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.
Not exact matches
By analyzing global
water vapor and temperature satellite data for the lower atmosphere, Texas A&M University
atmospheric scientist Andrew Dessler and his colleagues found that warming driven by carbon dioxide and other gases allowed the air to
hold more moisture, increasing the amount of
water vapor in the atmosphere.
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.
By harvesting
water vapor from the air and condensing it into liquid,
atmospheric water generators can essentially pull
water from the air, and these devices
hold a lot of promise for providing an independent source of drinking
water.
First, warm air
holds more
water vapor than cold air — and the rising air temperatures since the 1970s have caused the
atmospheric water vapor content to rise as well.