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夏季青藏高原附近云顶分布和对流层顶高度的关系

SHI Chun-Hua CHANG Shu-Jie GUO Dong XU Jian-Jun ZHANG Chen-Xin

大气和海洋科学快报(英文版)2018,Vol.11Issue(2):173-179,7.
大气和海洋科学快报(英文版)2018,Vol.11Issue(2):173-179,7.

夏季青藏高原附近云顶分布和对流层顶高度的关系

Exploring the relationship between the cloud-top and tropopause height in boreal summer over the Tibetan Plateau and its adjacent region

SHI Chun-Hua 1CHANG Shu-Jie 1GUO Dong 1XU Jian-Jun 1ZHANG Chen-Xin1

作者信息

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摘要

Abstract

The distribution characteristics of cloud-top and tropopause height in the tropics and subtropics in boreal summer are analyzed based on CALIPSO data for the period 2008-2012.The maximum values of cloud-top vertical cumulative frequency above the tropopause (CTAT) are concentrated in three tropical regions:the Asian summer monsoon region,Central America,and western Africa.The contributions to the area-weighted CTAT frequency in the three regions from the Northern Hemisphere are 49.0%,13.5%,and 12.4%,respectively.Moreover,the contribution of troposphere-to-stratosphere transport (TST) in the Asian monsoon region to global TST can be far greater than 50%,according to analysis of the continuous equation,velocity potential,and divergent wind from ERA-Interim data.Furthermore,the Asian summer monsoon circulation system controls the distribution of the cloud top.On the south side of the Tibetan Plateau,the maximum frequency of the cloud top,more than 10% per 500 m vertically,is most likely to appear in the core of the high-level easterlyjet near the tropopause height (16.5 km).Over the Tibetan Plateau,the maximum frequency of the cloud top,greater than 3% per 500 m vertically,is suppressed below 11 km,far away from the thermodynamic tropopause height but close to the dynamic tropopause height of 2 PVU (potential vorticity units).

关键词

云顶/对流层顶/对流层向平流层输送/亚洲夏季风环流/青藏高原

Key words

Cloud top/tropopause/troposphere-to-stratosphere transport/Asian summer monsoon circulation/Tibetan Plateau

引用本文复制引用

SHI Chun-Hua,CHANG Shu-Jie,GUO Dong,XU Jian-Jun,ZHANG Chen-Xin..夏季青藏高原附近云顶分布和对流层顶高度的关系[J].大气和海洋科学快报(英文版),2018,11(2):173-179,7.

基金项目

This work was jointly supported by National Key Research and Development Program of China [grant number 2017YFC1501802] ()

the National Natural Science Foundation of China [grant number 41375047],[grant number 91537213],and [grant number 41675039]. ()

大气和海洋科学快报(英文版)

OACSCD

1674-2834

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