We found that Colorado River flows decline by about 4 percent per degree F increase, which is roughly the same amount as the increased atmospheric water
vapor holding capacity discussed above.
«[T] he CMIP5 [climate model] results instead show an increase in temperature and a much subdued increase in specific humidity, which may be due to GHG - induced warming and subsequent increases in the water
vapor holding capacity of the atmosphere, respectively.
Not exact matches
Therefore, the August - Roche - Magnus equation implies that saturation water
vapor pressure changes approximately exponentially with temperature under typical atmospheric conditions, and hence the water -
holding capacity of the atmosphere increases by about 7 % for every 1 °C rise in temperature.
The
capacity of the atmosphere to
hold water
vapor (saturation specific humidity) increases exponentially with temperature.