Bollettino valanghe

Kootenay Boundary

Mar 26 – 27, 2017Avalanche Canada
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Archiviato · scaduto 10 years ago

Pericolo valanghe

Tue
Wed
Alta quota
3 · Marcato
Limite del bosco
2 · Moderato
Sotto il limite
1 · Debole

In sintesi

Keep your terrain selection in sync with the bonding of the recent storm snow. Remember that this bond is likely to vary with elevation and aspect.

Problemi valanghivi

  • Storm Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible - Likely
    Dimensione
    1–2
    Recent bouts of snowfall combined with moderate southwest winds to form storm slabs that may remain reactive to human triggering on Monday. This problem will be especially pronounced in the alpine and in wind affected areas.

Confidence

High -

Weather Forecast

Sunday night: Scattered flurries bringing approximately 5 cm of new snow. Light to moderate south winds.Monday: Mainly cloudy with isolated flurries and a trace of new snow. Light southwest winds. Freezing level to 1700 metres with alpine temperatures around -2Tuesday: Mainly cloudy with isolated flurries and a trace of new snow. Light to moderate southwest winds. Freezing level to 1600 metres with alpine temperatures around -3.Wednesday: Cloudy with flurries bringing approximately 10 cm of new snow. Moderate to strong southeast winds. Freezing level to 1600 metres with alpine temperatures around -2.

Avalanche Summary

Reports from Saturday showed storm slabs releasing from Size 1-2 with ski cutting and explosives control. One natural Size 1.5 slab was observed on a steep northeast slope. Crown fractures generally ranged from 10-40 cm. Natural loose wet avalanches were noted reaching to Size 1.5 in the Kootenay Pass area.

Snowpack Summary

Stormy weather over the past week brought roughly 40-50 cm of snow to the region. Periodic high freezing levels and solar exposure over the same period formed a series of crusts (March 19-24) that exist within this upper snowpack at lower elevations and on solar aspects. The new snow and series of crusts lie over a more widespread (March 14) rain crust that exists at all elevations. Moist or wet snow exists below this rain crust. The late-February facet / surface hoar interface (90-140 cm deep), the mid-February crust (110-150 cm deep), and basal facets in shallow snowpack areas may still be present at upper elevations. Overlying crusts have been noted acting as a bridge over these layers and any remaining reactivity is likely limited to high alpine locations.

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