is significantly lower than that for the visible bands. When we perform a four-band retrieval (490, 565, 670, 865 nm) with the extended RemoTAP, we obtain a good retrieval result for τ 550 , ω 550 and AE 440−870 . Therefore, the four-band retrieval with the extended RemoTAP is recommended for aerosol retrieval over snow.
format Text
author Zhang, Zihan
Fu, Guangliang
Hasekamp, Otto
spellingShingle Zhang, Zihan
Fu, Guangliang
Hasekamp, Otto
Aerosol retrieval over snow using the RemoTAP algorithm
author_facet Zhang, Zihan
Fu, Guangliang
Hasekamp, Otto
author_sort Zhang, Zihan
title Aerosol retrieval over snow using the RemoTAP algorithm
title_short Aerosol retrieval over snow using the RemoTAP algorithm
title_full Aerosol retrieval over snow using the RemoTAP algorithm
title_fullStr Aerosol retrieval over snow using the RemoTAP algorithm
title_full_unstemmed Aerosol retrieval over snow using the RemoTAP algorithm
title_sort aerosol retrieval over snow using the remotap algorithm
publishDate 2023
url https://doi.org/10.5194/amt-16-6051-2023
https://amt.copernicus.org/articles/16/6051/2023/
genre Aerosol Robotic Network
genre_facet Aerosol Robotic Network
op_source eISSN: 1867-8548
op_relation doi:10.5194/amt-16-6051-2023
https://amt.copernicus.org/articles/16/6051/2023/
op_doi https://doi.org/10.5194/amt-16-6051-2023
container_title Atmospheric Measurement Techniques
container_volume 16
container_issue 24
container_start_page 6051
op_container_end_page 6063
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