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北极海冰的年代际转型与中国冻雨年代际变化的关系

牛璐 黄菲 周晓

牛璐, 黄菲, 周晓. 北极海冰的年代际转型与中国冻雨年代际变化的关系[J]. 海洋学报, 2015, 37(11): 105-117. doi: 10.3969/j.issn.0253-4193.2015.11.010
引用本文: 牛璐, 黄菲, 周晓. 北极海冰的年代际转型与中国冻雨年代际变化的关系[J]. 海洋学报, 2015, 37(11): 105-117. doi: 10.3969/j.issn.0253-4193.2015.11.010
Niulu, Huang Fei, Zhou Xiao. Decadal regime shift of Arctic sea ice and associated decadal variability of Chinese freezing rain[J]. Haiyang Xuebao, 2015, 37(11): 105-117. doi: 10.3969/j.issn.0253-4193.2015.11.010
Citation: Niulu, Huang Fei, Zhou Xiao. Decadal regime shift of Arctic sea ice and associated decadal variability of Chinese freezing rain[J]. Haiyang Xuebao, 2015, 37(11): 105-117. doi: 10.3969/j.issn.0253-4193.2015.11.010

北极海冰的年代际转型与中国冻雨年代际变化的关系

doi: 10.3969/j.issn.0253-4193.2015.11.010
基金项目: 全球变化研究国家重大科学研究计划项目(2015CB953904,2012CB955604);国家自然科学基金委员会-山东省人民政府联合资助海洋科学研究中心项目(U1406401)。

Decadal regime shift of Arctic sea ice and associated decadal variability of Chinese freezing rain

  • 摘要: 基于1961-2013年HadISST海冰密集度资料,定义了北极海冰的季节性融冰指数,结果显示近几十年来北极季节性融冰范围呈显著的上升趋势,并分别在20世纪70年代末和90年代中期存在显著的年代际转型,相应地,中国冻雨发生频数总体上呈现出显著的减少趋势,但也存在显著的年代际转型。在20世纪70年代末之前,北极季节性融冰范围较小但显著增长,中国冻雨频数年际变化振幅较大,且主要受巴伦支海、喀拉海海冰的影响;20世纪70年代末至90年代中期北极季节性融冰范围维持振荡特征,没有显著的线性趋势,中国冻雨频数变化振幅减小,与北极海冰相关较弱,主要相关因子为北大西洋及北太平洋海表温度变化;而90年代中期以后,北极海冰融化加快,特别是2007年以后,季节性融冰范围大大增加,而中国冻雨频数处于低发时段,其变化与太平洋扇区海冰及堪察加半岛附近海温呈显著负相关,季节性融冰的显著区域也从东西伯利亚海逆时针旋转向波弗特海-加拿大群岛北部扩张,同时向北极中央区扩张。不同年代影响冻雨的海温或海冰关键海区不同,产生特定的大气环流异常响应,进而影响到我国冻雨。
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  • 收稿日期:  2015-04-16

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