SMAP Salinity Retrievals near the Sea-Ice Edge Using Multi-Channel AMSR2 Brightness Temperatures

Sea-ice contamination in the antenna field of view constitutes a large error source in retrieving sea-surface salinity (SSS) with the spaceborne Soil Moisture Active Passive (SMAP) L-band radiometer. This is a major obstacle in the current NASA/Remote Sensing Systems (RSS) SMAP SSS retrieval algorit...

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Published in:Remote Sensing
Main Authors: Thomas Meissner, Andrew Manaster
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2021
Subjects:
Online Access:https://doi.org/10.3390/rs13245120
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spelling ftmdpi:oai:mdpi.com:/2072-4292/13/24/5120/ 2023-10-09T21:55:50+02:00 SMAP Salinity Retrievals near the Sea-Ice Edge Using Multi-Channel AMSR2 Brightness Temperatures Thomas Meissner Andrew Manaster agris 2021-12-16 application/pdf https://doi.org/10.3390/rs13245120 eng eng Multidisciplinary Digital Publishing Institute Ocean Remote Sensing https://dx.doi.org/10.3390/rs13245120 https://creativecommons.org/licenses/by/4.0/ Remote Sensing Volume 13 Issue 24 Pages: 5120 SMAP AMSR2 sea surface salinity sea-ice cold water Text 2021 ftmdpi https://doi.org/10.3390/rs13245120 2023-09-10T23:55:40Z Sea-ice contamination in the antenna field of view constitutes a large error source in retrieving sea-surface salinity (SSS) with the spaceborne Soil Moisture Active Passive (SMAP) L-band radiometer. This is a major obstacle in the current NASA/Remote Sensing Systems (RSS) SMAP SSS retrieval algorithm in regards to obtaining accurate SSS measurements in the polar oceans. Our analysis finds a strong correlation between 8-day averaged SMAP L-band brightness temperature (TB) bias and TB measurements from the Advanced Microwave Scanning Radiometer (AMSR2) in the C-through Ka-band frequency range for sea-ice contaminated ocean scenes. We show how this correlation can be employed to develop: (1) a discriminant analysis that is able to reliably flag the SMAP observations for sea-ice contamination and (2) subsequently remove the sea-ice contamination from the SMAP observations, which results in significantly more accurate SMAP SSS retrievals near the sea-ice edge. We provide a case study that evaluates the performance of the proposed sea-ice flagging and correction algorithm. Our method is also able to detect drifting icebergs, which go often undetected in many available standard sea-ice products and thus result in spurious SMAP SSS retrievals. Text Sea ice MDPI Open Access Publishing Remote Sensing 13 24 5120
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic SMAP
AMSR2
sea surface salinity
sea-ice
cold water
spellingShingle SMAP
AMSR2
sea surface salinity
sea-ice
cold water
Thomas Meissner
Andrew Manaster
SMAP Salinity Retrievals near the Sea-Ice Edge Using Multi-Channel AMSR2 Brightness Temperatures
topic_facet SMAP
AMSR2
sea surface salinity
sea-ice
cold water
description Sea-ice contamination in the antenna field of view constitutes a large error source in retrieving sea-surface salinity (SSS) with the spaceborne Soil Moisture Active Passive (SMAP) L-band radiometer. This is a major obstacle in the current NASA/Remote Sensing Systems (RSS) SMAP SSS retrieval algorithm in regards to obtaining accurate SSS measurements in the polar oceans. Our analysis finds a strong correlation between 8-day averaged SMAP L-band brightness temperature (TB) bias and TB measurements from the Advanced Microwave Scanning Radiometer (AMSR2) in the C-through Ka-band frequency range for sea-ice contaminated ocean scenes. We show how this correlation can be employed to develop: (1) a discriminant analysis that is able to reliably flag the SMAP observations for sea-ice contamination and (2) subsequently remove the sea-ice contamination from the SMAP observations, which results in significantly more accurate SMAP SSS retrievals near the sea-ice edge. We provide a case study that evaluates the performance of the proposed sea-ice flagging and correction algorithm. Our method is also able to detect drifting icebergs, which go often undetected in many available standard sea-ice products and thus result in spurious SMAP SSS retrievals.
format Text
author Thomas Meissner
Andrew Manaster
author_facet Thomas Meissner
Andrew Manaster
author_sort Thomas Meissner
title SMAP Salinity Retrievals near the Sea-Ice Edge Using Multi-Channel AMSR2 Brightness Temperatures
title_short SMAP Salinity Retrievals near the Sea-Ice Edge Using Multi-Channel AMSR2 Brightness Temperatures
title_full SMAP Salinity Retrievals near the Sea-Ice Edge Using Multi-Channel AMSR2 Brightness Temperatures
title_fullStr SMAP Salinity Retrievals near the Sea-Ice Edge Using Multi-Channel AMSR2 Brightness Temperatures
title_full_unstemmed SMAP Salinity Retrievals near the Sea-Ice Edge Using Multi-Channel AMSR2 Brightness Temperatures
title_sort smap salinity retrievals near the sea-ice edge using multi-channel amsr2 brightness temperatures
publisher Multidisciplinary Digital Publishing Institute
publishDate 2021
url https://doi.org/10.3390/rs13245120
op_coverage agris
genre Sea ice
genre_facet Sea ice
op_source Remote Sensing
Volume 13
Issue 24
Pages: 5120
op_relation Ocean Remote Sensing
https://dx.doi.org/10.3390/rs13245120
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/rs13245120
container_title Remote Sensing
container_volume 13
container_issue 24
container_start_page 5120
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