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Comparison of direct and geodetic mass balances on a multi-annual time scale

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Figure

Fig. 1. Calculation of geodetic mass balance between t1 and t2. Themass loss at the surface removes a layer of ice, firn and possiblysnow, the gained mass has a much lower density
Table 1. Austrian glaciers chosen for the comparison the direct and the geodetic method
Fig. 4. Oblique photographs of the plateau glaciers SSK and HK, and the valley glaciers HEF, VF, KWF and JAM.
Table 2. Date and method of DEM acquisition at the test glaciers JAM, HEF, KWF, VF, SSK and HK
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