Abstract
In the summer of 1989 a glacio-meteorological experiment was carried out on Hintereisferner, Austria. At all stakes the albedo was measured several times with a simple light-weight instrument (described separately in the Appendix). The absorption of solar radiation was calculated for all stake positions, taking into account local albedo, slope, aspect and shading effects. It appears that the differences in ablation can be explained almost entirely by the differences in surface albedo, both along and across the glacier tongue. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 319-324 |
| Number of pages | 6 |
| Journal | Journal of Glaciology |
| Volume | 38 |
| Issue number | 130 |
| DOIs | |
| Publication status | Published - 1 Jan 1992 |
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