Arctic ice is declining rapidly—a trend with enormous implications for global weather and climate. Freshwater pours into the Arctic Ocean from the ice sheets and glaciers, and sea ice over the ocean itself is declining. Ocean Channels and currents there act as a kind of switchyard, sending fresh water into the North Atlantic, and small changes here may have larger impacts on climate downstream. To understand these processes, scientists are landing in small aircraft on the floating sea ice, and drilling down to study the water and currents below. Lamont-Doherty researchers Bill Smethie, Ronny Friedrich, Dale Chayes and Richard Perry report on their work here.
Date: April 28-May 18, 2012
Team: Bill Smethie, Ronny Friedrich, Dale Chayes, Richard Perry