详细信息
Response of Ozone to a Gravity Wave Process in the UTLS Region Over the Tibetan Plateau ( SCI-EXPANDED收录 EI收录) 被引量:9
文献类型:期刊文献
英文题名:Response of Ozone to a Gravity Wave Process in the UTLS Region Over the Tibetan Plateau
作者:Chang, Shujie[1,2];Sheng, Zheng[1];Zhu, Yanwei[3];Shi, Weilai[1];Luo, Zhixian[1]
机构:[1]Natl Univ Def Technol, Coll Meteorol & Oceanol, Changsha, Peoples R China;[2]Guangdong Ocean Univ, Coll Ocean & Meteorol, Zhanjiang, Peoples R China;[3]Natl Univ Def Technol, Coll Aerosp Sci & Engn, Changsha, Peoples R China
年份:2020
卷号:8
外文期刊名:FRONTIERS IN EARTH SCIENCE
收录:SCI-EXPANDED(收录号:WOS:000558860400001)、、EI(收录号:20212810638249)、WOS
基金:This work was supported by the National Natural Science Foundation of China (Grant Nos. 41875045 and 41775039), the National Key R&D Program of China (Grant No. 2018YFA0605604), and the project of Enhancing School with Innovation of Guangdong Ocean University (Grant No. 4230419053).
语种:英文
外文关键词:gravity wave; Tibetan Plateau; STE; ozone; WRF model
外文摘要:In this paper, ERA5 reanalysis data from the European Center for Medium-Range Weather Forecasts and the Weather Research and Forecasting (WRF) mesoscale model are used to compare and simulate a topographic gravity wave event that occurred over the Tibetan Plateau between 18:00 on 3 May 2014 and 00:00 on 4 May 2014. The stratosphere-troposphere exchange (STE) process and its detailed characteristics during the gravity wave event are presented. The response of the upper troposphere and lower stratosphere (UTLS) ozone to the gravity wave is discovered from the perspective of the gravity wave dynamic process. The results show that the gravity wave structure between 90 degrees E and 100 degrees E had a westward tilt with height. From 19:00 to 21:00 the gravity waves decayed and from 22:00 to 23:00 their shape gradually blurred. Meanwhile, there was a response of the ozone mixing ratio in the UTLS over the Tibetan Plateau to the gravity waves breaking. After 21:00, this wave process caused the STE, as air from the stratosphere with a greater ozone concentration was injected into the upper troposphere, leading to rapidly increased ozone concentration there.
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