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Cited by 2,937

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Elevation-dependent warming in mountain regions of the world

Open access
Mountain Research Initiative EDW Working Group·2015·Nature Climate Change

Abstract

There is growing evidence that the rate of warming is amplified with elevation, such that high-mountain environments experience more rapid changes in temperature than environments at lower elevations. Elevation-dependent warming (EDW) can accelerate the rate of change in mountain ecosystems, cryospheric systems, hydrological regimes and biodiversity. Here we review important mechanisms that contribute towards EDW: snow albedo and surface-based feedbacks; water vapour changes and latent heat release; surface water vapour and radiative flux changes; surface heat loss and temperature change; and aerosols. All lead to enhanced warming with elevation (or at a critical elevation), and it is believed that combinations of these mechanisms may account for contrasting regional patterns of EDW. We discuss future needs to increase knowledge of mountain temperature trends and their controlling mechanisms through improved observations, satellite-based remote sensing and model simulations.

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Metadata

Authors
Mountain Research Initiative EDW Working Group
Venue
Nature Climate Change
Published
2015-04-23
Volume
5
Issue
5
Pages
424-430
ISSN
  • 1758-678X (ISSN-L)
  • 1758-6798
OpenAlex
W1982518595
Cited by
2,937
References
1
FWCI
112.58
Type
journal article
Language
en
Open access
green

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CoChat. (2026). Citation check: Elevation-dependent warming in mountain regions of the world. https://app.cochat.ai/papers/10.1038/nclimate2563
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Mountain Research Initiative EDW Working Group. (2015). Elevation-dependent warming in mountain regions of the world. Nature Climate Change. https://doi.org/10.1038/nclimate2563

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