中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Long-wave trough and ridge controlling of the water vapor transport to the Tibet Plateau by the tropical cyclones in the Bay of Bengal in May

文献类型:期刊论文

作者Zhou, Xiaoli1,4; Xie, Qiang1; Yang, Lei2,3
刊名CLIMATE DYNAMICS
出版日期2021-08-25
页码18
关键词Tropical cyclones Tibetan Plateau Water vapor transport Bay of Bengal Moisture budget Momentum equation
ISSN号0930-7575
DOI10.1007/s00382-021-05930-6
英文摘要This study investigates the water vapor transport to the Tibetan Plateau (TP) induced by Bay of Bengal (BOB) tropical cyclones (TCs) in May during 1979-2019. The water vapor around the BOB TCs can be transported to the south of the TP by the southerlies at the upper troposphere east of the TC center. Whether the water vapor can cross the southern boundary of the Tibetan Plateau (SBTP) may rely on the different configurations of BOB TCs and long-wave trough and ridge. We found that the water vapor may (may not) cross SBTP if the TC's wind field converges with the westerlies in front of the trough (ridge). The physical mechanism is explored according to the momentum equation. When the TC moves northward around the SBTP, its wind field could interact with the trough (Type-T TC) and ridge (Type-R TC) in the westerlies. In the area close to the trough line (ridge line), the meridional acceleration is positive (negative), hence meridional component of velocity increases (decreases). Therefore, it is more favorable for the water vapor transported northward if the Type-T TC's wind field enters the westerlies from the area close to the trough line than the ridge line. The simulation of the BOB TC cases using WRF model confirms the importance of the relative position between the Type-T TC and the SBTP to the water vapor transport over the SBTP. For the Type-T TC, the meridional moisture budget over the SBTP is positively correlated with the TC intensity and negatively correlated with the meridional distance between the TC center and the SBTP. However, for the Type-R TC, the meridional moisture budget is not related to the TC intensity and the meridional distance. The configuration of TC and long-wave trough or ridge may be predictable through the intraseasonal oscillation activity in the eastern BOB and the southern Arabian Sea.
WOS关键词WESTERN NORTH PACIFIC ; LARGE-SCALE CIRCULATION ; ASIAN WINTER MONSOON ; SUMMER PRECIPITATION ; MOISTURE ; CLIMATOLOGY ; MODULATION ; RAINFALL ; CHINA ; HEAT
资助项目National key RD program[2017YFC1405100] ; Second Tibetan Plateau Scientific Expedition and Research (STEP) program[2019QZKK0102] ; Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou)[GML2019ZD0306] ; Strategic Priority Research Program of Chinese Academy of Sciences[XDA20060500] ; National natural Science Foundation of China[41676017] ; National natural Science Foundation of China[41906181] ; Independent Research Project Program of State Key Laboratory of Tropical Oceanography[LTOZZ2005] ; Independent Research Project Program of State Key Laboratory of Tropical Oceanography[LTOZZ2101] ; Guangzhou City Project[202102080482]
WOS研究方向Meteorology & Atmospheric Sciences
语种英语
WOS记录号WOS:000688394600003
出版者SPRINGER
资助机构National key RD program ; Second Tibetan Plateau Scientific Expedition and Research (STEP) program ; Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) ; Strategic Priority Research Program of Chinese Academy of Sciences ; National natural Science Foundation of China ; Independent Research Project Program of State Key Laboratory of Tropical Oceanography ; Guangzhou City Project
源URL[http://ir.idsse.ac.cn/handle/183446/8886]  
专题深海科学研究部_海洋环流观测与数值模拟研究室
通讯作者Xie, Qiang; Yang, Lei
作者单位1.Chinese Acad Sci, Inst Deep Sea Sci & Engn, Sanya, Peoples R China
2.Chinese Acad Sci, South China Sea Inst Oceanol, State Key Lab Trop Oceanog, Guangzhou, Peoples R China
3.Southern Marine Sci & Engn Guangdong Lab, Guangzhou, Peoples R China
4.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
推荐引用方式
GB/T 7714
Zhou, Xiaoli,Xie, Qiang,Yang, Lei. Long-wave trough and ridge controlling of the water vapor transport to the Tibet Plateau by the tropical cyclones in the Bay of Bengal in May[J]. CLIMATE DYNAMICS,2021:18.
APA Zhou, Xiaoli,Xie, Qiang,&Yang, Lei.(2021).Long-wave trough and ridge controlling of the water vapor transport to the Tibet Plateau by the tropical cyclones in the Bay of Bengal in May.CLIMATE DYNAMICS,18.
MLA Zhou, Xiaoli,et al."Long-wave trough and ridge controlling of the water vapor transport to the Tibet Plateau by the tropical cyclones in the Bay of Bengal in May".CLIMATE DYNAMICS (2021):18.

入库方式: OAI收割

来源:深海科学与工程研究所

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