A NEW WEATHER FILTER FOR REDUCING WEATHER EFFECT IN CALCULATING SEA ICE CONCENTRATION FROM AMSR2 DATA

Ice concentration is one of the most fundamental parameters of sea ice which can be calculated from brightness temperatures measured by passive microwave radiometers such as AMSR2 onboard satellites. However, the presence of atmospheric water vapor, cloud liquid water, etc. is likely to increase the...

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Published in:ISPRS Annals of the Photogrammetry, Remote Sensing and Spatial Information Sciences
Main Authors: Cho, K., Naoki, K.
Format: Text
Language:English
Published: 2023
Subjects:
Online Access:https://doi.org/10.5194/isprs-annals-X-1-W1-2023-793-2023
https://isprs-annals.copernicus.org/articles/X-1-W1-2023/793/2023/
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spelling ftcopernicus:oai:publications.copernicus.org:isprs-annals116502 2024-01-07T09:46:36+01:00 A NEW WEATHER FILTER FOR REDUCING WEATHER EFFECT IN CALCULATING SEA ICE CONCENTRATION FROM AMSR2 DATA Cho, K. Naoki, K. 2023-12-04 application/pdf https://doi.org/10.5194/isprs-annals-X-1-W1-2023-793-2023 https://isprs-annals.copernicus.org/articles/X-1-W1-2023/793/2023/ eng eng doi:10.5194/isprs-annals-X-1-W1-2023-793-2023 https://isprs-annals.copernicus.org/articles/X-1-W1-2023/793/2023/ eISSN: 2194-9050 Text 2023 ftcopernicus https://doi.org/10.5194/isprs-annals-X-1-W1-2023-793-2023 2023-12-11T17:24:18Z Ice concentration is one of the most fundamental parameters of sea ice which can be calculated from brightness temperatures measured by passive microwave radiometers such as AMSR2 onboard satellites. However, the presence of atmospheric water vapor, cloud liquid water, etc. is likely to increase the brightness temperatures over open water. As a result, sometimes, certain ice concentrations are calculated over open water covered with heavy clouds. The authors call this kind of area as “false sea ice” and the phenomenon is called the weather effect. In the AMSR2 ice concentration product, a weather filter is used to reduce the weather effect. However, it is known that false sea ice appears occasionally in some areas even in the summertime in AMSR2 ice concentration products. In this study, the authors have modified the original weather filter and added a new weather filter utilizing the following two equations which are TB(23GHzV)<−0.75×(TB(36GHzV)−TB(36GHzH))+253K and TB(36GHzV)−TB(36GHzH) < 57K. If the brightness temperature of the pixel meets the above two equations, we set the ice concentration of the pixel as 0%. By adding the new weather filter, most of the false sea ice that appeared in the ASMR2 ice concentration products could be rejected. JAXA has decided to add this weather filter for producing AMSR2 standard sea ice concentration products. Text Sea ice Copernicus Publications: E-Journals ISPRS Annals of the Photogrammetry, Remote Sensing and Spatial Information Sciences X-1/W1-2023 793 798
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Ice concentration is one of the most fundamental parameters of sea ice which can be calculated from brightness temperatures measured by passive microwave radiometers such as AMSR2 onboard satellites. However, the presence of atmospheric water vapor, cloud liquid water, etc. is likely to increase the brightness temperatures over open water. As a result, sometimes, certain ice concentrations are calculated over open water covered with heavy clouds. The authors call this kind of area as “false sea ice” and the phenomenon is called the weather effect. In the AMSR2 ice concentration product, a weather filter is used to reduce the weather effect. However, it is known that false sea ice appears occasionally in some areas even in the summertime in AMSR2 ice concentration products. In this study, the authors have modified the original weather filter and added a new weather filter utilizing the following two equations which are TB(23GHzV)<−0.75×(TB(36GHzV)−TB(36GHzH))+253K and TB(36GHzV)−TB(36GHzH) < 57K. If the brightness temperature of the pixel meets the above two equations, we set the ice concentration of the pixel as 0%. By adding the new weather filter, most of the false sea ice that appeared in the ASMR2 ice concentration products could be rejected. JAXA has decided to add this weather filter for producing AMSR2 standard sea ice concentration products.
format Text
author Cho, K.
Naoki, K.
spellingShingle Cho, K.
Naoki, K.
A NEW WEATHER FILTER FOR REDUCING WEATHER EFFECT IN CALCULATING SEA ICE CONCENTRATION FROM AMSR2 DATA
author_facet Cho, K.
Naoki, K.
author_sort Cho, K.
title A NEW WEATHER FILTER FOR REDUCING WEATHER EFFECT IN CALCULATING SEA ICE CONCENTRATION FROM AMSR2 DATA
title_short A NEW WEATHER FILTER FOR REDUCING WEATHER EFFECT IN CALCULATING SEA ICE CONCENTRATION FROM AMSR2 DATA
title_full A NEW WEATHER FILTER FOR REDUCING WEATHER EFFECT IN CALCULATING SEA ICE CONCENTRATION FROM AMSR2 DATA
title_fullStr A NEW WEATHER FILTER FOR REDUCING WEATHER EFFECT IN CALCULATING SEA ICE CONCENTRATION FROM AMSR2 DATA
title_full_unstemmed A NEW WEATHER FILTER FOR REDUCING WEATHER EFFECT IN CALCULATING SEA ICE CONCENTRATION FROM AMSR2 DATA
title_sort new weather filter for reducing weather effect in calculating sea ice concentration from amsr2 data
publishDate 2023
url https://doi.org/10.5194/isprs-annals-X-1-W1-2023-793-2023
https://isprs-annals.copernicus.org/articles/X-1-W1-2023/793/2023/
genre Sea ice
genre_facet Sea ice
op_source eISSN: 2194-9050
op_relation doi:10.5194/isprs-annals-X-1-W1-2023-793-2023
https://isprs-annals.copernicus.org/articles/X-1-W1-2023/793/2023/
op_doi https://doi.org/10.5194/isprs-annals-X-1-W1-2023-793-2023
container_title ISPRS Annals of the Photogrammetry, Remote Sensing and Spatial Information Sciences
container_volume X-1/W1-2023
container_start_page 793
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