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Tropical free‐tropospheric humidity differences and their effect on the clear‐sky radiation budget in global storm‐resolving models
2021
Journal of Advances in Modeling Earth Systems
Free-tropospheric water vapor strongly impacts the Earth's outgoing longwave radiation (OLR) and therefore plays a key role in controlling the clear-sky response of the climate system to an increase in greenhouse gases. It is now widely accepted that this response is described by a warming and moistening of the atmosphere that is implied if the relative humidity (RH) and lapse rate were to depend on temperature alone, which corresponds to a warming at approximately constant RH (e.g., Held &
doi:10.1029/2021ms002514
fatcat:fzu2zp4xozan3daj7vkyhnit34