Avalances.sk

Friday 17.11.2023

Published 16 11 2023, 17:00


Danger level

1700m
Avalanche Problem
Wind slab
1700m
Wind slab
1700m


Beware of wind-blown snow in the form of snow pillows and slabs!

From 1700 m.n.m in the High, Western and Low Tatras persists 2nd degree of avalanche danger. New snow is transported by strong winds on layers of older snow, with which it is not sufficiently bound. Dangerous pillows and slabs are formed, especially on the leeward sides of ridges under rock walls and in narrow couloirs. Their release is particularly possible with high additional loads on steep to very steep slopes (more than 35°). The avalanche danger increases with altitude. At altitudes above 1700 m there is more snow and therefore medium-sized avalanches can occur.

Snowpack

dp.4: cold following warm / warm following cold

During the last snowfall, 10-25 cm fell on the mountains. In total, the snow depth reaches up to 50 cm in places. As it is only the beginning of the season, there are mostly only 2 layers of snow in the snow cover, but they are not well interconnected. The new snow is unevenly distributed due to strong winds and deposited in terrain depressions and on the leeward sides of ridges. A continuous layer of snow cover can be found from about 1500 m above sea level.

Tendency

During the day, the avalanche situation will worsen due to strong winds and expected snowfall.


Danger level


Avalanche Problem
Wind slab


Watch out for wind-blown snow (snow slabs and pillows).

A small amount of new snow is blown by strong winds over layers of older snow. Dangerous pillows and slabs are formed. Avalanches are especially possible under heavy loads and on steep to very steep slopes. The avalanche danger increases with altitude. Only small avalanches may occur in isolated places.

Snowpack

dp.4: cold following warm / warm following cold

Due to the overall low amount of snow, the snowpack is stable.

Tendency

During the day, the avalanche situation will worsen due to strong winds and expected snowfall.