Earth Sciences

Warming and drying over the central Himalaya caused by an amplification of local mountain circulation

J. Norris, L. M. V. Carvalho, et al.

Dive into the intriguing dynamics of the central Himalayas where recent warming and drying trends are reshaping water resources. This exciting research conducted by Jesse Norris, Leila M. V. Carvalho, Charles Jones, and Forest Cannon reveals how the diurnal cycle significantly influences these climatic changes, offering crucial insights for future hydroclimate predictions.

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Playback language: English

Index

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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