Chiemgau Alps East

Heed freshly generated snowdrifts

Heed freshly generated snowdrifts

Avalanche danger in the Bavarian Alps is moderate. At high altitudes the fresh snowdrift accumulations are the main problem. One sole skier can trigger a slab avalanche in steep ridgelin terrain in N/W/S aspects and in wind-loaded gullies and bowls. Particularly at high altitudes, the triggered avalanches can release enough snow to bury a person. Apart from that, during the course of the day the danger of moist and wet loose-snow and glide-snow avalanches will increase. In the afternoon, naturally triggering wet-snow avalanches can be expected up to nearly 2000 m. On shady slopes where snowfall has been heaviest, these can reach medium size.

Westerly winds are rising, will transport the loose snow to exposed ridgeline and summit zones. Thereby fresh snowdrift accumulations will be generated, deposted atop the loose layers of snow and be prone to triggering. In addition, the layer of dust from the Sahara is a potential weak layer, especially at high alitutdes. At low altitudes, rainfall will set in tomorrow and the snowfall level will ascend. Due to mild temperatures and rain seepage, the snowpack will become weakened on the surface. In addition, the snow is becoming wet from the warm earth, it could begin to glide as a single mass.

Wet snow is becoming a problem even at high altitude.