The CLIVAR C20C project: selected twentieth century climate events
Abstract We use a simple methodology to test whether a set of atmospheric climate models with prescribed radiative forcings and ocean surface conditions can reproduce twentieth century climate variability. Globally, rapid land surface warming since the 1970s is reproduced by some models but others w...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.629.9418 2023-05-15T17:32:45+02:00 The CLIVAR C20C project: selected twentieth century climate events S. Kusunoki T. Nakaegawa The Pennsylvania State University CiteSeerX Archives 2008 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.629.9418 http://www.lasg.ac.cn/uploadfiles/file/papers/2008/2008clmdyn_c20c_part one.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.629.9418 http://www.lasg.ac.cn/uploadfiles/file/papers/2008/2008clmdyn_c20c_part one.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.lasg.ac.cn/uploadfiles/file/papers/2008/2008clmdyn_c20c_part one.pdf text 2008 ftciteseerx 2016-01-08T15:24:09Z Abstract We use a simple methodology to test whether a set of atmospheric climate models with prescribed radiative forcings and ocean surface conditions can reproduce twentieth century climate variability. Globally, rapid land surface warming since the 1970s is reproduced by some models but others warm too slowly. In the tropics, air-sea coupling allows models to reproduce the Southern Oscil-lation but its strength varies between models. We find a strong relationship between the Southern Oscillation in global temperature and the rate of global warming, which could in principle be used to identify models with realistic climate sensitivity. This relationship and a weak response to ENSO suggests weak sensitivity to changes in sea sur-face temperature in some of the models used here. In the tropics, most models reproduce part of the observed Sahel drought. In the extratropics, models do not reproduce the observed increase in the North Atlantic Oscillation in response to forcings, through internal variability, or as a combination of both. Text North Atlantic North Atlantic oscillation Unknown |
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ftciteseerx |
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English |
description |
Abstract We use a simple methodology to test whether a set of atmospheric climate models with prescribed radiative forcings and ocean surface conditions can reproduce twentieth century climate variability. Globally, rapid land surface warming since the 1970s is reproduced by some models but others warm too slowly. In the tropics, air-sea coupling allows models to reproduce the Southern Oscil-lation but its strength varies between models. We find a strong relationship between the Southern Oscillation in global temperature and the rate of global warming, which could in principle be used to identify models with realistic climate sensitivity. This relationship and a weak response to ENSO suggests weak sensitivity to changes in sea sur-face temperature in some of the models used here. In the tropics, most models reproduce part of the observed Sahel drought. In the extratropics, models do not reproduce the observed increase in the North Atlantic Oscillation in response to forcings, through internal variability, or as a combination of both. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
S. Kusunoki T. Nakaegawa |
spellingShingle |
S. Kusunoki T. Nakaegawa The CLIVAR C20C project: selected twentieth century climate events |
author_facet |
S. Kusunoki T. Nakaegawa |
author_sort |
S. Kusunoki |
title |
The CLIVAR C20C project: selected twentieth century climate events |
title_short |
The CLIVAR C20C project: selected twentieth century climate events |
title_full |
The CLIVAR C20C project: selected twentieth century climate events |
title_fullStr |
The CLIVAR C20C project: selected twentieth century climate events |
title_full_unstemmed |
The CLIVAR C20C project: selected twentieth century climate events |
title_sort |
clivar c20c project: selected twentieth century climate events |
publishDate |
2008 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.629.9418 http://www.lasg.ac.cn/uploadfiles/file/papers/2008/2008clmdyn_c20c_part one.pdf |
genre |
North Atlantic North Atlantic oscillation |
genre_facet |
North Atlantic North Atlantic oscillation |
op_source |
http://www.lasg.ac.cn/uploadfiles/file/papers/2008/2008clmdyn_c20c_part one.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.629.9418 http://www.lasg.ac.cn/uploadfiles/file/papers/2008/2008clmdyn_c20c_part one.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766131006872485888 |