Science, Volume 310John Michels (Journalist) Science Company, Moses King, 2005 A weekly record of scientific progress. |
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Page 841
... water vapor in the upper troposphere could double by the end of the century as a result of increases in greenhouse gases . Such moistening plays a key role in amplifying the rate at which the climate warms in response to anthropogenic ...
... water vapor in the upper troposphere could double by the end of the century as a result of increases in greenhouse gases . Such moistening plays a key role in amplifying the rate at which the climate warms in response to anthropogenic ...
Page 842
... water vapor , T12 , T2 , and T2 - T12 . The standard errors are estimated following Weatherhead et al . ( 42 ) . The rightmost column shows the trends for which the GCM - simulated T12 was computed under the " no moistening " scenario ...
... water vapor , T12 , T2 , and T2 - T12 . The standard errors are estimated following Weatherhead et al . ( 42 ) . The rightmost column shows the trends for which the GCM - simulated T12 was computed under the " no moistening " scenario ...
Page 844
... water vapor . Given the importance of water vapor feedback in determining the climatic response to anthropogenic forcings , such confirmation is essential to the use of these models for global warming projections . References and Notes ...
... water vapor . Given the importance of water vapor feedback in determining the climatic response to anthropogenic forcings , such confirmation is essential to the use of these models for global warming projections . References and Notes ...
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