Increasing precipitation due to climate change could partially offset the impact of warming on glacier loss in the monsoon-influenced Himalaya until 2100 CE
Anya M. Schlich-Davies,Ann V. Rowan,Andrew N. Ross,Duncan J. Quincey,and Vivi K. Pedersen
Anya M. Schlich-Davies
Priestley International Centre for Climate, School of Earth and Environment, University of Leeds, Leeds, UK
Department of Geoscience, Aarhus University, Aarhus C, Denmark
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Views and downloads (calculated since 04 Apr 2025)
Cumulative views and downloads
(calculated since 04 Apr 2025)
Total article views: 5,391 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
5,376
0
15
5,391
0
0
HTML: 5,376
PDF: 0
XML: 15
Total: 5,391
BibTeX: 0
EndNote: 0
Views and downloads (calculated since 04 Apr 2025)
Cumulative views and downloads
(calculated since 04 Apr 2025)
Viewed (geographical distribution)
Since the preprint corresponding to this journal article was posted outside of Copernicus Publications, the preprint-related metrics are limited to HTML views.
Total article views: 5,391 (including HTML, PDF, and XML)
Thereof 5,359 with geography defined
and 32 with unknown origin.
Total article views: 5,391 (including HTML, PDF, and XML)
Thereof 5,359 with geography defined
and 32 with unknown origin.
Glaciers in the Himalaya are shrinking in response to climate change. We use a glacier model to explore how future changes in precipitation distribution will drive the evolution of Khumbu Glacier in Nepal until 2100 CE. We find that, when compared to the impacts of climate warming alone, the combined effect of warming and the resulting increase in precipitation (rain and snowfall) could offset up to half of the glacier loss expected by the end of this Century.
Glaciers in the Himalaya are shrinking in response to climate change. We use a glacier model to...