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作 者:佟欣怡 吴秀兰 李元鹏[1] 陈颖[1] 贾孜拉·拜山 TONG Xinyi;WU Xiulan;LI Yuanpeng;CHEN Ying;Jiazila Baishan(Xinjiang Climate Center,Urumqi 830002,China)
出 处:《沙漠与绿洲气象》2023年第5期127-133,共7页Desert and Oasis Meteorology
基 金:新疆气象局创新发展专项面上项目(MS202302);新疆维吾尔自治区自然科学基金面上项目(2021D01A149);新疆气象局科研课题项目(Q201909)。
摘 要:利用1961年12月—2022年2月新疆冬季气温、北极海冰等资料,探讨北极海冰变化影响新疆冬季气温的物理模态、影响机制。结果表明:北极海冰的变化与新疆大部冬季气温呈正相关,北极海冰变化通过改变北半球大气高低空配置进而影响新疆冬季气温。格陵兰海—丹麦海峡、拉普捷夫海—东西伯利亚海海冰异常偏多时,新疆大部冬季气温偏高。巴伦支海—喀拉海、鄂霍次克海—白令海峡、哈德孙湾—戴维斯海峡海冰异常偏多时,新疆大部冬季气温偏低。Based on the data of the winter temperature and Arctic sea ice in Xinjiang from December 1961 to February 2022,the physical mode and mechanism of Arctic sea ice changes affecting Xinjiang winter temperature are discussed.The results show that the changes in Arctic sea ice is positively correlated with the winter temperature in most of Xinjiang.The changes of Arctic sea ice affects the winter temperature in Xinjiang by changing the circulation configuration between upper and lower levels in the northern hemisphere.When the sea ice is above normal in Greenland Sea-Denmark Strait,Laptev Sea-East Siberia Sea,there would be warmer than usual in the most of Xinjiang.However,when the sea ice is above normal in the Barents Sea-Kara Sea,the Sea of Okhotsk-Bering Strait,Hudson Bay-Davis Strait,the winter temperature would be lower than usual in the most of Xinjiang.
分 类 号:P461.6[天文地球—大气科学及气象学]
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