May 27, 2008
Understanding the rate at which the sun’s energy is transferred from the atmosphere – through the sea ice – to the ocean in a particular summer is important to understanding the reduction of sea ice during summer we’ve seen over the last 30 years (see figure from last blog entry) and for making projections of the fate of the sea ice and its effect on global climate into the future using models. It will also help us understand why, in the summer of 2007, we witnessed the lowest extent of sea ice observed during its summer minimum since we’ve been able to measure it with satellites.


