Bollettino valanghe

Kananaskis

Mar 14 – 15, 2018Alberta Parks
Vedi sulla mappa
Archiviato · scaduto 9 years ago

Pericolo valanghe

Fri
Sat
Alta quota
2 · Moderato
Limite del bosco
2 · Moderato
Sotto il limite
1 · Debole
Apri la mappa completa

In sintesi

New snow is coming tomorrow. Expect great skiing if we get the forecasted amounts.

Problemi valanghivi

  • Wind Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    1–2
    These will be fresh windslabs formed from gusting winds. They may slide easily if sitting on a crust.

  • Loose Dry

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Likely
    Dimensione
    1–1.5
    This will be more of an issue in areas that has a frozen crust underneath. They could run far and fast.

  • Storm Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible - Likely
    Dimensione
    1–2
    As the storm starts, the new snow will bond quickly as the remaining heat escapes from the snowpack. The air temp will also play a role especially if it snows before it cools off completely.

Confidence

High -

Weather Forecast

We're expecting a storm to roll through tonight with snow starting by early morning. Overnight lows will fall to -6, and by tomorrow, they'll fall further to -10 at treeline. The first pulse of this storm will bring us 21cm of snow by late day tomorrow. Another pulse will follow on saturday, but it will only leave 5cm. The winds will spike early on in the storm and max out at 45km/hr.

Avalanche Summary

A couple of small, cornice triggered loose wet avalanches were noted today. Their exact age is unknown, but suspected in the last 36 hours.

Snowpack Summary

Freezing levels went very high today. One of the radio repeater sites recorded a temp of +4 by mid afternoon. Only high, true north aspects are escaping the heat and moist snow. Expect a widespread crust pretty much everywhere. It will be more pronounced at low elevations and/or solar aspects. The freeze thaw cycle is helping the upper snowpack consolidate and become stronger. The deeper layers are deep enough that they'll remain unchanged from the warming cycle. Cornices and wind lips have been collapsing lately as well.

Regioni coperte