CL
Climate: Past, Present & Future

wind circulation

How glaciers record the winds of change

How glaciers record the winds of change

After decades of observation, one of the profound consequences of anthropogenic global warming is the rapid rise in temperature in the Arctic, refered to as Arctic Amplification. Compared to the mid-latitudes, warming in the Arctic is twice as fast. The reason is mainly due to the positive feedback of a melting cryosphere: Darker surfaces are revealed from melting cryosphere, reflecting less short ...[Read More]