Feasibility of retrieving Arctic sea ice thickness from the Chinese HY-2B Ku-band radar altimeter

With the continuous development of the China ocean dynamic environment satellite series (Haiyang-2, HY-2), it is urgent to explore the potential application of HY-2B in Arctic sea ice thickness retrievals. In this study, we first derive the Arctic radar freeboard and sea ice thickness during two cyc...

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Published in:The Cryosphere
Main Authors: Dong, Zhaoqing, Shi, Lijian, Lin, Mingsen, Jia, Yongjun, Zeng, Tao, Wu, Suhui
Format: Text
Language:English
Published: 2023
Subjects:
Online Access:https://doi.org/10.5194/tc-17-1389-2023
https://tc.copernicus.org/articles/17/1389/2023/
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spelling ftcopernicus:oai:publications.copernicus.org:tc106150 2023-05-15T14:59:08+02:00 Feasibility of retrieving Arctic sea ice thickness from the Chinese HY-2B Ku-band radar altimeter Dong, Zhaoqing Shi, Lijian Lin, Mingsen Jia, Yongjun Zeng, Tao Wu, Suhui 2023-03-31 application/pdf https://doi.org/10.5194/tc-17-1389-2023 https://tc.copernicus.org/articles/17/1389/2023/ eng eng doi:10.5194/tc-17-1389-2023 https://tc.copernicus.org/articles/17/1389/2023/ eISSN: 1994-0424 Text 2023 ftcopernicus https://doi.org/10.5194/tc-17-1389-2023 2023-04-03T16:23:10Z With the continuous development of the China ocean dynamic environment satellite series (Haiyang-2, HY-2), it is urgent to explore the potential application of HY-2B in Arctic sea ice thickness retrievals. In this study, we first derive the Arctic radar freeboard and sea ice thickness during two cycles (from October 2019 to April 2020 and from October 2020 to April 2021) using the HY-2B radar altimeter and compare the results with the Alfred Wegener Institute (AWI) CryoSat-2 (CS-2) products. We evaluate our HY-2B sea ice freeboard and thickness products using Operation IceBridge (OIB) airborne data and Ice, Cloud, and land Elevation Satellite 2 (ICESat-2) products. Finally, we estimate the uncertainties in the HY-2B sea ice freeboard and sea ice thickness. Here, we derive the radar freeboard by calculating the difference between the relative elevation of the floe obtained by subtracting the mean sea surface (MSS) height and sea surface height anomaly (SSHA) determined by an average of the 15 lowest points method. The radar freeboard deviation between HY-2B and CS-2 is within 0.02 m, whereas the sea ice thickness deviation between HY-2B and CS-2 is within 0.2 m. The HY-2B radar freeboards are generally thicker than AWI CS-2, except in spring (March and April). A spring segment likely has more floe points than an early winter segment. We also find that the deviations in radar freeboard and sea ice thickness between HY-2B and CS-2 over multiyear ice (MYI) are larger than those over first-year ice (FYI). The correlation between HY-2B (CS-2) sea ice freeboard retrievals and OIB values is 0.77 (0.84), with a root mean square error (RMSE) of 0.13 (0.10) m and a mean absolute error (MAE) of 0.12 (0.081) m. The correlation between HY-2B (CS-2) sea ice thickness retrievals and OIB values is 0.65 (0.80), with an RMSE of 1.86 (1.00) m and an MAE of 1.72 (0.75) m. The HY-2B sea ice freeboard uncertainty values range from 0.021 to 0.027 m, while the uncertainties in the HY-2B sea ice thickness range from 0.61 to 0.74 m. The ... Text Arctic Sea ice Copernicus Publications: E-Journals Arctic The Cryosphere 17 3 1389 1410
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description With the continuous development of the China ocean dynamic environment satellite series (Haiyang-2, HY-2), it is urgent to explore the potential application of HY-2B in Arctic sea ice thickness retrievals. In this study, we first derive the Arctic radar freeboard and sea ice thickness during two cycles (from October 2019 to April 2020 and from October 2020 to April 2021) using the HY-2B radar altimeter and compare the results with the Alfred Wegener Institute (AWI) CryoSat-2 (CS-2) products. We evaluate our HY-2B sea ice freeboard and thickness products using Operation IceBridge (OIB) airborne data and Ice, Cloud, and land Elevation Satellite 2 (ICESat-2) products. Finally, we estimate the uncertainties in the HY-2B sea ice freeboard and sea ice thickness. Here, we derive the radar freeboard by calculating the difference between the relative elevation of the floe obtained by subtracting the mean sea surface (MSS) height and sea surface height anomaly (SSHA) determined by an average of the 15 lowest points method. The radar freeboard deviation between HY-2B and CS-2 is within 0.02 m, whereas the sea ice thickness deviation between HY-2B and CS-2 is within 0.2 m. The HY-2B radar freeboards are generally thicker than AWI CS-2, except in spring (March and April). A spring segment likely has more floe points than an early winter segment. We also find that the deviations in radar freeboard and sea ice thickness between HY-2B and CS-2 over multiyear ice (MYI) are larger than those over first-year ice (FYI). The correlation between HY-2B (CS-2) sea ice freeboard retrievals and OIB values is 0.77 (0.84), with a root mean square error (RMSE) of 0.13 (0.10) m and a mean absolute error (MAE) of 0.12 (0.081) m. The correlation between HY-2B (CS-2) sea ice thickness retrievals and OIB values is 0.65 (0.80), with an RMSE of 1.86 (1.00) m and an MAE of 1.72 (0.75) m. The HY-2B sea ice freeboard uncertainty values range from 0.021 to 0.027 m, while the uncertainties in the HY-2B sea ice thickness range from 0.61 to 0.74 m. The ...
format Text
author Dong, Zhaoqing
Shi, Lijian
Lin, Mingsen
Jia, Yongjun
Zeng, Tao
Wu, Suhui
spellingShingle Dong, Zhaoqing
Shi, Lijian
Lin, Mingsen
Jia, Yongjun
Zeng, Tao
Wu, Suhui
Feasibility of retrieving Arctic sea ice thickness from the Chinese HY-2B Ku-band radar altimeter
author_facet Dong, Zhaoqing
Shi, Lijian
Lin, Mingsen
Jia, Yongjun
Zeng, Tao
Wu, Suhui
author_sort Dong, Zhaoqing
title Feasibility of retrieving Arctic sea ice thickness from the Chinese HY-2B Ku-band radar altimeter
title_short Feasibility of retrieving Arctic sea ice thickness from the Chinese HY-2B Ku-band radar altimeter
title_full Feasibility of retrieving Arctic sea ice thickness from the Chinese HY-2B Ku-band radar altimeter
title_fullStr Feasibility of retrieving Arctic sea ice thickness from the Chinese HY-2B Ku-band radar altimeter
title_full_unstemmed Feasibility of retrieving Arctic sea ice thickness from the Chinese HY-2B Ku-band radar altimeter
title_sort feasibility of retrieving arctic sea ice thickness from the chinese hy-2b ku-band radar altimeter
publishDate 2023
url https://doi.org/10.5194/tc-17-1389-2023
https://tc.copernicus.org/articles/17/1389/2023/
geographic Arctic
geographic_facet Arctic
genre Arctic
Sea ice
genre_facet Arctic
Sea ice
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-17-1389-2023
https://tc.copernicus.org/articles/17/1389/2023/
op_doi https://doi.org/10.5194/tc-17-1389-2023
container_title The Cryosphere
container_volume 17
container_issue 3
container_start_page 1389
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