Arctic Climate

There has been a lot of attention on the influence of rapid warming of the Arctic on weather in the Northern Hemisphere mid-latitudes. Much of the work has focused on changes to the Jetstream amplitudes and association of these changes to ice loss in the Arctic. 

We know that the Arctic is heating faster than the planet as a whole. Consequently, there is more energy in the Arctic which can be transmitted to the atmosphere. Much of the excess heat is transferred to the atmosphere in the late fall or early winter. This extra energy is connected to what’s called Arctic geopotential height, which has increased during the same times of the year. As a consequence, the Jetstream might weaken in the cold seasons.

But what about summer? Have these changes been detected then too? Well just recently, a paper was published in that answered this question. The authors, from the Potsdam Institute for Climate Impact Research and from the University of Potsdam reported on three measures of atmospheric dynamics (1) zonal winds, (2) eddy kinetic energy, and (3) amplitude of the fast-moving Rossby waves. Rossby waves are very large waves in the upper atmospheric winds. They are important because of their large influence on weather.

http://www.theguardian.com/environment/climate-consensus-97-per-cent/2015/mar/16/climate-change-in-the-arctic-is-messing-with-our-weather