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Snow cover patterns in a 9.4 km 2 basin in the Austrian Alps are examined during spring and summer 1989. Digital mono‐plotting from oblique aerophotographs is used for mapping. on the basis of a square grid with 25 m spacing, snow cover as mapped during nine surveys is analysed as a function of elevation and slope. During winter conditions the snow cover is found to be much better related to these terrain features than during the late ablation period.
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Bl et al. (1992) studied this question.
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