Holocene North Atlantic Overturning in an atmosphere-ocean-sea-ice model compared to proxy-based reconstructions

M. Blaschek; H. Renssen; C. Kissel; D. Thornalley

doi:10.1002/2015PA002828

Holocene North Atlantic Overturning in an atmosphere-ocean-sea-ice model compared to proxy-based reconstructions

M. Blaschek, H. Renssen, C. Kissel, D. Thornalley

Earth and Climate

Research output: Contribution to Journal › Article › Academic › peer-review

Abstract

Climate and ocean circulation in the North Atlantic region changed over the course of the Holocene, partly because of disintegrating ice sheets and partly because of an orbital-induced insolation trend. In the Nordic Seas, this impact was accompanied by a rather small, but significant, amount of Greenland ice sheet melting. We have employed the EMIC LOVECLIM and compared our model simulations with proxy-based reconstructions of δ

Original language	English
Journal	Paleoceanography
Issue number	30
DOIs	https://doi.org/10.1002/2015PA002828
Publication status	Published - 2015

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title = "Holocene North Atlantic Overturning in an atmosphere-ocean-sea-ice model compared to proxy-based reconstructions",

abstract = "Climate and ocean circulation in the North Atlantic region changed over the course of the Holocene, partly because of disintegrating ice sheets and partly because of an orbital-induced insolation trend. In the Nordic Seas, this impact was accompanied by a rather small, but significant, amount of Greenland ice sheet melting. We have employed the EMIC LOVECLIM and compared our model simulations with proxy-based reconstructions of δ",

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AU - Renssen, H.

AU - Kissel, C.

AU - Thornalley, D.

PY - 2015

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AB - Climate and ocean circulation in the North Atlantic region changed over the course of the Holocene, partly because of disintegrating ice sheets and partly because of an orbital-induced insolation trend. In the Nordic Seas, this impact was accompanied by a rather small, but significant, amount of Greenland ice sheet melting. We have employed the EMIC LOVECLIM and compared our model simulations with proxy-based reconstructions of δ

U2 - 10.1002/2015PA002828

DO - 10.1002/2015PA002828

M3 - Article

SN - 0883-8305

JO - Paleoceanography

JF - Paleoceanography

IS - 30

ER -

Holocene North Atlantic Overturning in an atmosphere-ocean-sea-ice model compared to proxy-based reconstructions

Abstract

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