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EOL Seminar Abstract


October 13 , 2006

How Do Clouds Regulate the Planetary Albedo and Climate Change?

It is remarkable that our general circulation climate models are able to explain the observed temperature trends during the last century solely through variations in greenhouse gases, aerosols and solar irradiance. This implies that the role of clouds in planetary albedo has not changed during the last 100 years by more than ±0.3% (out of 29 %). This seemingly improbable hypothesis has not been tested thus far. Another fundamental question we have to address is: Is the planetary albedo hovering around 29% , because of the need to maintain a habitable climate?; or is it sheer chance that the planet settled into the 29% albedo? There is practically no theory for either of these
two issues. New discoveries await us in a serious quest that sheds some observational insights into the processes by which aerosols and clouds regulate the albedo.

Professor Ramanathan will describe a new observing system that is designed to address the albedo regulation problem. It consists of vertically stacked and multiple UAVs (light weight and long range) carrying miniaturized aerosol-cloud-turbulence-radiation instruments. A campaign with 3 stacked UAVs was completed this year in the Indian Ocean and results from that experiment will be described to suggest that this new platform, in conjunction with models and other observations, offers a promising avenue for solving this outstanding problem in climate and climate change.

Friday October 13 at 3:30pm in FL2-1022.


 

 

 

 

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