Lawinenlagebericht

Middle Lys Valley

Regione Valle d'Aosta
Auf der Karte ansehen

Lawinengefahr

All elevations· Vormittag
2 · Mässig
All elevations· Nachmittag
3 · Erheblich
Veraltet — dieser Lagebericht ist 5 months ago abgelaufen. Du siehst vergangene Verhältnisse, nicht den aktuellen Bericht.

Kernpunkte

The weather will be warm. Moist and wet avalanches as the day progresses.

Lawinenprobleme

  • Wet snow· Vormittag

    • Alle Höhenlagen
    Größe
    2

    Stability: very poor · Frequency: few

  • Wet snow· Vormittag

    • Below 2,500 m
    Größe
    1

    Stability: very poor · Frequency: some

  • Wet snow· Nachmittag

    • Alle Höhenlagen
    Größe
    2

    Stability: very poor · Frequency: some

  • Wet snow· Nachmittag

    • Below 2,800 m
    Größe
    3

    Stability: very poor · Frequency: few

Avalanche Activity

The weather will be warm. Moist and wet avalanches as the day progresses.

Even at night, temperatures were positive above 3000 m. In particular above approximately 2500 m: A clear night will be followed in the early morning by sometimes favourable conditions, but the danger of wet and gliding avalanches will increase later. As a consequence of warming and solar radiation, the natural activity of medium moist and wet avalanches will rapidly increase, in particular on very steep sunny slopes. This also applies at the base of rock walls, including on very steep shady slopes at intermediate altitudes. Especially on extremely steep slopes avalanches can release the wet old snow as well and reach large size in isolated cases. Backcountry tours and off-piste skiing should be started and concluded very early.

Snowpack Structure

The surface of the snowpack will freeze to form a strong crust only at high altitudes and will soften quickly. In the last few days the natural activity of medium wet and gliding avalanches has gradually increased. At higher altitudes, snow cover becomes thinner and patchy; it is better at mid-altitudes, which are less exposed to the wind. The surface snowpack changes rapidly depending on the aspect and gradient: crusts of various types and thicknesses alternate. In steep terrain there is a danger of falling on the hard crust, especially adjacent to ridgelines and in pass areas. Weak layers exist in the snowpack in particular on steep shady slopes. As a consequence of mild temperatures and solar radiation the snowpack settled. These spring-like weather conditions will give rise to increasing consolidation of the snowpack. Below approximately 1800 m hardly any snow is lying.

Tendency

The danger of moist and wet avalanches will persist.

Bulletin data: Regione Autonoma Valle d'Aosta (via EAWS / avalanche.report)

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