Warm Water Causes Extra-cold Winters

Tapio Schneider, Frank J. Gilloon Professor of Environmental Science and Engineering, and Dr. Yohai Kaspi have found a mechanism that helps explain why average winter temperatures in northern Europe are at least 10 degrees Fahrenheit warmer than similar latitudes on the northeastern coast of the United States. Using computer simulations of the atmosphere, they have found that the warm water off an eastern coast will heat the air above it and lead to the formation of atmospheric waves, drawing cold air from the northern polar region. The cold air forms a plume just to the west of the warm water. In the case of the Atlantic Ocean, this means the frigid air ends up right over the northeastern United States. [Caltech Press Release]

Tags: research highlights ESE Tapio Schneider