Wet snow
- All elevations
- Size
- 2
Stability: poor · Frequency: some
As a consequence of the strong warming, the occurrence of wet and gliding avalanches is possible.
Stability: poor · Frequency: some
Stability: poor · Frequency: few
As a consequence of the strong warming, the occurrence of wet and gliding avalanches is possible.
MODERATE (2) avalanche danger level prevails in the Fatras and the eastern part of the Low Tatras. Wet snow is a defining avalanche problem, especially in the afternoon. Avalanche release is possible especially with high additional loads, but spontaneous wet avalanches on steep slopes are also expected. Sliding (foundation) avalanches may also occur on grassy slopes.
As a result of the strong warming (the 0°C isotherm rises up to 2300 m above sea level), the snow cover is wet especially in the afternoon, often in the whole profile. Wind-exposed ridges are often blown onto hard, even icy, surfaces. Continuous snow cover is found from 1100 (1200) m above sea level, reaching a height of 50 to 150 cm above the tree line
INCREASING when it gets warmer during the day
Bulletin data: Stredisko lavínovej prevencie HZS (via EAWS / avalanche.report)