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Analysis of the weak layers: (on a basis of several snow profiles and stabiliy tests):

Danger level 2 . Avalanche report for the Bavarian Alps Saturday, 24.12.2005, 07.30 am General: - 10 to 20cm new snow during the last 24 hours, light rain in low altitudes - clear up during the night. - Today: sonny by changing cloudy conditions, temperatures rising up to zero degrees at 2000 m

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Analysis of the weak layers: (on a basis of several snow profiles and stabiliy tests):

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  1. Danger level 2 Avalanche report for the Bavarian Alps Saturday, 24.12.2005, 07.30 am General:- 10 to 20cm new snow during the last 24 hours, light rain in low altitudes- clear up during the night.- Today: sonny by changing cloudy conditions, temperatures rising up to zero degrees at 2000 m Snowcover conditions:Low altidudes:- slightly moist snowsurface as a result of the rain- thin melt-freeze crust as a result of the clearence during the night, up to intermediate altitudes - In intermediate elevations the new snow lies on a well settled old snow cover that is still powdery. - good bonding between the new snow and the old snow cover surface Above the tree line: - from the wind intensely affected snowcover - Keep in mind the week bonding between the intens faceted snow layers near the ground and the overlaying wind packed layers. - Yesterday during the day little, fresh snow drinft accumulations were built up temporary by northwesterly winds. Avalanche danger:- moderate avalanche danger - avalanche prone terrain: mainly steep terrain adjacent to the ridge line in the aspects N-E-SE above about 1800m as well as in gullies and bowls with snow drift accumulations - Mainly in transition zones between bear areas and slopes charged with wind drift acculuations in particular with high additional loading, e.g. a goup without spacing, the release of a slab avalanche is possible.- As a result of the warming during the day and the insolation the new snow of the last days may release as little, superficial loose snow avalanches and slab avalanches on rocky, steep slopes. - In low and intermediate altitudes ground avalanches may occur as a result of the increasing humidity penetration. • Analysis of the weak layers: • (on a basis of several snow profiles and stabiliy tests): • visible weak layer between 50 and 80cm beneath the surface • the weak layer breaks plain, but not until high additional loading • the weak layer is relatively thin • the overlaying layers are bonded and rather compact

  2. Danger level 2 Reasons for the danger level Typical avalanche prone locations: New snow (10-20cm) only with little relevance, as the case may be the bonding between the old and new snow from the 17./18.12. could be problematic, but the overlaying layer is relatively compact. Number of avalanche prone locations: Slopes near the ridge line and gullies with wind drifted snow, avalanche prone locations definable, on some slopes  matrix row 2 Realease probability: A singel skier is in general not enough additional load, large additional load necessary  matrix row 2 As the case may be spontaneous little avalanches at the snow surface  matrix column 5 Information from observers, avalanches No avalanche releases in high altitudes. Few little wet snow avalanches near the snow surface (loose snow avalanches) in SE-S-SW exposed slopes between 1300 and 1800m. Few little loose snow and full-depth slab avalanches in SE-S-.SW exposed slopes below 1300m.

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