Three Decades of Volume Change of a Small Greenlandic Glacier Using Ground Penetrating Radar, Structure from Motion, and Aerial Photogrammetry

Glaciers in the Arctic are losing mass at an increasing rate. Here we use surface topography derived from Structure from Motion (SfM) and ice volume from ground penetrating radar (GPR) to describe the 2014 state of Aqqutikitsoq glacier (2.85 km2) on Greenland's west coast. A photogrammetrically...

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Bibliographic Details
Published inArctic, antarctic, and alpine research Vol. 49; no. 3; pp. 411 - 425
Main Authors Marcer, M, Stentoft, P. A, Bjerre, E, Cimoli, E, Bjørk, A, Stenseng, L, Machguth, H
Format Journal Article
LanguageEnglish
Published Boulder Institute of Arctic and Alpine Research (INSTAAR), University of Colorado 01.08.2017
Taylor & Francis
Institute of Arctic and Alpine Research
Taylor & Francis Ltd
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