Bollettino valanghe

South Columbia

Apr 18 – 19, 2017Avalanche Canada
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Archiviato · scaduto 9 years ago

Pericolo valanghe

Thu
Fri
Alta quota
2 · Moderato
Limite del bosco
2 · Moderato
Sotto il limite
1 · Debole

In sintesi

Convective flurries and moderate southerly winds may create new wind slabs in lee features below ridge tops.

Problemi valanghivi

  • Wind Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    1–2
    Convective flurries and moderate southwesterly winds may create small wind slabs in the lee of terrain features.
  • Cornices

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Unlikely - Possible
    Dimensione
    2–4
    The likelihood of cornices triggering increases with intense sunshine and/or during the warmest parts of the day.

Confidence

Moderate - Due to the number of field observations

Weather Forecast

WEDNESDAY: Cloudy with sunny periods / Moderate southwest wind / Alpine temperature -3 / Freezing level 1900mTHURSDAY: Cloudy with sunny periods and isolated flurries/ Light west wind / Alpine temperature -2 / Freezing level 2000 mFRIDAY: Cloudy with sunny periods / Light northwest wind / Alpine temperature -4 / Freezing level 1800mNOTE: Convective flurries which are common during this time of year can result in widely varying snowfall amounts throughout a region. These spring squalls routinely drop 20+ cm of snow in one valley while the adjacent drainage remains dry. For this reason, the distribution of avalanche problems associated with new snow, such as wind slabs, can vary greatly within a region.

Avalanche Summary

Several size 1 skier triggered wind slabs were reported on northeast aspects in this region on Sunday. Exposure to large overhanging cornices remains a significant concern.

Snowpack Summary

Recent new snow tree line and above has been redistributed by west and south winds. The middle of the snowpack is generally well settled and continues to transition into a spring melt/freeze regime except for high elevation northerly aspects. Expect the entire thickness of the snowpack to be moist or wet at lower elevations. At upper elevations a deep persistent layer consisting of facets sitting on a crust that was buried back in November has been sporadically reactive to heavy loads i.e. a cornice fall or the weight of a smaller avalanche running. Cornices remain large and continue to become more overhanging.

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