LETTERS Influence of the Thermohaline Circulation on Projected Sea Level Rise
A zonally averaged three-basin ocean–atmosphere model is used to investigate mean steric sea level rise in global warming scenarios. It is shown that if the North Atlantic deep water formation stops due to global warming, steric sea level rise is much larger for the same global mean atmospheric temp...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.502.3384 2023-05-15T17:25:23+02:00 LETTERS Influence of the Thermohaline Circulation on Projected Sea Level Rise Reto Knutti Thomas F. Stocker The Pennsylvania State University CiteSeerX Archives 1999 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.502.3384 http://www.climate.unibe.ch/~stocker/papers/knutti00jc.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.502.3384 http://www.climate.unibe.ch/~stocker/papers/knutti00jc.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.climate.unibe.ch/~stocker/papers/knutti00jc.pdf text 1999 ftciteseerx 2016-01-08T09:11:42Z A zonally averaged three-basin ocean–atmosphere model is used to investigate mean steric sea level rise in global warming scenarios. It is shown that if the North Atlantic deep water formation stops due to global warming, steric sea level rise is much larger for the same global mean atmospheric temperature increase than if the thermohaline circulation remains near the present state. In the equilibrium, global mean steric sea level rise depends linearly on the global mean atmospheric temperature increase. The influence of different subgrid-scale ocean mixing parameterizations on steric sea level rise is investigated. 1. Text North Atlantic Deep Water North Atlantic Unknown |
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ftciteseerx |
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English |
description |
A zonally averaged three-basin ocean–atmosphere model is used to investigate mean steric sea level rise in global warming scenarios. It is shown that if the North Atlantic deep water formation stops due to global warming, steric sea level rise is much larger for the same global mean atmospheric temperature increase than if the thermohaline circulation remains near the present state. In the equilibrium, global mean steric sea level rise depends linearly on the global mean atmospheric temperature increase. The influence of different subgrid-scale ocean mixing parameterizations on steric sea level rise is investigated. 1. |
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The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Reto Knutti Thomas F. Stocker |
spellingShingle |
Reto Knutti Thomas F. Stocker LETTERS Influence of the Thermohaline Circulation on Projected Sea Level Rise |
author_facet |
Reto Knutti Thomas F. Stocker |
author_sort |
Reto Knutti |
title |
LETTERS Influence of the Thermohaline Circulation on Projected Sea Level Rise |
title_short |
LETTERS Influence of the Thermohaline Circulation on Projected Sea Level Rise |
title_full |
LETTERS Influence of the Thermohaline Circulation on Projected Sea Level Rise |
title_fullStr |
LETTERS Influence of the Thermohaline Circulation on Projected Sea Level Rise |
title_full_unstemmed |
LETTERS Influence of the Thermohaline Circulation on Projected Sea Level Rise |
title_sort |
letters influence of the thermohaline circulation on projected sea level rise |
publishDate |
1999 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.502.3384 http://www.climate.unibe.ch/~stocker/papers/knutti00jc.pdf |
genre |
North Atlantic Deep Water North Atlantic |
genre_facet |
North Atlantic Deep Water North Atlantic |
op_source |
http://www.climate.unibe.ch/~stocker/papers/knutti00jc.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.502.3384 http://www.climate.unibe.ch/~stocker/papers/knutti00jc.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766116801117159424 |