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中纬度瞬变涡旋活动对东亚夏季平均环流和降水的影响
引用本文:林昊雄,房佳蓓,胡海波,杨修群. 中纬度瞬变涡旋活动对东亚夏季平均环流和降水的影响[J]. 气象科学, 2021, 41(6): 739-751
作者姓名:林昊雄  房佳蓓  胡海波  杨修群
作者单位:南京大学大气科学学院,南京210023
基金项目:国家自然科学基金资助项目(41875086);国家重点研发计划项目(2018YFC1505902)
摘    要:首先利用CFSR再分析数据,分析了东亚夏季平均环流结构及瞬变涡旋活动特征,再通过WRF模式设计控制性试验和敏感性试验分别模拟受到/不受到来自北边界中纬度瞬变涡旋活动影响的东亚夏季环流和降水,通过两组试验对比揭示了瞬变涡旋活动对东亚夏季平均环流和降水的贡献.结果 表明,中纬度瞬变涡旋活动可以通过系统性的输送动量、热量、水...

关 键 词:东亚夏季环流  瞬变涡旋活动  中纬度  夏季降水  WRF模式
收稿时间:2020-12-19
修稿时间:2021-03-14

The influence of mid-latitude transient eddy activities on the summer mean circulation and precipitation in East Asia
LIN Haoxiong,FANG Jiabei,HU Haibo,YANG Xiuqun. The influence of mid-latitude transient eddy activities on the summer mean circulation and precipitation in East Asia[J]. Journal of the Meteorological Sciences, 2021, 41(6): 739-751
Authors:LIN Haoxiong  FANG Jiabei  HU Haibo  YANG Xiuqun
Affiliation:School of Atmospheric Sciences, Nanjing University, Nanjing 210023, China
Abstract:Based on the CFSR reanalysis data, the structure of summertime mean circulation and the characteristics of transient eddy activities in East Asia were firstly analyzed. Then by using the WRF model, a control run and a sensitivity run were designed to simulate the East Asian mean circulation and precipitation in summer that with/without the influence of the mid-latitude transient eddy activities from the northern boundary, respectively. The comparison between the two sets of runs reveals the contribution of transient eddy activities in the mid-latitudes to the East Asia summertime mean circulation and precipitation. Results show that the mid-latitude transient eddy activities can change the background field by systematically transporting momentum, heat, moisture and vorticity, thereby affecting the mean circulation and precipitation in summer. When the mid-latitude transient eddy activities are greatly weakened, their induced poleward momentum, heat and water vapor flux transportation are also significantly weakened. On one hand, the decreasing of poleward heat and water vapor flux transportation increases the mean temperature and water vapor in the lower layers in the eastern continent of East Asia, which provides unstable conditions and moisture conditions for precipitation. On the other hand, the change of transient eddy dynamic transportation causes an equivalent-barotropic structure response in the circulation field. The entire eastern part of China is controlled by stronger southwesterly, thus the East Asian summer monsoon strengthens and extends to further north. The combined effect of these two factors results in moisture convergence and enhanced convection in the northern and southern parts of eastern China, leading to increasing of precipitation in this area.
Keywords:East Asian circulation in summer  transient eddy activity  middle latitudes  precipitation in summer  WRF model
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