Arctic Sea Ice Concentration Assimilation in an Operational Global 1/10° Ocean Forecast System

To understand the Arctic environment, which is closely related to sea ice and to reduce potential risks, reliable sea ice forecasts are indispensable. A practical, lightweight yet effective assimilation scheme of sea ice concentration based on Optimal Interpolation is designed and adopted in an oper...

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Published in:Remote Sensing
Main Authors: Qiuli Shao, Qi Shu, Bin Xiao, Lujun Zhang, Xunqiang Yin, Fangli Qiao
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2023
Subjects:
Online Access:https://doi.org/10.3390/rs15051274
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spelling ftmdpi:oai:mdpi.com:/2072-4292/15/5/1274/ 2023-08-20T04:04:04+02:00 Arctic Sea Ice Concentration Assimilation in an Operational Global 1/10° Ocean Forecast System Qiuli Shao Qi Shu Bin Xiao Lujun Zhang Xunqiang Yin Fangli Qiao agris 2023-02-25 application/pdf https://doi.org/10.3390/rs15051274 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/rs15051274 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 15; Issue 5; Pages: 1274 sea ice concentration data assimilation global ocean forecasting system Text 2023 ftmdpi https://doi.org/10.3390/rs15051274 2023-08-01T08:59:38Z To understand the Arctic environment, which is closely related to sea ice and to reduce potential risks, reliable sea ice forecasts are indispensable. A practical, lightweight yet effective assimilation scheme of sea ice concentration based on Optimal Interpolation is designed and adopted in an operational global 1/10° surface wave-tide-circulation coupled ocean model (FIO-COM10) forecasting system to improve Arctic sea ice forecasting. Twin numerical experiments with and without data assimilation are designed for the simulation of the year 2019, and 5-day real-time forecasts for 2021 are implemented to study the sea ice forecast ability. The results show that the large biases in the simulation and forecast of sea ice concentration are remarkably reduced due to satellite observation uncertainty levels by data assimilation, indicating the high efficiency of the data assimilation scheme. The most significant improvement occurs in the marginal ice zones. The sea surface temperature bias averaged over the marginal ice zones is also reduced by 0.9 °C. Sea ice concentration assimilation has a profound effect on improving forecasting ability. The Root Mean Square Error and Integrated Ice-Edge Error are reduced to the level of the independent satellite observation at least for 24-h forecast, and sea ice forecast by FIO-COM10 has better performance than the persistence forecasts in summer and autumn. Text Arctic Sea ice MDPI Open Access Publishing Arctic Remote Sensing 15 5 1274
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic sea ice concentration
data assimilation
global ocean forecasting system
spellingShingle sea ice concentration
data assimilation
global ocean forecasting system
Qiuli Shao
Qi Shu
Bin Xiao
Lujun Zhang
Xunqiang Yin
Fangli Qiao
Arctic Sea Ice Concentration Assimilation in an Operational Global 1/10° Ocean Forecast System
topic_facet sea ice concentration
data assimilation
global ocean forecasting system
description To understand the Arctic environment, which is closely related to sea ice and to reduce potential risks, reliable sea ice forecasts are indispensable. A practical, lightweight yet effective assimilation scheme of sea ice concentration based on Optimal Interpolation is designed and adopted in an operational global 1/10° surface wave-tide-circulation coupled ocean model (FIO-COM10) forecasting system to improve Arctic sea ice forecasting. Twin numerical experiments with and without data assimilation are designed for the simulation of the year 2019, and 5-day real-time forecasts for 2021 are implemented to study the sea ice forecast ability. The results show that the large biases in the simulation and forecast of sea ice concentration are remarkably reduced due to satellite observation uncertainty levels by data assimilation, indicating the high efficiency of the data assimilation scheme. The most significant improvement occurs in the marginal ice zones. The sea surface temperature bias averaged over the marginal ice zones is also reduced by 0.9 °C. Sea ice concentration assimilation has a profound effect on improving forecasting ability. The Root Mean Square Error and Integrated Ice-Edge Error are reduced to the level of the independent satellite observation at least for 24-h forecast, and sea ice forecast by FIO-COM10 has better performance than the persistence forecasts in summer and autumn.
format Text
author Qiuli Shao
Qi Shu
Bin Xiao
Lujun Zhang
Xunqiang Yin
Fangli Qiao
author_facet Qiuli Shao
Qi Shu
Bin Xiao
Lujun Zhang
Xunqiang Yin
Fangli Qiao
author_sort Qiuli Shao
title Arctic Sea Ice Concentration Assimilation in an Operational Global 1/10° Ocean Forecast System
title_short Arctic Sea Ice Concentration Assimilation in an Operational Global 1/10° Ocean Forecast System
title_full Arctic Sea Ice Concentration Assimilation in an Operational Global 1/10° Ocean Forecast System
title_fullStr Arctic Sea Ice Concentration Assimilation in an Operational Global 1/10° Ocean Forecast System
title_full_unstemmed Arctic Sea Ice Concentration Assimilation in an Operational Global 1/10° Ocean Forecast System
title_sort arctic sea ice concentration assimilation in an operational global 1/10° ocean forecast system
publisher Multidisciplinary Digital Publishing Institute
publishDate 2023
url https://doi.org/10.3390/rs15051274
op_coverage agris
geographic Arctic
geographic_facet Arctic
genre Arctic
Sea ice
genre_facet Arctic
Sea ice
op_source Remote Sensing; Volume 15; Issue 5; Pages: 1274
op_relation https://dx.doi.org/10.3390/rs15051274
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/rs15051274
container_title Remote Sensing
container_volume 15
container_issue 5
container_start_page 1274
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