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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Main Authors: Qiuli Shao, Qi Shu, Bin Xiao, Lujun Zhang, Xunqiang Yin, Fangli Qiao
Format: Article
Language:English
Published: MDPI AG 2023-02-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/15/5/1274
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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
collection DOAJ
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.
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spelling doaj.art-0aed6332bf8a46328eec9f9fe26bb6df2023-11-17T08:30:49ZengMDPI AGRemote Sensing2072-42922023-02-01155127410.3390/rs15051274Arctic Sea Ice Concentration Assimilation in an Operational Global 1/10° Ocean Forecast SystemQiuli Shao0Qi Shu1Bin Xiao2Lujun Zhang3Xunqiang Yin4Fangli Qiao5Institute of Oceanographic Instrumentation, Qilu University of Technology (Shandong Academy of Sciences), Qingdao 266061, ChinaFirst Institute of Oceanography, and Key Laboratory of Marine Science and Numerical Modeling, Ministry of Natural Resources, Qingdao 266061, ChinaFirst Institute of Oceanography, and Key Laboratory of Marine Science and Numerical Modeling, Ministry of Natural Resources, Qingdao 266061, ChinaSchool of Atmospheric Sciences, Nanjing University, Nanjing 210093, ChinaFirst Institute of Oceanography, and Key Laboratory of Marine Science and Numerical Modeling, Ministry of Natural Resources, Qingdao 266061, ChinaFirst Institute of Oceanography, and Key Laboratory of Marine Science and Numerical Modeling, Ministry of Natural Resources, Qingdao 266061, ChinaTo 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.https://www.mdpi.com/2072-4292/15/5/1274sea ice concentrationdata assimilationglobal ocean forecasting system
spellingShingle 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
Remote Sensing
sea ice concentration
data assimilation
global ocean forecasting system
title 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_short 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
topic sea ice concentration
data assimilation
global ocean forecasting system
url https://www.mdpi.com/2072-4292/15/5/1274
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AT binxiao arcticseaiceconcentrationassimilationinanoperationalglobal110oceanforecastsystem
AT lujunzhang arcticseaiceconcentrationassimilationinanoperationalglobal110oceanforecastsystem
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