How Were the Eastward-Moving Heavy Rainfall Events from the Tibetan Plateau to the Lower Reaches of the Yangtze River Enhanced?Source: Journal of Climate:;2021:;volume( 034 ):;issue: 002::page 607Author:Zhao, Yang;Chen, Deliang;Deng, Yi;Son, Seok-Woo;Wang, Xiang;Di, Di;Pan, Mengting;Ma, Xiaodan
DOI: 10.1175/JCLI-D-20-0226.1Publisher: American Meteorological Society
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| contributor author | Zhao, Yang;Chen, Deliang;Deng, Yi;Son, Seok-Woo;Wang, Xiang;Di, Di;Pan, Mengting;Ma, Xiaodan | |
| date accessioned | 2022-03-26T18:44:28Z | |
| date available | 2022-03-26T18:44:28Z | |
| date copyright | 01 Jan. 2021 | |
| date issued | 2021 | |
| identifier other | JCLI-D-20-0226.1.pdf | |
| identifier uri | http://yetl.yabesh.ir/yetl1/handle/yetl/4279161 | |
| publisher | American Meteorological Society | |
| title | How Were the Eastward-Moving Heavy Rainfall Events from the Tibetan Plateau to the Lower Reaches of the Yangtze River Enhanced? | |
| type | Journal Paper | |
| journal volume | 34 | |
| journal issue | 2 | |
| journal title | Journal of Climate | |
| identifier doi | 10.1175/JCLI-D-20-0226.1 | |
| journal fristpage | 607 | |
| journal lastpage | 620 | |
| tree | Journal of Climate:;2021:;volume( 034 ):;issue: 002 | |
| contenttype | Fulltext |