Atlantic water inflow to Labrador Sea and its interaction with ice sheet dynamics during the Holocene

Atlantic water inflow to Labrador Sea and its interaction with ice sheet dynamics during the Holocene

The hydrodynamics of the Labrador Sea, controlled by the complex interplay of oceanographic, atmospheric and ice-sheet processes, play a crucial role for the Atlantic Meridional Overturning Circulation (AMOC). An improved understanding of the hydrodynamics and its forcing in the past could therefore...

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Bibliographic Details
Main Authors: Hebbeln, D. (Author), Kienast, M. (Author), Lochte, A.A (Author), McCave, I.N (Author), Saini, J. (Author), Stein, R. (Author), Titschack, J. (Author), Weiser, J. (Author)
Format: Article
Language:English
Published: Elsevier Ltd 2021
Subjects:
8.2-ka event
Agassiz
AMOC
Analytical geochemistry
Arctic
Atlantic meridional overturning circulations
Atlantic Ocean
Atlantic Ocean (North)
atmosphere-ocean coupling
Atmospheric cooling
Baffin Bay
British Columbia
Canada
Current-speed reconstructions
Geochemical analysis
Glacial geology
Glacial Lake Agassiz
glacier advance
Glaciers
grain size
Grain size and shape
Greenland
Greenland Ice Sheet
Heat transfer
Holocene
Holocene thermal maximums
Hydrodynamics
Hypsithermal
Ice
Labrador Sea
Melting
meltwater
Melt-water discharges
microfossil
Mooring
Oceanography
seawater
Sortable Silt
surface water
Surface waters
West Greenland
West greenland currents
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