Is Water Vapor in the Stratosphere Slowing Global Warming?
Friday, January 29, 2010 - 11:14
in Earth & Climate
Earth's stratosphere is a cold, dry place, above the troposphere--the bottom layer of the atmosphere we breathe on a daily basis. Ruled by winds and hosting everything from bacteria to long-distance jet travel, about the only way that water gets into this high-altitude layer 10 kilometers above the Earth's surface is when it billows up from the humid tropics, rising from the troposphere via the atmospheric interface known as the tropopause. But since 2001 there has been less water vapor in a narrow, lower band of the stratosphere thanks to cooler temperatures in the tropopause, and that may just be holding back global warming at ground level, according to new research published online in Science on January 28. [More]