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dc.contributor.authorSokolov, Andrei
dc.date.accessioned2010-08-26T15:36:53Z
dc.date.available2010-08-26T15:36:53Z
dc.date.issued2010-08
dc.identifier.urihttp://globalchange.mit.edu/pubs/abstract.php?publication_id=2070
dc.identifier.urihttp://hdl.handle.net/1721.1/57566
dc.descriptionAbstract and PDF report are also available on the MIT Joint Program on the Science and Policy of Global Change website (http://globalchange.mit.edu/)en_US
dc.description.abstractThe possible correlation between climate sensitivity and radiative forcing is studied using versions of the NCAR Community Atmospheric Model (CAM) model with different climate sensitivities. No such correlation was found for the CO2 forcing. A weak correlation for the direct sulfate aerosol forcing is associated with differences in cloud cover in control climate simulations with different versions of the model. Presented results suggest that correlation between sensitivity and radiative forcing in the 20th century simulations with different AOGCMs is not a reflection of physical reality but is a result of different treatments of forcing agents, primarily aerosols.en_US
dc.description.sponsorshipThis study received support from the MIT Joint Program on the Science and Policy of Global Change, which is funded by a consortium of government, industry and foundation sponsors.en_US
dc.language.isoen_USen_US
dc.publisherMIT Joint Program on the Science and Policy of Global Changeen_US
dc.relation.ispartofseries;Report no. 188
dc.titleOn the Correlation between Forcing and Climate Sensitivityen_US
dc.typeTechnical Reporten_US
dc.identifier.citationReport no. 188en_US


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