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1000 Titel
  • Subglacial valleys preserved in the highlands of south and east Greenland record restricted ice extent during past warmer climates
1000 Autor/in
  1. Paxman, Guy J. G. |
  2. Jamieson, Stewart S. R. |
  3. Dolan, Aisling M. |
  4. Bentley, Michael J. |
1000 Verlag
  • Copernicus Publications
1000 Erscheinungsjahr 2024
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2024-03-28
1000 Erschienen in
1000 Quellenangabe
  • 18(3):1467-1493
1000 Copyrightjahr
  • 2024
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.5194/tc-18-1467-2024 |
1000 Publikationsstatus
1000 Begutachtungsstatus
1000 Sprache der Publikation
1000 Abstract/Summary
  • <jats:p>Abstract. The Greenland Ice Sheet is a key contributor to contemporary global sea level rise, but its long-term history and response to episodes of warming in Earth's geological past remain uncertain. The terrain covered by the ice sheet comprises ∼ 79 % of Greenland and ∼ 1.1 % of the Earth's land surface and contains geomorphological records that may provide valuable insights into past ice-sheet behaviour. Here we use ice surface morphology and radio-echo sounding data to identify ice-covered valleys within the highlands of southern and eastern Greenland and use numerical ice-sheet modelling to constrain the climatological and glaciological conditions responsible for valley incision. Our mapping reveals intricate subglacial valley networks with morphologies that are indicative of substantial glacial modification of an inherited fluvial landscape, yet many of these valleys are presently situated beneath cold-based, slow-moving (i.e. non-erosive) ice. We use the morphology of the valleys and our simple ice-sheet model experiments to infer that incision likely occurred beneath erosive mountain valley glaciers during one or more phases of Greenland's glacial history when ice was restricted to the southern and eastern highlands and when Greenland's contribution to barystatic sea level was up to +7 m relative to today. We infer that this valley incision primarily occurred prior to the growth of a continental-scale ice sheet, most likely during the late Miocene (ca. 7–5 Ma) and/or late Pliocene (ca. 3.6–2.6 Ma). Our findings therefore provide new data-based constraints on early Greenland Ice Sheet extent and dynamics that can serve as valuable boundary conditions in models of regional and global palaeoclimate during past warm periods that are important analogues for climate change in the 21st century and beyond. </jats:p>
1000 Liste der Beteiligten
  1. https://frl.publisso.de/adhoc/uri/UGF4bWFuLCBHdXnCoEouwqBHLg==|https://frl.publisso.de/adhoc/uri/SmFtaWVzb24sIFN0ZXdhcnTCoFMuwqBSLg==|https://frl.publisso.de/adhoc/uri/RG9sYW4sIEFpc2xpbmfCoE0u|https://frl.publisso.de/adhoc/uri/QmVudGxleSwgTWljaGFlbMKgSi4=
1000 Hinweis
  • DeepGreen-ID: fe57bf3da0d94d91be08078adc5ea499 ; 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. Leverhulme Trust |
  2. H2020 European Research Council |
1000 Fördernummer
  1. -
  2. -
1000 Förderprogramm
  1. -
  2. -
1000 Dateien
1000 Förderung
  1. 1000 joinedFunding-child
    1000 Förderer Leverhulme Trust |
    1000 Förderprogramm -
    1000 Fördernummer -
  2. 1000 joinedFunding-child
    1000 Förderer H2020 European Research Council |
    1000 Förderprogramm -
    1000 Fördernummer -
1000 Objektart article
1000 Beschrieben durch
1000 @id frl:6481965.rdf
1000 Erstellt am 2024-05-24T01:21:33.221+0200
1000 Erstellt von 322
1000 beschreibt frl:6481965
1000 Zuletzt bearbeitet Mon May 27 12:07:41 CEST 2024
1000 Objekt bearb. Mon May 27 12:07:41 CEST 2024
1000 Vgl. frl:6481965
1000 Oai Id
  1. oai:frl.publisso.de:frl:6481965 |
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