Holocene warmth explains the Little Ice Age advance of Sermeq Kujalleq-Reference-Cited by-同舟云学术

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Holocene warmth explains the Little Ice Age advance of Sermeq Kujalleq

Published:2024-10 Issue: Volume:341 Page:108840
ISSN:0277-3791
Container-title:Quaternary Science Reviews
language:en
Short-container-title:Quaternary Science Reviews

Author:

Kajanto Karita,Andresen Camilla^ORCID,Seroussi Helene^ORCID,Rieckh Therese^ORCID,Briner Jason P.,de Fleurian Basile,Born Andreas,Nisancioglu Kerim

Funder

Norwegian Research Centre for Hydropower Technology

Kansas NSF EPSCoR

Health Research Fund of Central Denmark Region

Erciyes Üniversitesi

European Research Council

Council for Chemical Research

Villum Fonden

Seventh Framework Programme

Norges Forskningsråd

Nordisk Ministerråd

Publisher

Elsevier BV

Reference59 articles.

1. Ice-sheet configuration in the CMIP5/PMIP3 Last Glacial Maximum experiments;Abe-Ouchi;Geosci. Model Dev.,2015

2. Petermann ice shelf may not recover after a future breakup;Åkesson;Nature Commun.,2022

3. Sediment discharge from Greenland’s marine-terminating glaciers is linked with surface melt;Andresen;Nature Commun.,2024

4. Interaction between subsurface ocean waters and calving of the Jakobshavn Isbræ during the late Holocene;Andresen;Holocene,2010

5. Interaction between subsurface ocean waters and calving of the Jakobshavn Isbræ during the late Holocene;Andresen;Holocene,2011

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