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East Greenland Ice Sheet retreat history from Scoresby Sund and Storstrømmen Glacier during the last deglaciation

Title: East Greenland Ice Sheet retreat history from Scoresby Sund and Storstrømmen Glacier during the last deglaciation
Authors: Anderson, Jacob T. H.; Young, Nicolás E.; Balter-Kennedy, Allie; Prince, Karlee K.; Walcott-George, Caleb K.; Graham, Brandon L.; Charton, Joanna; Briner, Jason P.; Schaefer, Joerg M.
Source: eISSN: 1814-9332
Publication Year: 2025
Collection: Copernicus Publications: E-Journals
Description: The lack of geological constraints on past ice-sheet change in marine-based sectors of the Greenland Ice Sheet (GrIS) following the Last Glacial Maximum limits our ability to assess (1) the drivers of ice-sheet change, and (2) the performance of ice-sheet models that are benchmarked against the paleo-record of GrIS change. Here, we provide new in situ 10 Be surface exposure chronologies of ice-sheet margin retreat from the outer Scoresby Sund and Storstrømmen Glacier regions in eastern and northeastern Greenland, respectively. Ice retreated from Rathbone Island, east of Scoresby Sund, by ∼ 14.1 ka, recording some of the earliest documentations of terrestrial deglaciation in Greenland. The mouth of Scoresby Sund deglaciated by ∼ 13.2 ka, and retreated at an average rate of ∼ 43 m yr −1 between 13.2 and 9.7 ka. Storstrømmen Glacier retreated from the outer coast to within ∼ 3 km of the modern ice margin between ∼ 12.7 and 8.6 ka at an average rate of ∼ 28 m yr −1 . Retreat then slowed or reached a stillstand as ice retreated ∼ 3 km between ∼ 8.6 ka to the modern ice margin at ∼ 8.0 ka. These retreat rates are consistent with late glacial and Holocene estimates for marine-terminating outlet glaciers across East Greenland, and comparable to modern retreat rates observed at the largest ice streams in northeastern, and northwestern Greenland.
Document Type: text
File Description: application/pdf
Language: English
Relation: https://cp.copernicus.org/articles/21/2263/2025/
DOI: 10.5194/cp-21-2263-2025
Availability: https://doi.org/10.5194/cp-21-2263-2025; https://cp.copernicus.org/articles/21/2263/2025/
Accession Number: edsbas.E2C0FFDE
Database: BASE