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

M. Marcer Arctic Technology Centre ARTEK, Department of Civil Engineering, Technical University of Denmark, Brovej, Building 118, 2800 Kgs. Lyngby, Denmark; Institut de Géographie Alpine IGA, PACTE, Université Grenoble-Alpes, Avenue Marie Reynoard 14 bis, 3800 Grenoble, FranceCorrespondence[email protected]

P. A. Stentoft Arctic Technology Centre ARTEK, Department of Civil Engineering, Technical University of Denmark, Brovej, Building 118, 2800 Kgs. Lyngby, Denmark; DTU Environment, Technical University of Denmark, Bygningstorvet Bygning 115, 2800 Kgs. Lyngby, Denmark

E. Bjerre Arctic Technology Centre ARTEK, Department of Civil Engineering, Technical University of Denmark, Brovej, Building 118, 2800 Kgs. Lyngby, Denmark; DTU Environment, Technical University of Denmark, Bygningstorvet Bygning 115, 2800 Kgs. Lyngby, Denmark

E. Cimoli Arctic Technology Centre ARTEK, Department of Civil Engineering, Technical University of Denmark, Brovej, Building 118, 2800 Kgs. Lyngby, Denmark; Institute for Marine and Antarctic Studies, University of Tasmania, Castray Explanade 20, 7004 Hobart, Australia

A. Bjørk Centre for GeoGenetics, Natural History Museum of Denmark, Oster Voldgade 5–7, 1350 Copenhagen K, Denmark

L. Stenseng DTU Space—National Space Institute, Technical University of Denmark, Department of Geodesy, Elektrovej 328, DK-2800 Kgs. Lyngby, Denmark

H. Machguth Arctic Technology Centre ARTEK, Department of Civil Engineering, Technical University of Denmark, Brovej, Building 118, 2800 Kgs. Lyngby, Denmark; Department of Geography, University of Zurich, Winterthurerstrasse 190, 8057 Zurich, Switzerland; Department of Geosciences, University of Fribourg, Chemin du Musée 4, 1700 Fribourg, Switzerland

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

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

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