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学科主题: 地理学::自然地理学
题名: Summer rainfall over the southwestern Tibetan Plateau controlled by deep convection over the Indian subcontinent
作者: Dong, WH (Dong, Wenhao)1, 2; Lin, YL (Lin, Yanluan)1, 2; Wright, JS (Wright, Jonathon S.)1, 2; Ming, Y (Ming, Yi)3; Xie, YY (Xie, Yuanyu)1, 2; Wang, B (Wang, Bin)1, 2, 4; Luo, Y (Luo, Yong)1, 2; Huang, WY (Huang, Wenyu)1, 2; Huang, JB (Huang, Jianbin)1, 2; Wang, L (Wang, Lei)5, 6; Tian, LD (Tian, Lide)5, 6; Peng, YR (Peng, Yiran)1, 2; Xu, FH (Xu, Fanghua)1, 2
通讯作者: Lin, YL
刊名: NATURE COMMUNICATIONS
发表日期: 2016
DOI: 10.1038/ncomms10925
卷: 7, 期:0, 页:10925
收录类别: SCI
合作性质: 国际
文章类型: Article
英文摘要: Despite the importance of precipitation and moisture transport over the Tibetan Plateau for glacier mass balance, river runoff and local ecology, changes in these quantities remain highly uncertain and poorly understood. Here we use observational data and model simulations to explore the close relationship between summer rainfall variability over the southwestern Tibetan Plateau (SWTP) and that over central-eastern India (CEI), which exists despite the separation of these two regions by the Himalayas. We show that this relationship is maintained primarily by 'up-and-over' moisture transport, in which hydrometeors and moisture are lifted by convective storms over CEI and the Himalayan foothills and then swept over the SWTP by the mid-tropospheric circulation, rather than by upslope flow over the Himalayas. Sensitivity simulations confirm the importance of up-and-over transport at event scales, and an objective storm classification indicates that this pathway accounts for approximately half of total summer rainfall over the SWTP.
语种: 英语
WOS记录号: WOS:000371720600001
Citation statistics:
内容类型: 期刊论文
URI标识: http://ir.itpcas.ac.cn/handle/131C11/7753
Appears in Collections:图书馆_期刊论文

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作者单位: 1.Tsinghua Univ, Minist Educ, Key Lab Earth Syst Modeling, Ctr Earth Syst Sci, Room S813,MengMinwei Sci Bldg,Qinghuayuan 1, Beijing 100084, Peoples R China
2.Tsinghua Univ, Joint Ctr Global Change Studies, Room S813,MengMinwei Sci Bldg,Qinghuayuan 1, Beijing 100084, Peoples R China
3.NOAA, Geophys Fluid Dynam Lab, Princeton, NJ 08540 USA
4.Chinese Acad Sci, State Key Lab Numer Modeling Atmospher Sci & Geop, Inst Atmospher Phys, Beijing 100029, Peoples R China
5.Chinese Acad Sci, Key Lab Tibetan Environm Changes & Land Surface P, Inst Tibetan Plateau Res, Beijing 100101, Peoples R China
6.CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China

Recommended Citation:
Dong, WH ,Lin, YL ,Wright, JS ,et al. Summer rainfall over the southwestern Tibetan Plateau controlled by deep convection over the Indian subcontinent[J]. NATURE COMMUNICATIONS,2016,7(0):10925.
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文件名: V.7 10925 2016.pdf
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