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![]() ![]() |
刊名 | CLIMATE DYNAMICS
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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 |
DOI | 10.1007/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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