Citation

Ballesteros-Cánovas JA, Trappmann D, Madrigal-González J, Eckert N, Stoffel M. Proc. Natl. Acad. Sci. U. S. A. 2018; 115(13): 3410-3415.

Affiliation

Department F.-A. Forel for Aquatic and Environmental Sciences, University of Geneva, CH-1205 Geneva, Switzerland.

Copyright

(Copyright © 2018, National Academy of Sciences)

DOI

10.1073/pnas.1716913115

PMID

29535224

Abstract

Ongoing climate warming has been demonstrated to impact the cryosphere in the Indian Himalayas, with substantial consequences for the risk of disasters, human well-being, and terrestrial ecosystems. Here, we present evidence that the warming observed in recent decades has been accompanied by increased snow avalanche frequency in the Western Indian Himalayas. Using dendrogeomorphic techniques, we reconstruct the longest time series (150 y) of the occurrence and runout distances of snow avalanches that is currently available for the Himalayas. We apply a generalized linear autoregressive moving average model to demonstrate linkages between climate warming and the observed increase in the incidence of snow avalanches. Warming air temperatures in winter and early spring have indeed favored the wetting of snow and the formation of wet snow avalanches, which are now able to reach down to subalpine slopes, where they have high potential to cause damage. These findings contradict the intuitive notion that warming results in less snow, and thus lower avalanche activity, and have major implications for the Western Himalayan region, an area where human pressure is constantly increasing. Specifically, increasing traffic on a steadily expanding road network is calling for an immediate design of risk mitigation strategies and disaster risk policies to enhance climate change adaption in the wider study region.

Copyright © 2018 the Author(s). Published by PNAS.

Language: en

Keywords

Himalayas; climate change; cryosphere; snow avalanche; tree rings