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10.1038/ncomms10925 http://scihub22266oqcxt.onion/10.1038/ncomms10925 C4786685!4786685!26948491     free     free     free Deprecated: Implicit conversion from float 233.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534 Deprecated: Implicit conversion from float 233.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534 Deprecated: Implicit conversion from float 233.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534 Deprecated: Implicit conversion from float 233.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534 Deprecated: Implicit conversion from float 233.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534 Deprecated: Implicit conversion from float 233.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534 Deprecated: Implicit conversion from float 233.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534 Deprecated: Implicit conversion from float 267.2 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534       Nat+Commun 2016 ; 7 (ä): ä Nephropedia Template TP {{tp|p=26948491|t=2016. Summer rainfall over the southwestern Tibetan Plateau controlled by deep convection over the Indian subcontinent |pdf=|usr=}}{{26948491}} gab.com Text Summer rainfall over the southwestern Tibetan Plateau controlled by deep convection over the Indian subcontinent JO: Nat Commun http://www.kidney.de/pget.php?&tw=1&pmid=26948491 #FOAvip 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. Twit Text FOAVip Summer rainfall over the southwestern Tibetan Plateau controlled by deep convection over the Indian subcontinent ????Nat Commun http://www.kidney.de/pget.php?&tw=1&pmid=26948491 #FOAvip Twit Text # Free Paper on # # # # # LINK http://www.kidney.de/pget.php?&tw=1&pmid=26948491 #FOAvip English Wikipedia <ref>{{Cite pmid|26948491}}</ref> Summer rainfall over the southwestern Tibetan Plateau controlled by deep convection over the Indian subcontinent #MMPMID26948491 Dong W; Lin Y; Wright JS; Ming Y; Xie Y; Wang B; Luo Y; Huang W; Huang J; Wang L; Tian L; Peng Y; Xu F Nat Commun 2016[]; 7 (ä): ä PMID26948491show ga 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. äSummer rainfall over the southwestern Tibetan Plateau controlled by de(epmc).pdf DeepDyve Pubget Overpricing