Bollettino valanghe

Západné Tatry

HZS
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Pericolo valanghe

Above 1,700 m
2 · Moderato
Below 1,700 m
1 · Debole
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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

    • Above 1,700 m
    Dimensione
    2

    Stability: very poor · Frequency: few

  • Wind slab

    • Above 2,000 m
    Dimensione
    2

    Stability: 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. Cold temperatures and rain cause the snow cover to lose stability. On steep slopes with sufficient snow, small to medium-sized spontaneous avalanches from wet snow may occur. At high altitudes, on slopes, in couloirs, under saddles and rock faces, there are 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)

Regioni coperte