| Summary: | Ice mélange is a densely packed, granular material consisting of icebergs bound together with sea ice in a rigid matrix at glacier termini. Ice mélange has been shown to affect glacier stability and terminus dynamics at some tidewater glaciers by influencing glacier advance and retreat, inhibiting calving, changing fjord circulation, and altering near surface ocean temperatures which can change iceberg melt rates. Prior studies have focused on extreme cases of mélange formation where mélange exists year-round or in winter. These studies indicate that mélange can provide significant back stress or a “buttressing” effect on the terminus through lateral resistance with fjord walls and dynamic jamming of mélange which creates large localized resistive stresses. For some Greenland glaciers, a short-lived mélange can develop following winter mélange disintegration and this mélange’s ability to impact terminus flow is undetermined. Here, I illustrate the capability of short-term, summer mélange at Rink Isbræ, West Greenland to compress and stabilize a rifting piece of terminus, that we term a loose ""ice tooth,"" torn open following three large calving events ranging in surface area from 0.22 km2 to 0.64 km2. Using terrestrial radar interferometry, I analyze variations in glacier and mélange velocities within 0.5 km of the terminus of Rink Isbrae during calving events, evaluate mélange rigidity, and determine the forces acting on a calving iceberg to estimate the shear strength of terminus ice at Rink Isbrae. While the mélange did not affect flow of fully attached glacier ice, mélange indirectly influences glacier dynamics by 1) compressing developing mélange on the ice tooth, which slowed down the ice tooth after calving, and 2) temporarily stabilizing the ice tooth as the mélange developed through ice-to-rock contact along the fjord walls. The in-situ terminus shear strength I find, 50 kPa to 540 kPa, falls on the low end of shear strengths of ice proposed by prior field and theoretical experiments, which have been ...
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