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Provedor de dados:  ArchiMer
País:  France
Título:  Ice-shelf collapse from subsurface warming as a trigger for Heinrich events
Autores:  Marcott, Shaun A.
Clark, Peter U.
Padman, Laurie
Klinkhammer, Gary P.
Springer, Scott R.
Liu, Zhengyu
Otto-bliesner, Bette L.
Carlson, Anders E.
Ungerer, Andy
Padman, June
He, Feng
Cheng, Jun
Schmittner, Andreas
Data:  2011-08
Ano:  2011
Palavras-chave:  Paleoceanography
Paleoclimatology
Abrupt climate change
Resumo:  Episodic iceberg-discharge events from the Hudson Strait Ice Stream (HSIS) of the Laurentide Ice Sheet, referred to as Heinrich events, are commonly attributed to internal ice-sheet instabilities, but their systematic occurrence at the culmination of a large reduction in the Atlantic meridional overturning circulation (AMOC) indicates a climate control. We report Mg/Ca data on benthic foraminifera from an intermediate-depth site in the northwest Atlantic and results from a climate-model simulation that reveal basin-wide subsurface warming at the same time as large reductions in the AMOC, with temperature increasing by approximately 2 C over a 1-2 kyr interval prior to a Heinrich event. In simulations with an ocean model coupled to a thermodynamically active ice shelf, the increase in subsurface temperature increases basal melt rate under an ice shelf fronting the HSIS by a factor of approximately 6. By analogy with recent observations in Antarctica, the resulting ice-shelf loss and attendant HSIS acceleration would produce a Heinrich event.
Tipo:  Text
Idioma:  Inglês
Identificador:  https://archimer.ifremer.fr/doc/00227/33819/32479.pdf

https://archimer.ifremer.fr/doc/00227/33819/32480.pdf

DOI:10.1073/pnas.1104772108

https://archimer.ifremer.fr/doc/00227/33819/
Editor:  Natl Acad Sciences
Formato:  application/pdf
Fonte:  Proceedings Of The National Academy Of Sciences Of The United States Of America (0027-8424) (Natl Acad Sciences), 2011-08 , Vol. 108 , N. 33 , P. 13415-13419
Direitos:  2011 National Academy of Sciences.

info:eu-repo/semantics/openAccess

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