Preceding winter Okhotsk Sea ice as a precursor to the following winter extreme precipitation in South China

Abstract The winter extreme precipitation over South China (SC) experiences a large year‐to‐year variability, causing uncertainty in its prediction. Here, we find that the boreal winter sea ice concentration (SIC) in the Okhotsk Sea can serve as a precursor to the following winter's extreme pre...

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Main Authors: Kai Ji, Zhongshi Zhang, Ruiqiang Ding, Jianping Li, Yurun Tian, Yongqi Gao, Jiayu Zheng
Format: Article
Language:English
Published: Wiley 2022-08-01
Series:Atmospheric Science Letters
Subjects:
Online Access:https://doi.org/10.1002/asl.1095
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author Kai Ji
Zhongshi Zhang
Ruiqiang Ding
Jianping Li
Yurun Tian
Yongqi Gao
Jiayu Zheng
author_facet Kai Ji
Zhongshi Zhang
Ruiqiang Ding
Jianping Li
Yurun Tian
Yongqi Gao
Jiayu Zheng
author_sort Kai Ji
collection DOAJ
description Abstract The winter extreme precipitation over South China (SC) experiences a large year‐to‐year variability, causing uncertainty in its prediction. Here, we find that the boreal winter sea ice concentration (SIC) in the Okhotsk Sea can serve as a precursor to the following winter's extreme precipitation frequency (EPF) over SC, which has important implications for its prediction. Further analysis reveals that the Okhotsk Sea SIC anomalies help to reinforce North Pacific Oscillation‐like atmospheric variability over the North Pacific, which induces the development of El Niño‐Southern Oscillation (ENSO)‐like SST anomalies in the equatorial eastern Pacific. The ENSO may act as a “power amplifier” to boost the impact of the Okhotsk Sea winter SIC anomalies on the following winter EPF over SC via a positive atmosphere–ocean feedback process. Our findings suggest that the Okhotsk Sea SIC may act as a potential precursor for the winter EPF over SC leading by about 1 year, and further improve our understanding of extratropical‐tropical interactions and aid predictability of winter extreme precipitation over SC.
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spelling doaj.art-ea89a6aecdd148fea9682dc47586efa22022-12-22T02:06:05ZengWileyAtmospheric Science Letters1530-261X2022-08-01238n/an/a10.1002/asl.1095Preceding winter Okhotsk Sea ice as a precursor to the following winter extreme precipitation in South ChinaKai Ji0Zhongshi Zhang1Ruiqiang Ding2Jianping Li3Yurun Tian4Yongqi Gao5Jiayu Zheng6Department of Atmospheric Science School of Environmental Studies, China University of Geosciences Wuhan ChinaDepartment of Atmospheric Science School of Environmental Studies, China University of Geosciences Wuhan ChinaState Key Laboratory of Earth Surface Processes and Resource Ecology Beijing Normal University Beijing ChinaLaboratory for Regional Oceanography and Numerical Modeling Qingdao National Laboratory for Marine Science and Technology Qingdao ChinaNansen‐Zhu International Research Center Institute of Atmospheric Physics, Chinese Academy of Sciences Beijing ChinaNansen Environmental and Remote Sensing Center/Bjerknes Center for Climate Research Bergen NorwayState Key Laboratory of Tropical Oceanography South China Sea Institute of Oceanology, Chinese Academy of Sciences Guangzhou ChinaAbstract The winter extreme precipitation over South China (SC) experiences a large year‐to‐year variability, causing uncertainty in its prediction. Here, we find that the boreal winter sea ice concentration (SIC) in the Okhotsk Sea can serve as a precursor to the following winter's extreme precipitation frequency (EPF) over SC, which has important implications for its prediction. Further analysis reveals that the Okhotsk Sea SIC anomalies help to reinforce North Pacific Oscillation‐like atmospheric variability over the North Pacific, which induces the development of El Niño‐Southern Oscillation (ENSO)‐like SST anomalies in the equatorial eastern Pacific. The ENSO may act as a “power amplifier” to boost the impact of the Okhotsk Sea winter SIC anomalies on the following winter EPF over SC via a positive atmosphere–ocean feedback process. Our findings suggest that the Okhotsk Sea SIC may act as a potential precursor for the winter EPF over SC leading by about 1 year, and further improve our understanding of extratropical‐tropical interactions and aid predictability of winter extreme precipitation over SC.https://doi.org/10.1002/asl.1095air–sea–ice interactionsOkhotsk Seasea ice concentrationwinter extreme precipitation frequency
spellingShingle Kai Ji
Zhongshi Zhang
Ruiqiang Ding
Jianping Li
Yurun Tian
Yongqi Gao
Jiayu Zheng
Preceding winter Okhotsk Sea ice as a precursor to the following winter extreme precipitation in South China
Atmospheric Science Letters
air–sea–ice interactions
Okhotsk Sea
sea ice concentration
winter extreme precipitation frequency
title Preceding winter Okhotsk Sea ice as a precursor to the following winter extreme precipitation in South China
title_full Preceding winter Okhotsk Sea ice as a precursor to the following winter extreme precipitation in South China
title_fullStr Preceding winter Okhotsk Sea ice as a precursor to the following winter extreme precipitation in South China
title_full_unstemmed Preceding winter Okhotsk Sea ice as a precursor to the following winter extreme precipitation in South China
title_short Preceding winter Okhotsk Sea ice as a precursor to the following winter extreme precipitation in South China
title_sort preceding winter okhotsk sea ice as a precursor to the following winter extreme precipitation in south china
topic air–sea–ice interactions
Okhotsk Sea
sea ice concentration
winter extreme precipitation frequency
url https://doi.org/10.1002/asl.1095
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