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Calving retreat and proglacial lake growth at Hooker Glacier,Southern Alps,New Zealand
Authors:Clare M Robertson  Martin S Brook  Kat A Holt  Ian C Fuller  Douglas I Benn
Institution:1. Physical Geography Group, Institute of Natural Resources, Massey University, , Palmerston North, New Zealand;2. Moultrie Geology, , Banyo, Queensland, Australia;3. Department of Geology, University Centre in Svalbard, , Longyearbyen, Norway;4. School of Geography and Geosciences, University of St Andrews, , St Andrews, UK
Abstract:Hooker Glacier in the central Southern Alps of New Zealand has undergone significant downwasting and recession (~2.14 km) during the last two centuries. High retreat rates (51 m a?1 1986–2001, 43 m a?1 2001–2011) have produced a large (1.22 km2) proglacial lake. We present a retreat scenario for Hooker Glacier. A retreat scenario predicts that the glacier terminus will stabilise >3 km up‐valley of the current lake outlet after 2028 when ice velocity equals calving rate.
Keywords:calving retreat  Hooker Glacier  proglacial lake
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