This graphic is a summit ice core timeline depicting the phenomena that as we drill deeper ice cores, the ice gets older. The graphic compares this timeframe with major milestones in history. It is a concept developed by Zoe Courville and Dr. Mary Albert at Dartmouth University, in partnership with CRREL (Cold Regions Research and Engineering Laboratory).
This blog documents the process of creating a 25-minute animated film at the University of Alaska Museum of the North that tells the story of bowhead whale annual migration in the Bering, Beaufort and Chukchi Seas. The film takes its basic narrative and title from the 2013 calendar edited by Steve Okkonen, A Year in the Life of Bowhead Whales
The life of the bowhead whales calendar is a teaching tool created by Dr. Steve Okkonen and colleagues to portray science and natural history of bowhead whales in a compelling form. The calendar is available as a PDF and in poster PDF forms.
The Transantarctic Mountains are an extreme example of rift flank uplift, extending over 3500 km across Antarctica and reaching elevations up to 4500 m (see map of the region). The mountain range was formed in the extensional environment associated with the breakup of Gondwanaland. Geological and geophysical work has shown that the Transantarctic Mountains developed along a long-lived lithospheric boundary
CTD Data plots from the Winter Sampling Expedition. CTD is an acronym for Conductivity-Temperature-Depth. It is a device that measures the salinity, temperature, depth in a vertical profile from the surface. The data comes from the Chukchi Sea.
Polar researchers Jackie Grebmeier and Lee Cooper, joined PolarTREC teacher Deanna Wheeler in a presentation about their work in the Bering Sea. The presentation was at the Old Durham Church in Maryland.