The water vapor feedback quantifies the change in outgoing LW and absorbed SW radiation at the top of the atmosphere due to changes in atmospheric water vapor concentration associated with a change in global mean surface temperature. It arises because water vapor absorbs both LW and SW radiation and its concentration is expected to increase exponentially with temperature. The equilibrium (saturation) concentration increases following fundamental thermodynamic theory of the Clausius-Clapeyron relationship. Although concentrations are usually below saturation (relative humidity less than 100%), this difference is well understood (Sherwood, Roca, et al.,
2010) and well captured by GCMs with adequate resolution (Sherwood, Ingram, et al.,
2010). Increases in specific humidity in response to 1 K of warming at constant relative humidity in the middle and upper troposphere result in a greater reduction in outgoing LW radiation than similar increases in the lower troposphere due to the masking effects of overlying water vapor and clouds (Soden et al.,
2008; Vial et al.,
2013). A given increase in specific humidity generally has a larger impact on LW than on SW radiation. GCM simulations and observations of the seasonal cycle, interannual variability, and climate trends all exhibit relatively small changes in relative humidity with warming, and therefore large increases in specific humidity with warming (Boucher et al.,
2013; Dessler & Sherwood,
2009). The agreement of observations and GCMs with expectations from basic thermodynamic theory (Romps,
2014) leads to high confidence in robustly positive water vapor feedback.