Bollettino valanghe

Purcells

Apr 26 – 27, 2019Avalanche Canada
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Archiviato · scaduto 7 years ago

Pericolo valanghe

Sun
Mon
Alta quota
3 · Marcato
Limite del bosco
3 · Marcato
Sotto il limite
2 · Moderato

In sintesi

Last Avalanche Forecast for the season. For additional information check out our Spring Conditions page at: https://goo.gl/cpx8Dq

New snow and moderate winds from a variety of directions may form touchy wind slabs reactive to human triggers.

Problemi valanghivi

  • Wind Slabs

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

    New snow and moderate winds from a variety of directions may form touchy wind slabs reactive to human triggers; especially in the northern part of the region where more snow is expected.

  • Loose Wet

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

    Any appearance of the strong April sun can initiate a loose wet avalanche cycle. The likelihood of loose wet avalanches increases as temperatures warm through the day and/or if the sun comes out for a prolonged period of time.

Confidence

Low - Forecast snowfall amounts are uncertain

Weather Forecast

FRIDAY NIGHT: Snow in northern part of the region; 5-10 cm. / Moderate, westerly winds / Alpine low -6 C / Freezing level 1400 m.

SATURDAY: Snow (more in the north); 5-15 cm. / Light, westerly winds / Alpine high -5 C / Freezing level 1500 m.

SUNDAY: Sunny / Moderate, northeasterly winds / Alpine high -4 C / Freezing level 1600 m.

MONDAY: Mix of sun and cloud / Light, westerly winds / Alpine high -4 C / Freezing level 1600 m.

Avalanche Summary

On Thursday, several naturally triggered size 2 wind slabs were reported on a variety of aspects in the alpine. There are currently very few professional observers submitting daily observations. Please submit your observations to the MIN. Photos of avalanches or current conditions are particularly useful.

Snowpack Summary

A supportive surface crust caps a mostly isothermal snowpack at lower elevations. In the alpine, the recent snow is likely settling and preserved as cold, wintery, snow on north aspects where reactive wind slabs may still linger. A crust is present on all solar alpine aspects to mountain tops and below 2200 m on all aspects. The strength of the crust will depend on overnight freeze and the speed at which the snowpack warms up during the day.

Weak and sugary faceted grains may remain at the bottom of the snowpack in the alpine, producing a low likelihood but high consequence scenario. Steep, rocky areas with a shallow or highly variable snowpack depth are the most likely places to trigger this layer.

Below treeline, snow is disappearing rapidly.

Regioni coperte