Retrieval of Arctic Sea Ice Motion from FY-3D/MWRI Brightness Temperature Data
Sea ice motion (SIM) has significant implications for sea–air interactions, thermohaline circulation, and the development of the Arctic passage. This research proposes an improved SIM retrieval method from Fengyun-3D’s (FY-3D) microwave radiometer imager’s (MWRI) brightness temperature (T<i>&l...
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MDPI AG
2023-08-01
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Online Access: | https://www.mdpi.com/2072-4292/15/17/4191 |
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author | Haihua Chen Kun Ni Jun Liu Lele Li |
author_facet | Haihua Chen Kun Ni Jun Liu Lele Li |
author_sort | Haihua Chen |
collection | DOAJ |
description | Sea ice motion (SIM) has significant implications for sea–air interactions, thermohaline circulation, and the development of the Arctic passage. This research proposes an improved SIM retrieval method from Fengyun-3D’s (FY-3D) microwave radiometer imager’s (MWRI) brightness temperature (T<i><sub>b</sub></i>) data based on the modified classical maximum cross-correlation (MCC) method and the multisource data merging method. This study utilized buoy data to establish the search area range, applied distinct thresholds across various Arctic regions, and merged the buoy data, reanalysis wind data, and SIM retrieved from FY-3D/MWRI T<i><sub>b</sub></i> data. In 2019, for the final Arctic SIM results retrieved from the MWRI 89 GHz and 36.5 GHz T<i><sub>b</sub></i> data, the root-mean-square error (RMSE) and the mean average error (MAE) in the east–west direction were 2.07 cm/s and 1.38 cm/s and those in the north–south direction were 1.96 cm/s and 1.15 cm/s, compared to the ice-tethered profiler (ITP) data. Compared with the daily average data of the National Snow and Ice Data Center (NSIDC), the RMSE and MAE of the SIM results obtained in this study were 0.74 cm/s and 0.93 cm/s in the east–west direction, and 0.56 cm/s and 0.72 cm/s in the north–south direction, respectively. The monthly average of the SIM retrieved from the MWRI T<i><sub>b</sub></i> data in this research also showed a good agreement with the monthly average of the NSIDC SIM product. The comparison showed that the MWRI T<i><sub>b</sub></i> data could be used to retrieve the Arctic SIM, and the Arctic SIM retrieval method presented in this paper was accurate and general. |
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language | English |
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publishDate | 2023-08-01 |
publisher | MDPI AG |
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series | Remote Sensing |
spelling | doaj.art-c7054b61aeae4bdf872da1ecdcb82e7c2023-11-19T08:45:43ZengMDPI AGRemote Sensing2072-42922023-08-011517419110.3390/rs15174191Retrieval of Arctic Sea Ice Motion from FY-3D/MWRI Brightness Temperature DataHaihua Chen0Kun Ni1Jun Liu2Lele Li3College of Marine Technology, Faculty of Information Science and Engineering, Ocean University of China, Qingdao 266100, ChinaCollege of Marine Technology, Faculty of Information Science and Engineering, Ocean University of China, Qingdao 266100, ChinaCollege of Marine Technology, Faculty of Information Science and Engineering, Ocean University of China, Qingdao 266100, ChinaCollege of Marine Technology, Faculty of Information Science and Engineering, Ocean University of China, Qingdao 266100, ChinaSea ice motion (SIM) has significant implications for sea–air interactions, thermohaline circulation, and the development of the Arctic passage. This research proposes an improved SIM retrieval method from Fengyun-3D’s (FY-3D) microwave radiometer imager’s (MWRI) brightness temperature (T<i><sub>b</sub></i>) data based on the modified classical maximum cross-correlation (MCC) method and the multisource data merging method. This study utilized buoy data to establish the search area range, applied distinct thresholds across various Arctic regions, and merged the buoy data, reanalysis wind data, and SIM retrieved from FY-3D/MWRI T<i><sub>b</sub></i> data. In 2019, for the final Arctic SIM results retrieved from the MWRI 89 GHz and 36.5 GHz T<i><sub>b</sub></i> data, the root-mean-square error (RMSE) and the mean average error (MAE) in the east–west direction were 2.07 cm/s and 1.38 cm/s and those in the north–south direction were 1.96 cm/s and 1.15 cm/s, compared to the ice-tethered profiler (ITP) data. Compared with the daily average data of the National Snow and Ice Data Center (NSIDC), the RMSE and MAE of the SIM results obtained in this study were 0.74 cm/s and 0.93 cm/s in the east–west direction, and 0.56 cm/s and 0.72 cm/s in the north–south direction, respectively. The monthly average of the SIM retrieved from the MWRI T<i><sub>b</sub></i> data in this research also showed a good agreement with the monthly average of the NSIDC SIM product. The comparison showed that the MWRI T<i><sub>b</sub></i> data could be used to retrieve the Arctic SIM, and the Arctic SIM retrieval method presented in this paper was accurate and general.https://www.mdpi.com/2072-4292/15/17/4191arctic sea ice motion (SIM)FY-3D/MWRIbrightness temperaturemaximum cross-correlation |
spellingShingle | Haihua Chen Kun Ni Jun Liu Lele Li Retrieval of Arctic Sea Ice Motion from FY-3D/MWRI Brightness Temperature Data Remote Sensing arctic sea ice motion (SIM) FY-3D/MWRI brightness temperature maximum cross-correlation |
title | Retrieval of Arctic Sea Ice Motion from FY-3D/MWRI Brightness Temperature Data |
title_full | Retrieval of Arctic Sea Ice Motion from FY-3D/MWRI Brightness Temperature Data |
title_fullStr | Retrieval of Arctic Sea Ice Motion from FY-3D/MWRI Brightness Temperature Data |
title_full_unstemmed | Retrieval of Arctic Sea Ice Motion from FY-3D/MWRI Brightness Temperature Data |
title_short | Retrieval of Arctic Sea Ice Motion from FY-3D/MWRI Brightness Temperature Data |
title_sort | retrieval of arctic sea ice motion from fy 3d mwri brightness temperature data |
topic | arctic sea ice motion (SIM) FY-3D/MWRI brightness temperature maximum cross-correlation |
url | https://www.mdpi.com/2072-4292/15/17/4191 |
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