A $17 million expedition aimed at studying the effects of climate change in Canada’s Hudson Bay has been postponed due to complications brought about by climate change itself. An unusually heavy southward flow of surface ice from the Arctic has blocked the safe passage of the Canadian Research Icebreaker CCGS Amundsen, on the first leg of her mission to ferry 40 scientists participating in the Hudson Bay System Study (BaySys).
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The massive crack running through Antarctica’s fourth-largest ice shelf dramatically accelerated its growth last month, extending over 11 miles in just six days. According to the UK-based Project Midas research group, the 110 kilometer (68 mile) long chasm extended an additional 17 km (11 miles) between May 25 and May 31.

The crack’s course has also suddenly turned seaward, with only 13 km (8 miles) remaining before the ice front calves off. Provided the ice front stays intact after calving, the resulting iceberg would account for more than ten percent of Larsen C’s area, a 5,000 square kilometer (1,150 sq mi) island of ice 350 meters (1,150 feet) thick, approximately the size of the state of Delaware. A berg that size would be one of the largest on record.
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The results of two new studies regarding Antarctic glaciers have been released, and the results of each shocked the researchers conducting them, including the first on-site survey of the Totten Ice Shelf, and the first large-scale survey of the Antarctic continent as a whole. Additionally, the results of the two studies do not paint an optimistic picture for the stability of our southern continent’s glaciers.
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