Bollettino valanghe

Purcells

Mar 21 – 22, 2024Avalanche Canada
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Archiviato · scaduto 3 years ago

Pericolo valanghe

Sat
Sun
Alta quota
2 · Moderato
Limite del bosco
2 · Moderato
Sotto il limite
2 · Moderato

In sintesi

Cooling temperatures are reducing the likelihood of triggering large persistent slab avalanches.

Avoid steep or convex terrain features with a shallow or thin-to-thick snowpack.

Problemi valanghivi

  • Persistent Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    2–3.5

    A crust with weak facets above is down 40 to 110 cm. Steep or convex terrain features with a shallow or thin to thick snowpack at treeline and above are the most likely places to trigger this layer.

Confidence

Moderate

Avalanche Summary

Naturally triggered wet loose avalanches up to size 2.5 were reported on sunny aspects at all elevations on Wednesday.

Snowpack Summary

0 to 5 cm of new snow overlies predominantly crusty surfaces.

A widespread, hard crust down 40 - 110 cm with weak facets above continues to be the primary layer of concern for human triggering of very large persistent slab avalanches.

The bottom of the snowpack is generally weak and faceted, with the potential to produce very large avalanches. The most likely areas to trigger this deeply buried weak layer are steep, rocky areas in the alpine with a shallow or thin to thick snowpack.

Weather Summary

Thursday night

Mostly cloudy. 10 to 20 km/h west ridgetop wind. Treeline temperature -7 °C. Freezing level valley bottom.

Friday

Mix of sun and cloud. 10 to 20 km/h west ridgetop wind. Treeline temperature -4 °C. Freezing level 1600 m.

Saturday

Cloudy. 10 to 20 km/h southeast ridgetop wind. Treeline temperature -5 °C. Freezing level 1300 m.

Sunday

Mostly cloudy. 10 to 20 km/h east ridgetop wind. Treeline temperature -9 °C. Freezing level 900 m.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Avoid steep, rocky, and wind effected areas where triggering slabs is more likely.
  • When a thick, melt-freeze surface crust is present, avalanche activity is unlikely.
  • Conditions may have improved, but be mindful that deep instabilities are still present.
  • Cornice failure may trigger large avalanches.

Regioni coperte