Holocene lowering of the Laurentide ice sheet affects North Atlantic gyre circulation and climate

The Laurentide ice sheet, which covered Canada during glacial periods, had a major influence on atmospheric circulation and surface climate, but its role in climate during the early Holocene (9–7 ka), when it was thinner and confined around Hudson Bay, is unclear. It has been suggested that the demi...

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Bibliographic Details
Published in:Climate Dynamics
Main Authors: Gregoire, Lauren J., Ivanovic, Ruza F., Maycock, Amanda C., Valdes, Paul J., Stevenson, Samantha
Format: Article in Journal/Newspaper
Language:English
Published: 2018
Subjects:
8.2 kyr event
Atmospheric circulation
Holocene
Ice sheet topography
Laurentide Ice sheet
Wind driven Ocean circulation
Canada
Curl
Hudson
Hudson Bay
Ice Sheet
Iceland
North Atlantic
Online Access:https://hdl.handle.net/1983/3555adb8-a664-4382-a119-0e601249e95f
https://research-information.bris.ac.uk/en/publications/3555adb8-a664-4382-a119-0e601249e95f
https://doi.org/10.1007/s00382-018-4111-9
https://research-information.bris.ac.uk/ws/files/153590498/Full_text_PDF_final_published_version_.pdf
http://www.scopus.com/inward/record.url?scp=85041566365&partnerID=8YFLogxK

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