How closely do changes in surface and column water vapor follow Clausius-Clapeyron scaling in climate change simulations?
The factors governing the rate of change in the amount of atmospheric water vapor are analyzed in simulations of climate change. The global-mean amount of water vapor is estimated to increase at a differential rate of 7.3% K[superscript − 1] with respect to global-mean surface air temperature in the...
| Main Authors: | , |
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| Other Authors: | |
| Format: | Article |
| Language: | English |
| Published: |
IOP Publishing,
2011-06-23T17:14:01Z.
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| Subjects: | |
| Online Access: | Get fulltext |