Rapid northern hemisphere ice sheet melting during the penultimate deglaciation

The rate and consequences of future high latitude ice sheet retreat remain a major concern given ongoing anthropogenic warming. Here, new precisely dated stalagmite data from NW Iberia provide the first direct, high-resolution records of periods of rapid melting of Northern Hemisphere ice sheets dur...

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Bibliographic Details
Main Authors: Stoll, Heather M., Cacho, Isabel, Gasson, Edward, Sliwinski, Jakub, Kost, Oliver, Moreno, Ana, Iglesias, Miguel, Torner, Judit, Perez-Mejias, Carlos, Haghipour, Negar, Cheng, Hai, Edwards, R. Lawrence
Format: Article in Journal/Newspaper
Language:English
Published: Nature 2022
Subjects:
Palaeoceanography
Palaeoclimate
Ice Sheet
North Atlantic
Online Access:https://hdl.handle.net/20.500.11850/557118
https://doi.org/10.3929/ethz-b-000557118
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Summary:The rate and consequences of future high latitude ice sheet retreat remain a major concern given ongoing anthropogenic warming. Here, new precisely dated stalagmite data from NW Iberia provide the first direct, high-resolution records of periods of rapid melting of Northern Hemisphere ice sheets during the penultimate deglaciation. These records reveal the penultimate deglaciation initiated with rapid century-scale meltwater pulses which subsequently trigger abrupt coolings of air temperature in NW Iberia consistent with freshwater-induced AMOC slowdowns. The first of these AMOC slowdowns, 600-year duration, was shorter than Heinrich 1 of the last deglaciation. Although similar insolation forcing initiated the last two deglaciations, the more rapid and sustained rate of freshening in the eastern North Atlantic penultimate deglaciation likely reflects a larger volume of ice stored in the marine-based Eurasian Ice sheet during the penultimate glacial in contrast to the land-based ice sheet on North America as during the last glacial. ISSN:2041-1723

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