High-resolution ice thickness and bed topography of a land-terminating section of the Greenland Ice Sheet, with links to GeoTIFFs and text files, supplement to: Lindbäck, Katrin; Pettersson, Rickard; Doyle, Samuel H; Helanow, Christian; Jansson, Peter; Kristensen, Steen Savstrup; Stenseng, Lars; Forsberg, René; Hubbard, Alun L (2014): High-resolution ice thickness and bed topography of a land-terminating section of the Greenland Ice Sheet. Earth System Science Data, 6(2), 331-338

• Main Authors: Lindbäck, Katrin, Pettersson, Rickard, Doyle, Samuel H, Helanow, Christian, Jansson, Peter, Kristensen, Steen Savstrup, Stenseng, Lars, Forsberg, René, Hubbard, Alun L
• Format: Dataset
• Language: English
• Published: PANGAEA - Data Publisher for Earth & Environmental Science 2014
• Subjects: File name; Uniform resource locator/link to file; Satellite remote sensing; Greenland; North Pole; Doyle; Kristensen; Steen; Isunnguata Sermia; Ørkendalen; glacier; Ice Sheet
• Online Access: https://dx.doi.org/10.1594/pangaea.830314; https://doi.pangaea.de/10.1594/PANGAEA.830314

We present ice thickness and bed topography maps with a high spatial resolution (250-500 m) of a land-terminating section of the Greenland Ice Sheet derived from ground-based and airborne radar surveys. The data have a total area of ~12 000 km^2 and cover the whole ablation area of the outlet glaciers of Isunnguata Sermia, Russell, Leverett, Ørkendalen and Isorlersuup up to the long-term mass balance equilibrium line altitude at ~1600 m above sea level. The bed topography shows highly variable subglacial trough systems, and the trough of Isunnguata Sermia Glacier is overdeepened and reaches an elevation of ~500 m below sea level. The ice surface is smooth and only reflects the bedrock topography in a subtle way, resulting in a highly variable ice thickness. The southern part of our study area consists of higher bed elevations compared to the northern part. The compiled data sets of ground-based and airborne radar surveys cover one of the most studied regions of the Greenland Ice Sheet and can be valuable for detailed studies of ice sheet dynamics and hydrology. : Spatial reference: WGS 84 Stereographic North Pole; False easting: 0; False northing: 0; Central meridian: -39; Standard parallel 1: 71By downloading the data set you agree to refer to the data set paper (Lindbäck et al., 2014, doi:10.5194/essd-6-331-2014) in presentations and publications arising from use of these data. The data set authors make no guarantees of product accuracy and the authors cannot be held liable for any errors, events, etc. arising from its use.