Bollettino valanghe

Eastern Carniche Alps

Protezione Civile FVG
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Pericolo valanghe

Above 1,600 m· Mattina
2 · Moderato
Below 1,600 m· Mattina
1 · Debole
Above 1,600 m· Pomeriggio
3 · Marcato
Below 1,600 m· Pomeriggio
2 · Moderato
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Non aggiornato — questo bollettino è scaduto last year. Stai vedendo condizioni passate, non il bollettino in corso.

In sintesi

As a consequence of warming during the day and solar radiation the avalanche prone locations will become more prevalent as the day progresses. Backcountry tours should be started and concluded early.

Problemi valanghivi

  • Wet snow· Mattina

    • Above 1,600 m
    Dimensione
    2

    Stability: fair · Frequency: some

  • Wind slab· Mattina

    • Above 1,900 m
    Dimensione
    2

    Stability: fair · Frequency: some

  • Wet snow· Pomeriggio

    • Above 1,600 m
    Dimensione
    3

    Stability: poor · Frequency: many

  • Wet snow· Pomeriggio

    • Below 1,600 m
    Dimensione
    2

    Stability: poor · Frequency: some

  • Wind slab· Pomeriggio

    • Above 1,900 m
    Dimensione
    2

    Stability: fair · Frequency: some

Avalanche Activity

As a consequence of warming during the day and solar radiation the avalanche prone locations will become more prevalent as the day progresses. Backcountry tours should be started and concluded early.

As the day progresses as a consequence of warming during the day and solar radiation there will be a gradual increase in the danger of moist and wet avalanches. The avalanche prone locations are to be found in particular at the base of rock walls and behind abrupt changes in the terrain and adjacent to ridgelines and in gullies and bowls. In addition the wind slabs must be taken into account. In particular at intermediate and high altitudes the avalanches can penetrate even deep layers. Gliding avalanches can also occur. The avalanches can be released, even by small loads in isolated cases. In many places there is a danger of falling on the hard snow surface.

Snowpack Structure

The surface of the snowpack will freeze to form a strong crust and will soften during the day. The weather conditions will give rise to thorough wetting of the snowpack. Weak layers exist in the snowpack.

Tendency

Over a wide area strong wind. As a consequence of falling temperatures, the avalanche activity will gradually decrease.

Bulletin data: Protezione Civile Friuli-Venezia Giulia (via EAWS / avalanche.report)

Regioni coperte