Bollettino valanghe

Kananaskis

Avalanche Canada
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Pericolo valanghe

Sat
Sun
Alta quota
Condizioni primaverili
Limite del bosco
Condizioni primaverili
Sotto il limite
Condizioni primaverili
Non aggiornato — questo bollettino è scaduto 4 months ago. Stai vedendo condizioni passate, non il bollettino in corso.

In sintesi

Spring is here! Early starts and early finishes are important as the Avalanche danger will increase throughout the day as conditions warm up.

Problemi valanghivi

  • Persistent Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    1.5–2.5

    Repeated warming/cooling cycles are helping stabilize these layers. Continue to watch steep polar aspects where the warming cycles are fewer and less intense.

  • Loose Wet

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Likely
    Dimensione
    1–2

    This problem will become more likely throughout the day as temperatures warm up.

Confidence

Avalanche Summary

A few loose wet avalanche's from steep solar aspects. No new slab avalanche activity.

Snowpack Summary

Crusts are the prominent layers in our changing snowpack. Thick, supportive surface crusts are up to 2500m on most aspects except true polar. Even polar aspects have crusts up to about 2200m. Beneath that are various other crusts that are helping hold it all together. With that said, the Mar 24 layer/interface is still evident and a potential failure plain on steep, high north country. Don't rule it out just yet.

Be sure to check the quality of the freeze overnight before you go! Stability will change throughout the day as the conditions warm up.

Weather Summary

Spring is here it feels like! Friday will be a beautiful day with a freezing level around 2600m, light winds, and clear skies.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Be alert to conditions that change with elevation and sun exposure.
  • Avoid steep, sun-exposed slopes when the air temperature is warm or when solar radiation is strong.
  • Avalanche activity is unlikely when a thick melt-freeze crust is present on the snow surface.

Regioni coperte