Western Greenland ice sheet retreat history reveals elevated precipitation during the Holocene thermal maximum

We investigate changing precipitation patterns in the Kangerlussuaq region of western central Greenland during the Holocene thermal maximum (HTM), using a new chronology of ice sheet terminus position through the Holocene and a novel inverse modeling approach based on the unscented transform (UT). T...

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Bibliographic Details
Published in:The Cryosphere
Main Authors: Downs, Jacob, Johnson, Jesse, Briner, Jason, Young, Nicolás, Lesnek, Alia, Cuzzone, Josh
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2020
Subjects:
Online Access:https://doi.org/10.5194/tc-14-1121-2020
https://noa.gwlb.de/receive/cop_mods_00051069
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00050726/tc-14-1121-2020.pdf
https://tc.copernicus.org/articles/14/1121/2020/tc-14-1121-2020.pdf
Description
Summary:We investigate changing precipitation patterns in the Kangerlussuaq region of western central Greenland during the Holocene thermal maximum (HTM), using a new chronology of ice sheet terminus position through the Holocene and a novel inverse modeling approach based on the unscented transform (UT). The UT is applied to estimate changes in annual precipitation in order to reduce the misfit between modeled and observed terminus positions. We demonstrate the effectiveness of the UT for time-dependent data assimilation, highlighting its low computational cost and trivial parallel implementation. Our results indicate that Holocene warming coincided with elevated precipitation, without which modeled retreat in the Kangerlussuaq region is more rapid than suggested by observations. Less conclusive is whether high temperatures during the HTM were specifically associated with a transient increase in precipitation, as the results depend on the assumed temperature history. Our results highlight the important role that changing precipitation patterns had in controlling ice sheet extent during the Holocene.