Mapping of a Hydrological Ice Sheet Drainage Basin on the West Greenland Ice Sheet Margin from ERS-1/2 SAR Interferometry, Ice-Radar Measurement, and Modelling

• Published in: Annals of Glaciology
• Main Authors: Ahlstrøm, Andreas P., Bøggild, C.E., Stenseng, L., Mohr, Johan Jacob, Reeh, Niels, Christensen, Erik Lintz, Olesen, O.B., Keller, K.
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2002
• Subjects: Greenland; Tasersiaq; Annals of Glaciology; Ice Sheet
• Online Access: https://orbit.dtu.dk/en/publications/dc21ddab-977a-4267-8dfa-fa4a9d804c58; https://doi.org/10.3189/172756402781817860

The hydrological ice-sheet basin draining into the Tasersiaq lake, West Greenland (66°13'N, 50°30'W), was delineated, First using standard digital elevation models (DEMs) for ice-sheet surface and bedrock, and subsequently using a new high-resolution dataset, with a surface DEM derived from repeat-track interferometric synthetic aperture radar (SAR) and a bedrock topography derived from an airborne 60 MHz ice-penetrating radar. The extent of the delineation was calculated from a water-pressure potential as a function of the ice-sheet surface and bedrock elevations and a hydraulic factor κ describing the relative importance of the potential of the ice overburden pressure compared to the bedrock topography. The meltwater run-off for the basin delineations was modelled with an energy-balance model calibrated with observed ice-sheet ablation and compared to a 25 year time series of measured basin run-off. The standard DEMs were found to be inadequate for delineation purposes, whereas delineations from high-resolution data were found to be very sensitive to changes in κ in a non-linear way, causing a factor 5 change of basin area, corresponding to a doubling of the modelled runoff. The 50% standard deviation of the measured basin run-off could thus be explained by small year-to-year variations of the κ-factor