Holocene glacial history of Svalbard: Status, perspectives and challenges

Publisher's version (útgefin grein) We synthesize the current understanding of glacier activity on Svalbard from the end of the Late Pleistocene (12,000 yrs. before present) to the end of the Little Ice Age (c. 1920 AD). Our glacier history is derived from the SVALHOLA database, the first compi...

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Bibliographic Details
Published in:Earth-Science Reviews
Main Authors: Farnsworth, Wesley, Allaart, Lis, Ingolfsson, Olafur, Alexanderson, Helena, Forwick, Matthias, Noormets, Riko, Retelle, Michael, Schomacker, Anders
Other Authors: Jarðvísindastofnun (HÍ), Institute of Earth Sciences (UI), Verkfræði- og náttúruvísindasvið (HÍ), School of Engineering and Natural Sciences (UI), Háskóli Íslands, University of Iceland
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier BV 2020
Subjects:
Online Access:https://hdl.handle.net/20.500.11815/2215
https://doi.org/10.1016/j.earscirev.2020.103249
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Summary:Publisher's version (útgefin grein) We synthesize the current understanding of glacier activity on Svalbard from the end of the Late Pleistocene (12,000 yrs. before present) to the end of the Little Ice Age (c. 1920 AD). Our glacier history is derived from the SVALHOLA database, the first compilation of Holocene geochronology for Svalbard and the surrounding waters, including over 1,800 radiocarbon, terrestrial cosmogenic nuclide and optically stimulated luminescence ages. Data have been categorized by geological setting, uniformly (re-)calibrated, quality assessed and ultimately used to constrain glacier fluctuations (deglaciation, ice free conditions, glacier re-advances and ice marginal positions). We advance existing knowledge by mapping the extent and distribution of ice-cover during the Holocene glacial maximum and the glacial minimum, as well as present retreat rates (and percentages) within Early Holocene fjord-systems. Throughout the Holocene, Svalbard glaciers have responded to a varying combination of climatic, environmental and dynamic driving factors which influence both the extent and behavior of ice margins. We discuss the complexities of glacier systems and their dynamics in response to changes in climate. This review provides a holistic state of the art of Holocene glaciers on Svalbard, suitable for orienting future works which address gaps in our current knowledge. Fianancial support has been provided by the Svalbard Environmental Protection Fund (16/35; to WRF), the Carlsberg Foundation (CF14-0756 to AS), The University Center in Svalbard (UNIS) (research grant to ÓI), and Arctic Research and Studies funded by the Ministries for Foreign Affairs of Norway and Iceland (2017-ARS-79772 to AS & WRF). We are grateful for extensive support from the UNIS Library (Berit Jakobsen and Catherine Fjeldstad). Constructive comments from and discussions with Skafti Brynjólfsson, Kelly Hogan, Anna L.C. Hughes, Sofia Kjellman, Nicolaj K. Larsen and Anne Sofie Søndergaard have improved this manuscript. ...