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DOI10.1038/ncomms10925
Summer rainfall over the southwestern Tibetan Plateau controlled by deep convection over the Indian subcontinent
Dong, Wenhao; Lin, Yanluan; Wright, Jonathon S.; Ming, Yi; Xie, Yuanyu; Wang, Bin; Luo, Yong; Huang, Wenyu; Huang, Jianbin; Wang, Lei; Tian, Lide; Peng, Yiran; Xu, Fanghua
通讯作者Lin, YL (通讯作者)
发表日期2016
ISSN2041-1723
卷号7
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.
关键词GLOBAL PRECIPITATIONMONSOONCLIMATEASIAVARIABILITYWATERIMPACTSORIGINCLOUDS
语种英语
WOS研究方向Science & Technology - Other Topics
WOS类目Multidisciplinary Sciences
WOS记录号WOS:000371720600001
来源期刊NATURE COMMUNICATIONS
来源机构中国科学院青藏高原研究所
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/258781
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GB/T 7714
Dong, Wenhao,Lin, Yanluan,Wright, Jonathon S.,et al. Summer rainfall over the southwestern Tibetan Plateau controlled by deep convection over the Indian subcontinent[J]. 中国科学院青藏高原研究所,2016,7.
APA Dong, Wenhao.,Lin, Yanluan.,Wright, Jonathon S..,Ming, Yi.,Xie, Yuanyu.,...&Xu, Fanghua.(2016).Summer rainfall over the southwestern Tibetan Plateau controlled by deep convection over the Indian subcontinent.NATURE COMMUNICATIONS,7.
MLA Dong, Wenhao,et al."Summer rainfall over the southwestern Tibetan Plateau controlled by deep convection over the Indian subcontinent".NATURE COMMUNICATIONS 7(2016).
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