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1000 Titel
  • Modelling present and future rock wall permafrost distribution in the Sisimiut mountain area, West Greenland
1000 Autor/in
  1. Marcer, Marco |
  2. Duvillard, Pierre-Allain |
  3. Tomaškovičová, Soňa |
  4. Nielsen, Steffen Ringsø |
  5. Revil, André |
  6. Ingeman-Nielsen, Thomas |
1000 Verlag Copernicus Publications
1000 Erscheinungsjahr 2024
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2024-04-15
1000 Erschienen in
1000 Quellenangabe
  • 18(4):1753-1771
1000 Copyrightjahr
  • 2024
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.5194/tc-18-1753-2024 |
1000 Publikationsstatus
1000 Begutachtungsstatus
1000 Sprache der Publikation
1000 Abstract/Summary
  • <jats:p>Abstract. Degrading rock wall permafrost was found responsible for the increase in rockfall and landslide activity in several cold mountain regions across the globe. In Greenland, rock wall permafrost has so far received little attention from the scientific community, despite mountains being a predominant feature on the ice-free coastline and landslide activity being significant. In this study, we aim to make a first step towards a better understanding of rock wall permafrost in Greenland by modelling rock wall temperatures in the mountain area around the town of Sisimiut, which is 68° N on the west coast of Greenland. We first acquire rock surface temperature (RST) data for the period September 2020–September 2022 to model rock surface temperatures from weather forcing. The model is then applied to weather data from 1870 to 2022, generating rock surface temperatures to force transient heat transfer simulations over the same period. By extrapolating this method at the landscape scale, we obtain permafrost distribution maps and ad hoc simulations for complex topographies. Our model results are compared to temperature data from two lowland boreholes (100 m depth) and geophysical data describing frozen and unfrozen conditions across a mid-elevation mountain ridge. Finally, we use regional carbon pathway scenarios 2.6 and 8.5 to evaluate future evolution of rock wall temperatures until the end of the 21st century. Our data and simulation describe discontinuous permafrost distribution in rock walls up to roughly 400 m a.s.l. Future scenarios suggest a decline of deep frozen bodies up to 800 m a.s.l., i.e. the highest summits in the area. In summary, this study depicts a picture of warm permafrost in this area, highlighting its sensitivity to ongoing climate change. </jats:p>
1000 Fächerklassifikation (DDC)
1000 Liste der Beteiligten
  1. https://orcid.org/0000-0002-2749-8051|https://frl.publisso.de/adhoc/uri/RHV2aWxsYXJkLCBQaWVycmUtQWxsYWlu|https://orcid.org/0000-0002-2461-8863|https://frl.publisso.de/adhoc/uri/TmllbHNlbiwgU3RlZmZlbiBSaW5nc8O4|https://frl.publisso.de/adhoc/uri/UmV2aWwsIEFuZHLDqQ==|https://orcid.org/0000-0002-0776-4869
1000 Hinweis
  • DeepGreen-ID: d8147ff056e04967a101b52c57799a50 ; metadata provieded by: DeepGreen (https://www.oa-deepgreen.de/api/v1/), LIVIVO search scope life sciences (http://z3950.zbmed.de:6210/livivo), Crossref Unified Resource API (https://api.crossref.org/swagger-ui/index.html), to.science.api (https://frl.publisso.de/), ZDB JSON-API (beta) (https://zeitschriftendatenbank.de/api/), lobid - Dateninfrastruktur für Bibliotheken (https://lobid.org/resources/search)
1000 Label
1000 Förderer
  1. Horizon 2020 |
  2. Nunatsinni Ilisimatusarnermik Siunnersuisoqatigiit |
1000 Fördernummer
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1000 Förderprogramm
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1000 Dateien
1000 Förderung
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    1000 Förderer Horizon 2020 |
    1000 Förderprogramm -
    1000 Fördernummer -
  2. 1000 joinedFunding-child
    1000 Förderer Nunatsinni Ilisimatusarnermik Siunnersuisoqatigiit |
    1000 Förderprogramm -
    1000 Fördernummer -
1000 Objektart article
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1000 @id frl:6481197.rdf
1000 Erstellt am 2024-05-23T19:41:44.064+0200
1000 Erstellt von 322
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1000 Zuletzt bearbeitet 2025-08-15T19:36:40.336+0200
1000 Objekt bearb. Fri Aug 15 19:36:40 CEST 2025
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