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Climate Change and Permafrost

Bibliographic Data

ID23675313
AuthorsNadine Salzmann (0000-0001-5876-7624, University of Fribourg), Isabelle Gärtner‐roer (0000-0003-3621-488X, University of Zurich)
Year2017
Pages1-13
Publication date2017-03-06
Open AccessYes
TypeCHAPTER
VenueInternational Encyclopedia of Geography (SOURCE_BOOK)
PublisherWiley (PUBLISHER • GB)
DOI10.1002/9781118786352.wbieg1124
OpenAlexW2594513733
ISBN9781118786352
LanguageEN
References cited8

Permafrost is a thermal phenomenon of the lithosphere and applies to ground that remains at or below 0°C for at least two consecutive years. Permafrost is coupled to atmospheric conditions and as such is sensitive to climatic changes. Thawing of permafrost can lead to destabilization of steep slopes or infrastructure, and a major concern is the release of radiative active forcing gases such as methane stored in permafrost ground. Projections of permafrost changes suggest further degradation in both high altitudes and high latitudes.

Atmospheric sciences · Climate change · Climatology · Earth science · Forcing (mathematics) · Geodesy · Geography · Global warming · Latitude · Lithosphere · Methane · Permafrost · Physical geography · Radiative forcing · Tectonics · Climate change and permafrost · Cryospheric studies and observations · Ecology · Environmental Science · Geology · Geology and Paleoclimatology Research · Oceanography

Highly citedNo

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