Wind slab· Matin
- Above 1,700 m
- Taille
- 2
Stability: poor · Frequency: some
The danger is fresh, wind-drifted snow deposited in the form of wind slabs and pillows.
Stability: poor · Frequency: some
Stability: poor · Frequency: some
Stability: poor · Frequency: some
Stability: poor · Frequency: some
The danger is fresh, wind-drifted snow deposited in the form of wind slabs and pillows.
In the high altitudes of the Western and High Tatras (above 1700 m above sea level) the avalanche danger increases from 2nd to 3rd degree - CONSIDERABLE, due to snowfall and strong wind during the day. Snowfall accompanied by extremely strong northerly wind creates dangerous snow slabs and pillows of varying thickness. Their distribution is very local - depending on the relief and the prevailing wind direction. Often under saddles, rock walls and in leeward troughs, where new snow reaches more than 50 cm. Avalanche release on steep slopes is possible with only a small additional load. Occasional spontaneous medium-sized avalanches are possible.
The weather and snow cover changed significantly after a period of warm weather due to a strong cooling. Winter conditions prevail in the mountains and the air temperature has dropped to -10 to -20 °C. Between 15 and 30 cm of new snow will fall during the night from Saturday to Sunday + Sunday, but accompanied by extremely strong winds of 25 m/s, gusting up to 35 m/s. Older snow will freeze as a stone, and new snow of varying thickness will be on the surface - depending on wind and relief. At altitudes up to 1600 m there is almost no older snow under the new snow.
Rising during the day during snowfall.
Bulletin data: Stredisko lavínovej prevencie HZS (via EAWS / avalanche.report)