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Increasing precipitation due to climate change could partially offset the impact of warming on glacier loss in the monsoon-influenced Himalaya until 2100 CE

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Bibliographic Details
Published in:The Cryosphere (TC)
Format: Online Article RSS Article
Published: 2026
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container_title The Cryosphere (TC)
description
discipline_display Meteorology
discipline_facet Meteorology
format Online Article
RSS Article
genre Journal Article
id rss_article:62433
institution FRELIP
journal_source_facet The Cryosphere (TC)
publishDate 2026
publishDateSort 2026
record_format rss_article
spellingShingle Increasing precipitation due to climate change could partially offset the impact of warming on glacier loss in the monsoon-influenced Himalaya until 2100 CE
Meteorology
General
Meteorology
sub_discipline_display General
sub_discipline_facet General
subject_display Meteorology
General
Meteorology
Meteorology
General
Meteorology
subject_facet Meteorology
General
Meteorology
title Increasing precipitation due to climate change could partially offset the impact of warming on glacier loss in the monsoon-influenced Himalaya until 2100 CE
title_auth Increasing precipitation due to climate change could partially offset the impact of warming on glacier loss in the monsoon-influenced Himalaya until 2100 CE
title_full Increasing precipitation due to climate change could partially offset the impact of warming on glacier loss in the monsoon-influenced Himalaya until 2100 CE
title_fullStr Increasing precipitation due to climate change could partially offset the impact of warming on glacier loss in the monsoon-influenced Himalaya until 2100 CE
title_full_unstemmed Increasing precipitation due to climate change could partially offset the impact of warming on glacier loss in the monsoon-influenced Himalaya until 2100 CE
title_short Increasing precipitation due to climate change could partially offset the impact of warming on glacier loss in the monsoon-influenced Himalaya until 2100 CE
title_sort increasing precipitation due to climate change could partially offset the impact of warming on glacier loss in the monsoon-influenced himalaya until 2100 ce
topic Meteorology
General
Meteorology
url https://doi.org/10.5194/tc-20-3151-2026