Lasörling Group

Increase in avalanche danger in the evening.

Increase in avalanche danger in the evening.

During the day: As a consequence of new snow and a sometimes strong southwesterly wind, mostly small wind slabs will form. The fresh wind slabs can in very isolated cases be released, even by a single winter sport participant, especially on very steep shady slopes above approximately 2600 m. These avalanche prone locations are to be found in particular in gullies and bowls, and behind abrupt changes in the terrain. The prevalence of the avalanche prone locations will increase with altitude. In very isolated cases dry avalanches can also be released in the old snowpack. Avalanche prone locations are to be found in particular in little used terrain above approximately 2400 m, especially on very steep shady slopes. Mostly avalanches are small. Only isolated gliding avalanches are possible. Evening and first half of night: Increase in danger of dry avalanches as the snowfall becomes more intense, in particular on steep shady slopes at high altitudes and in high Alpine regions.

In some localities up to 10 cm of snow, and even more in some localities, will fall on Thursday above approximately 1500 m, especially in the evening. The snowpack remains subject to considerable local variations. Within the snowpack, there are multiple melt-freeze crusts sandwiches with faceted layers in between, in particular on steep sunny slopes in all altitude zones, as well as on shady slopes below approximately 2600 m. At intermediate altitudes only a little snow is lying.

Significant increase in avalanche danger as a consequence of new snow and wind. Over a wide area 20 to 40 cm of snow will fall on Friday above approximately 1500 m. Especially from the Ortler Range via the Passeier Tal to the Southern Zillertal Alps and High Tauern up to 70 cm of snow will fall. More frequent natural dry avalanches are to be expected, even large ones in isolated cases, especially on steep shady slopes at high altitudes and in high Alpine regions in the regions exposed to heavier precipitation. As a consequence of the snowfall, the likelihood of gliding avalanches being released will increase gradually in particular on steep grassy slopes at intermediate and high altitudes.