Atlantic inflow into the southern Nordic Seas at the onset of the LGM promotes open-ocean conditions and Fennoscandian Ice Sheet growth
The Atlantic water inflow into the Nordic Seas has proven difficult to reconstruct for the Last Glacial Maximum (LGM). At that time, the Fennoscandian Ice Sheet grew potentially to its maximum extent. Sea-ice free conditions in the eastern Nordic Seas have been proposed as an essential moisture sour...
Main Authors: | , , , , , , , |
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Format: | Dataset |
Language: | unknown |
Published: |
SEANOE
2023
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Subjects: | |
Online Access: | https://doi.org/10.17882/96079 https://www.seanoe.org/data/00849/96079/ |