Climate models used for climate change projections are on the threshold of including much greater biological and chemical detail than previous models. Today, standard cli-mate models (referred to generically as atmosphere-ocean general circulation mod-els, or AOGCMs) include components that simulate...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.469.1221 2023-05-15T18:17:51+02:00 The Pennsylvania State University CiteSeerX Archives 2007 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.469.1221 http://www.cec.yamanashi.ac.jp/~tetsu/englishpaper/2008/3rd/2007EO200002.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.469.1221 http://www.cec.yamanashi.ac.jp/~tetsu/englishpaper/2008/3rd/2007EO200002.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.cec.yamanashi.ac.jp/~tetsu/englishpaper/2008/3rd/2007EO200002.pdf text 2007 ftciteseerx 2016-01-08T07:07:02Z Climate models used for climate change projections are on the threshold of including much greater biological and chemical detail than previous models. Today, standard cli-mate models (referred to generically as atmosphere-ocean general circulation mod-els, or AOGCMs) include components that simulate the coupled atmosphere, ocean, land, and sea ice. Some modeling centers are now incorporating carbon cycle models into AOGCMs in a move toward an Earth sys-tem model (ESM) capability. Additional can-didate components to include in ESMs are aerosols, chemistry, ice sheets, and dynamic vegetation [e.g., Cox et al., 2000; Friedling- Text Sea ice Unknown |
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Climate models used for climate change projections are on the threshold of including much greater biological and chemical detail than previous models. Today, standard cli-mate models (referred to generically as atmosphere-ocean general circulation mod-els, or AOGCMs) include components that simulate the coupled atmosphere, ocean, land, and sea ice. Some modeling centers are now incorporating carbon cycle models into AOGCMs in a move toward an Earth sys-tem model (ESM) capability. Additional can-didate components to include in ESMs are aerosols, chemistry, ice sheets, and dynamic vegetation [e.g., Cox et al., 2000; Friedling- |
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The Pennsylvania State University CiteSeerX Archives |
format |
Text |
publishDate |
2007 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.469.1221 http://www.cec.yamanashi.ac.jp/~tetsu/englishpaper/2008/3rd/2007EO200002.pdf |
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Sea ice |
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Sea ice |
op_source |
http://www.cec.yamanashi.ac.jp/~tetsu/englishpaper/2008/3rd/2007EO200002.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.469.1221 http://www.cec.yamanashi.ac.jp/~tetsu/englishpaper/2008/3rd/2007EO200002.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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