Influence of Bering Strait flow and North Atlantic circulation on glacial sea-level changes
Sea-level fluctuations of about 20–30 m occurred throughout the last glacial period. These fluctuations seem to have been derived primarily from changes in the volume of Northern Hemisphere ice sheets 1–3, and cannot be attributed solely to ice melt caused by varying solar radiation 4. Here we use a...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.391.8727 2023-05-15T15:44:09+02:00 Influence of Bering Strait flow and North Atlantic circulation on glacial sea-level changes Aixue Hu Gerald A. Meehl Bette L. Otto-bliesner Claire Waelbroeck Weiqing Han Marie-france Loutre Kurt Lambeck Jerry X. Mitrovica Nan Rosenbloom The Pennsylvania State University CiteSeerX Archives 2010 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.391.8727 http://www.cgd.ucar.edu/ccr/publications/ngeo729.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.391.8727 http://www.cgd.ucar.edu/ccr/publications/ngeo729.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.cgd.ucar.edu/ccr/publications/ngeo729.pdf text 2010 ftciteseerx 2016-01-08T02:17:41Z Sea-level fluctuations of about 20–30 m occurred throughout the last glacial period. These fluctuations seem to have been derived primarily from changes in the volume of Northern Hemisphere ice sheets 1–3, and cannot be attributed solely to ice melt caused by varying solar radiation 4. Here we use a fully coupled climate model to show that the transport of relatively fresh Pacific water into the North Atlantic Ocean was limited when lower sea level restricted or closed the Bering Strait, resulting in saltier North Atlantic surface waters. This invigorated deep convection in the North Atlantic Ocean, strengthening meridional overturning circulation and northward heat transport in our model, which consequently promoted melting of ice sheets in North America and Europe. Our simulations show that the associated sea-level rise led to a reopening of the Bering Strait; the flux of relatively fresh water Text Bering Strait North Atlantic Unknown Bering Strait Pacific |
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ftciteseerx |
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English |
description |
Sea-level fluctuations of about 20–30 m occurred throughout the last glacial period. These fluctuations seem to have been derived primarily from changes in the volume of Northern Hemisphere ice sheets 1–3, and cannot be attributed solely to ice melt caused by varying solar radiation 4. Here we use a fully coupled climate model to show that the transport of relatively fresh Pacific water into the North Atlantic Ocean was limited when lower sea level restricted or closed the Bering Strait, resulting in saltier North Atlantic surface waters. This invigorated deep convection in the North Atlantic Ocean, strengthening meridional overturning circulation and northward heat transport in our model, which consequently promoted melting of ice sheets in North America and Europe. Our simulations show that the associated sea-level rise led to a reopening of the Bering Strait; the flux of relatively fresh water |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Aixue Hu Gerald A. Meehl Bette L. Otto-bliesner Claire Waelbroeck Weiqing Han Marie-france Loutre Kurt Lambeck Jerry X. Mitrovica Nan Rosenbloom |
spellingShingle |
Aixue Hu Gerald A. Meehl Bette L. Otto-bliesner Claire Waelbroeck Weiqing Han Marie-france Loutre Kurt Lambeck Jerry X. Mitrovica Nan Rosenbloom Influence of Bering Strait flow and North Atlantic circulation on glacial sea-level changes |
author_facet |
Aixue Hu Gerald A. Meehl Bette L. Otto-bliesner Claire Waelbroeck Weiqing Han Marie-france Loutre Kurt Lambeck Jerry X. Mitrovica Nan Rosenbloom |
author_sort |
Aixue Hu |
title |
Influence of Bering Strait flow and North Atlantic circulation on glacial sea-level changes |
title_short |
Influence of Bering Strait flow and North Atlantic circulation on glacial sea-level changes |
title_full |
Influence of Bering Strait flow and North Atlantic circulation on glacial sea-level changes |
title_fullStr |
Influence of Bering Strait flow and North Atlantic circulation on glacial sea-level changes |
title_full_unstemmed |
Influence of Bering Strait flow and North Atlantic circulation on glacial sea-level changes |
title_sort |
influence of bering strait flow and north atlantic circulation on glacial sea-level changes |
publishDate |
2010 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.391.8727 http://www.cgd.ucar.edu/ccr/publications/ngeo729.pdf |
geographic |
Bering Strait Pacific |
geographic_facet |
Bering Strait Pacific |
genre |
Bering Strait North Atlantic |
genre_facet |
Bering Strait North Atlantic |
op_source |
http://www.cgd.ucar.edu/ccr/publications/ngeo729.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.391.8727 http://www.cgd.ucar.edu/ccr/publications/ngeo729.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766378421083963392 |