Evaluation of Arctic Sea Ice Thickness from a Parameter-Optimized Arctic Sea Ice–Ocean Model
Sea ice thickness (SIT) presents comprehensive information on Arctic sea ice changes and their role in the climate system. However, our understanding of SIT is limited by a scarcity of observations and inaccurate model simulations. Based on simultaneous parameter optimization with a micro genetic al...
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ftmdpi:oai:mdpi.com:/2072-4292/15/10/2537/ 2023-08-20T04:03:22+02:00 Evaluation of Arctic Sea Ice Thickness from a Parameter-Optimized Arctic Sea Ice–Ocean Model Qiaoqiao Zhang Hao Luo Chao Min Yongwu Xiu Qian Shi Qinghua Yang agris 2023-05-12 application/pdf https://doi.org/10.3390/rs15102537 EN eng Multidisciplinary Digital Publishing Institute Earth Observation for Emergency Management https://dx.doi.org/10.3390/rs15102537 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 15; Issue 10; Pages: 2537 sea ice thickness Arctic model parameter optimization NAOSIM CS2SMOS Text 2023 ftmdpi https://doi.org/10.3390/rs15102537 2023-08-01T10:02:45Z Sea ice thickness (SIT) presents comprehensive information on Arctic sea ice changes and their role in the climate system. However, our understanding of SIT is limited by a scarcity of observations and inaccurate model simulations. Based on simultaneous parameter optimization with a micro genetic algorithm, the North Atlantic/Arctic Ocean–Sea Ice Model (NAOSIM) has already demonstrated advantages in Arctic sea ice simulations. However, its performance in simulating pan-Arctic SITs remains unclear. In this study, a further evaluation of Arctic SITs from NAOSIM was conducted based on a comparison with satellite and in situ observations. Generally, NAOSIM can reproduce the annual cycle and downward trend in the sea ice volume. However, deficiencies can still be found in the simulation of SIT spatial patterns. NAOSIM overestimates the SIT of thinner ice (<1.5 m) in the Beaufort Sea, underestimates the SIT of thick ice (>1.5 m) in the central Arctic and is unable to capture the upward trend in the SIT in the north of the Canadian Archipelago as well as to reproduce the intensity of the observed SIT variability. In terms of SIT simulation, NAOSIM performs better as the time approaches the optimization window (2000–2012). Therefore, in the context of rapid changes in Arctic sea ice, how to optimize this model based on limited observations still remains a challenge. Text Arctic Arctic Ocean Atlantic Arctic Atlantic-Arctic Beaufort Sea Canadian Archipelago North Atlantic Sea ice MDPI Open Access Publishing Arctic Arctic Ocean Remote Sensing 15 10 2537 |
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Open Polar |
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MDPI Open Access Publishing |
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ftmdpi |
language |
English |
topic |
sea ice thickness Arctic model parameter optimization NAOSIM CS2SMOS |
spellingShingle |
sea ice thickness Arctic model parameter optimization NAOSIM CS2SMOS Qiaoqiao Zhang Hao Luo Chao Min Yongwu Xiu Qian Shi Qinghua Yang Evaluation of Arctic Sea Ice Thickness from a Parameter-Optimized Arctic Sea Ice–Ocean Model |
topic_facet |
sea ice thickness Arctic model parameter optimization NAOSIM CS2SMOS |
description |
Sea ice thickness (SIT) presents comprehensive information on Arctic sea ice changes and their role in the climate system. However, our understanding of SIT is limited by a scarcity of observations and inaccurate model simulations. Based on simultaneous parameter optimization with a micro genetic algorithm, the North Atlantic/Arctic Ocean–Sea Ice Model (NAOSIM) has already demonstrated advantages in Arctic sea ice simulations. However, its performance in simulating pan-Arctic SITs remains unclear. In this study, a further evaluation of Arctic SITs from NAOSIM was conducted based on a comparison with satellite and in situ observations. Generally, NAOSIM can reproduce the annual cycle and downward trend in the sea ice volume. However, deficiencies can still be found in the simulation of SIT spatial patterns. NAOSIM overestimates the SIT of thinner ice (<1.5 m) in the Beaufort Sea, underestimates the SIT of thick ice (>1.5 m) in the central Arctic and is unable to capture the upward trend in the SIT in the north of the Canadian Archipelago as well as to reproduce the intensity of the observed SIT variability. In terms of SIT simulation, NAOSIM performs better as the time approaches the optimization window (2000–2012). Therefore, in the context of rapid changes in Arctic sea ice, how to optimize this model based on limited observations still remains a challenge. |
format |
Text |
author |
Qiaoqiao Zhang Hao Luo Chao Min Yongwu Xiu Qian Shi Qinghua Yang |
author_facet |
Qiaoqiao Zhang Hao Luo Chao Min Yongwu Xiu Qian Shi Qinghua Yang |
author_sort |
Qiaoqiao Zhang |
title |
Evaluation of Arctic Sea Ice Thickness from a Parameter-Optimized Arctic Sea Ice–Ocean Model |
title_short |
Evaluation of Arctic Sea Ice Thickness from a Parameter-Optimized Arctic Sea Ice–Ocean Model |
title_full |
Evaluation of Arctic Sea Ice Thickness from a Parameter-Optimized Arctic Sea Ice–Ocean Model |
title_fullStr |
Evaluation of Arctic Sea Ice Thickness from a Parameter-Optimized Arctic Sea Ice–Ocean Model |
title_full_unstemmed |
Evaluation of Arctic Sea Ice Thickness from a Parameter-Optimized Arctic Sea Ice–Ocean Model |
title_sort |
evaluation of arctic sea ice thickness from a parameter-optimized arctic sea ice–ocean model |
publisher |
Multidisciplinary Digital Publishing Institute |
publishDate |
2023 |
url |
https://doi.org/10.3390/rs15102537 |
op_coverage |
agris |
geographic |
Arctic Arctic Ocean |
geographic_facet |
Arctic Arctic Ocean |
genre |
Arctic Arctic Ocean Atlantic Arctic Atlantic-Arctic Beaufort Sea Canadian Archipelago North Atlantic Sea ice |
genre_facet |
Arctic Arctic Ocean Atlantic Arctic Atlantic-Arctic Beaufort Sea Canadian Archipelago North Atlantic Sea ice |
op_source |
Remote Sensing; Volume 15; Issue 10; Pages: 2537 |
op_relation |
Earth Observation for Emergency Management https://dx.doi.org/10.3390/rs15102537 |
op_rights |
https://creativecommons.org/licenses/by/4.0/ |
op_doi |
https://doi.org/10.3390/rs15102537 |
container_title |
Remote Sensing |
container_volume |
15 |
container_issue |
10 |
container_start_page |
2537 |
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1774713735636582400 |