Warming and drying over the central Himalaya caused by an | ResearchBunny

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Abstract

Recent warming and drying trends in the central Himalayas are impacting downstream water resources. This study uses a 36-year high-resolution dynamical downscaling to investigate the role of the diurnal cycle in these trends. Enhanced daytime upslope winds prevent drying, while amplified nighttime downslope winds cause significant nocturnal drying at high elevations. This amplification of the diurnal mountain circulation is crucial for predicting future hydroclimate in this complex terrain.

Publisher

npj Climate and Atmospheric Science

Published On

Jan 16, 2020

Authors

Jesse Norris, Leila M. V. Carvalho, Charles Jones, Forest Cannon

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