Bollettino valanghe

Werdenfels Alps

LWD Bayern
Vedi sulla mappa

Pericolo valanghe

Above 1,500 m· Mattina
2 · Moderato
Below 1,500 m· Mattina
1 · Debole
Above 1,500 m· Pomeriggio
3 · Marcato
Below 1,500 m· Pomeriggio
1 · Debole
Non aggiornato — questo bollettino è scaduto 6 months ago. Stai vedendo condizioni passate, non il bollettino in corso.

In sintesi

Danger of falling on a hard frozen snow surface!

Problemi valanghivi

  • Gliding snow· Mattina

    • Above 1,500 m
  • Gliding snow· Mattina

    • Below 1,500 m
  • Persistent weak layers· Mattina

    • Above 1,500 m
  • Wet snow· Pomeriggio

    • Above 1,500 m
  • Wet snow· Pomeriggio

    • Below 1,500 m
  • Persistent weak layers· Pomeriggio

    • Above 1,500 m

Avalanche Activity

Danger of falling on a hard frozen snow surface!

The avalanche danger above 1500 m increases from moderate to considerable during the daytime changes. Below that, it is low. Until the morning, gliding snow is the main problem at medium altitudes. Small and medium-sized gliding avalanches will spontaneously release themselves on a few steep slopes with a smooth surface. Staying under glide cracks should be avoided.

When the sun shines, the activity of sliding snow increases on sunny slopes and small and medium-sized, wet loose snow avalanches can be expected from extremely steep terrain that has not yet been discharged.

In addition, weak persistent layers above 1500 metres are problematic. With large additional loads, for example due to cornice breakage, large slab avalanches can also be triggered in isolated cases in the west, north and east aspects. Take particular care in transition areas from a little to a lot of snow.

Snowpack Structure

On the surface, the snowpack freezes overnight in many places and is capable of bearing loads; in the sun, it softens again during the day and soaking progresses. Up to high altitudes, the snowpack is slightly moist, in medium altitudes it is sometimes completely soaked to the ground. In shady slopes at higher altitudes, faceted crystals can be found deeper in the snowpack.

Tendency

Slow decline in the wet snow problem - the persistent weak layer problem remains.

Bulletin data: Avalanche Warning Service Bavaria (CC BY 4.0)

Regioni coperte