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A method to derive the snow line elevation usingNOAA-AVHRR satellite data in combination witha digital elevation model is presented. The AVHRRsensor enables the frequent Observation of snow coverwith a sufficiently high temporal resolution.  The definition of the snow line and the impact of geocodingerrors, as well as errors due to misclassification,are discussed. A comparison of the NOAA-AVHRRdata with data from the higher resolution IRS-WiFSindicates that even at a spatial resolution of 1.1 km, aquantitative analysis of the snow line elevation is possible.  The influence of different winter conditions in Switzerland on the elevation of the snow line is reflected insatellite data from 1990,1996 and 1999. The results ofthe investigation were, firstly the presentation of thespatial pattern of the average snow line elevation, secondlythe derivation of snow line signatures for threeregions. These were then compared with the Overallalpine snow line signature

Spatial and temporal analysis of the snow line in the alps : based on NOAA-AVHRR data