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北半球西风带准周期性转换的理论分析——初步探讨北极与中纬度及副热带能量相互输送的机制
引用本文:刘春,李跃凤,宋伟,刘自牧.北半球西风带准周期性转换的理论分析——初步探讨北极与中纬度及副热带能量相互输送的机制[J].大气科学,2019,43(2):456-466.
作者姓名:刘春  李跃凤  宋伟  刘自牧
作者单位:中国气象局气象干部培训学院/世界气象组织(WMO)区域培训中心,北京100081;高原与盆地暴雨旱涝灾害四川省重点实验室,成都610072;四川省内江市气象局,四川内江641000;中国气象局气象干部培训学院/世界气象组织(WMO)区域培训中心,北京,100081;中国气象局气象干部培训学院/世界气象组织(WMO)区域培训中心,北京100081;南京信息工程大学,南京210044;四川省气象服务中心,成都,610072
基金项目:国家自然科学资金项目41675095、41730959
摘    要:本文运用准地转模式,通过等值投影方法,将等值线转换为向量场结构,探讨西风带高低指数周期性转换的机制,结果表明:(1)仅有位能转化所引起的水平涡动输送,可能产生大振幅的行星波,但不会产生西风带的断裂;(2)在波流相互作用下,平均纬向风速与基波波幅满足分岔条件时,会出现西风带断裂现象,即当满足这个分岔条件时,更有利于北极与中纬度及副热带能量的相互输送。如北极冷空气的跨纬度输送会导致东亚极端冷事件的发生;同时,也能维持西风带的高低指数循环。

关 键 词:Rossby波  西风带高低指数周期性转换  水平涡动输送  分岔  西风带断裂
收稿时间:2017/12/6 0:00:00

Theoretical Analysis of the Quasi-periodic Conversion of Westerlies in the Northern Hemisphere-Preliminary Discussion on the Mechanism for Energy Transport between the Arctic and the Mid-latitudes and the Subtropics
LIU Chun,LI Yuefeng,SONG Wei and LIU Zimu.Theoretical Analysis of the Quasi-periodic Conversion of Westerlies in the Northern Hemisphere-Preliminary Discussion on the Mechanism for Energy Transport between the Arctic and the Mid-latitudes and the Subtropics[J].Chinese Journal of Atmospheric Sciences,2019,43(2):456-466.
Authors:LIU Chun  LI Yuefeng  SONG Wei and LIU Zimu
Institution:1.China Meteorological Administration Training Center, World Meteorological Organization(WMO) Regional Training Center, Beijing 1000812.Heavy Rain and Drought-Flood Disasters in Plateau and Basin Key Laboratory of Sichuan Province, Chengdu 6100723.Neijiang Meteorological Bureau, Neijiang, Sichuan Province 6410004.Nanjing University of Information Science & Technology, Nanjing 2100445.Sichuan Meteorological Service Center, Chengdu 610072
Abstract:In this paper, a quasi-geostrophic model is used to convert contour lines into vector field structure by the equivalent projection. The results show that:(1) Horizontal vortex transmission caused by potential energy conversion may generate planetary waves with large amplitude, but it will not break the westerlies; (2) the fracture of the westerlies will occur when the average zonal wind velocity and wave amplitude meet the bifurcation condition under the wave flow interaction. Namely, it is more conducive to the mutual transmission of energy between the Arctic and the middle latitudes and the subtropics when this bifurcation condition is satisfied. For example, the translatitudinal transportation of Arctic cold air leads to the extreme cold events over East Asia. At the same time, it can maintain the high and low index cycle of the westerlies.
Keywords:Rossby wave  Quasi-periodical conversion between high and low index of westerlies  Horizontal vortex transmission  Bifurcation  Fracture of the westerlies
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