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作 者:李琳琳 南素兰[2] 赵平[2] 巩远发[1] LI Linlin;NAN Sulan;ZHAO Ping;GONG Yuanfa(College of Atmospheric Sciences,Chengdu University of Information Technology,Chengdu 610225,China;Chinese Academy of Meteorological Sciences,Beijing 100081,China)
机构地区:[1]成都信息工程大学大气科学学院,四川成都610225 [2]中国气象科学研究院,北京100081
出 处:《成都信息工程大学学报》2021年第2期185-189,共5页Journal of Chengdu University of Information Technology
基 金:中科院先导专项资助项目(XDA20100300);国家自然科学基金资助项目(41775084);气科院基本科研业务资助项目(2019Z008)。
摘 要:目前南亚高压与全球大气环流和气候的联系主要集中于北半球,很少研究与南半球气候系统之间的联系。因此主要应用相关、合成方法,利用1979-2014年ERA-Interim逐月再分析资料,选取南亚高压中心区域平均的位势高度来指示南亚高压强度,探讨对流层中高层欧亚大陆与南半球印度洋中、低纬地区大气环流特征及其成因。结果表明,在年际尺度上,该区域在高度场和温度场上呈现以热带为轴的对称结构,这与南亚高压密切相关,并且与异常的纬向-垂直环流密切相关。该环流圈减弱了北半球欧亚大陆区域Hadley环流的下沉支,加强了南半球印度洋区域Hadley环流的下沉支。因此,该环流圈可能是南北半球相互作用的一个重要"通道",可以在欧亚大陆与南印度洋地区热量、能量等传输过程中起着重要作用。At present,the connection between the South Asia High(SAH)and global atmospheric circulation and climate is mainly concentrated in the Northern hemisphere.However,there are few studies on the relationship between the SAH and the southern hemisphere climate system.Therefore,relevant and synthesis methods are mainly used.Then employing monthly reanalysis data from 1979-2014 ERA-Interim,and selecting average geopotential height of SAH center area to represent the high pressure intensity of South Asia High,meanwhile,discussing the atmospheric circulation characteristics in Eurasia located in the middle and upper troposphere and in the middle and low latitude area in the south hemisphere.The results show that,on the interannual scale,this area shows a symmetrical structure with tropics as axis,which is closely related to the South Asian High and anomalous zonal vertical circulation in the region.The circulation weakens the sinking branch of the Hadley circulation in the Eurasian region of the northern hemisphere and strengthens the sinking branch of the Hadley circulation in the Indian Ocean region of the southern hemisphere.This circulation may be an important"channel"for the interaction between the northern and southern hemispheres,and plays an important role in the heat and energy transfer process between Eurasia and southern Indian ocean.
关 键 词:气象学 青藏高原气候学 南亚高压 青藏高原 对称结构 经向环流 欧亚大陆-南印度洋中低纬度
分 类 号:P466[天文地球—大气科学及气象学]
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