The Cryosphere Discuss., 6, 2399-2436, 2012
www.the-cryosphere-discuss.net/6/2399/2012/
doi:10.5194/tcd-6-2399-2012
© Author(s) 2012. This work is distributed
under the Creative Commons Attribution 3.0 License.
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This discussion paper has been under review for the journal The Cryosphere (TC). Please refer to the corresponding final paper in TC.
The first complete glacier inventory for the whole of Greenland
P. Rastner1, T. Bolch1,2, N. Mölg1, H. Machguth1,3, and F. Paul1
1Department of Geography, University of Zurich, Winterthurer Str. 190, 8057 Zurich, Switzerland
2Institute for Cartography, Technische Universität Dresden, 01069 Dresden, Germany
3Marine Geology and Glaciology, Geological Survey of D. and Gl. – GEUS, Ø. Volgade 10, 1350 København, Denmark

Abstract. Glacier inventories provide important baseline information for the determination of water resources, glacier-specific changes in area and volume, climate change impacts, and the past, potential and future contribution of glaciers to sea-level rise. Though heavily glacierized and thus highly relevant for all of the above points, such an inventory of all local glaciers and icecaps (GIC) was not available so far for Greenland. Here we present the details and results of our inventory, that has been compiled from more than 70 Landsat scenes mostly acquired between 1999 and 2002 using semi-automated multispectral mapping techniques. A digital elevation model (DEM) was used to derive drainage divides from watershed analysis and topographic parameters for each glacier entity. We assigned to each entity one of three connectivity levels (CL0, CL1, CL2; i.e. no, weak, and strong connection) with the ice sheet to distinguish the local GIC from the ice sheet and its outlet glaciers and to serve the specific needs of different user communities. All GIC larger 0.05 km2 include ~20 300 entities (of which 900 are marine terminating), covering an area of 129 983 ± 4029 km2, or 89 273 ± 2767 km2 without the CL2 GIC. The latter is about 50% more than according to all previous estimates. Glaciers smaller 0.5 km2 contribute only 1.5% to the total area but more than 50% (11 000) to the total number. In contrast, the 25 largest GIC (>500 km2) contribute 28% to the total area, but only 0.1% to the total number. Most of the ice was located at elevations around 1000 m, except in the eastern sector with elevation arround 1700 m. In addition, a strong dependence of the median elevation to the distance from the ocean was found, but only a weak dependence on aspect. All data will be made available in the Global Land Ice Measurement from Space (GLIMS) glacier database.

Citation: Rastner, P., Bolch, T., Mölg, N., Machguth, H., and Paul, F.: The first complete glacier inventory for the whole of Greenland, The Cryosphere Discuss., 6, 2399-2436, doi:10.5194/tcd-6-2399-2012, 2012.
 
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