Wet snow· Mattina
N
NE
E
SE
S
SW
W
NW
- Above 1,700 m
- Dimensione
- 2
Stability: very poor · Frequency: few
Bollettino valanghe
Vedi sulla mappaZápadné Tatry
HZS
Pericolo valanghe
- Above 1,700 m· Mattina
- 2 · Moderato
- Below 1,700 m· Mattina
- 1 · Debole
- Above 1,700 m· Pomeriggio
- 2 · Moderato
- Below 1,700 m· Pomeriggio
- 1 · Debole
Non aggiornato — questo bollettino è scaduto last year. Stai vedendo condizioni passate, non il bollettino in corso.
In sintesi
Due to warming, the main avalanche problem is WET SNOW.
Problemi valanghivi
Wet snow· Pomeriggio
NNEESESSWWNW- Above 1,700 m
- Dimensione
- 2
Stability: very poor · Frequency: few
Avalanche Activity
Due to warming, the main avalanche problem is WET SNOW.
Moderate avalanche danger in the high altitudes of the High, Western and Low Tatras, 2nd degree. Positive temperatures during the day cause the snow cover to lose stability. In the morning on the eastern slopes and in the afternoon on the western slopes. Small to moderate spontaneous avalanches from wet snow may occur on steep slopes with sufficient snow. At high altitudes, in couloirs, under saddles and rock faces, very occasionally on shady northern slopes, there are still snow slabs and pillows which can release an avalanche with a large additional load.
Snowpack Structure
The snow cover is very heterogeneous due to variable precipitation, which is snow only at altitudes above 1800-2000 m above sea level. Below this threshold the snow is moist to wet, above it new snow is slightly increasing. Overall, however, only 5 to 10 cm. At high altitudes (above 2000 m), snow slabs and pillows of varying hardness continue to occur. At altitudes below 1500 m, there is only patchy snow cover.
Tendency
no significant change pk
Bulletin data: Stredisko lavínovej prevencie HZS (via EAWS / avalanche.report)