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<p><strong>Abstract.</strong> We report on the recent reactivation of a large rift in the Brunt Ice Shelf, East Antarctica, in December 2012 and the formation of a 50<span class="thinspace"></span>km long new rift in October 2016. Observations from a suite of ground-based and remote sensing instruments between January 2000 and July 2017 were used to track progress of both rifts in unprecedented detail. Results reveal a steady accelerating trend in their width, in combination with alternatingdoi:10.5194/tc-12-505-2018 fatcat:soxnagwmmfeknonjjjhmgd5tde