Boletín de aludes

Waterton Lakes

Apr 4 – 5, 2013Parks Canada
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Archivado · caducó 13 years ago

Peligro de aludes

Fri
Sat
Alta montaña
Sin grado
Límite del bosque
Sin grado
Bajo el límite
Sin grado
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Lo esencial

This is the end of our regular forecast season. Avalanche hazard will persist. Hazard will be higher with heating from rain or sun and will be lowest during cool periods. Spring storms may also bring a return to winter at upper elevations.

Problemas de aludes

  • Cornices

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    1–3
    With warm temperatures, solar heating, or rain to upper elevations cornice failures will occur. These are large triggers and have the potential to create larger avalanches. Minimize your exposure especially during rapid warming.

  • Loose Wet

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Likely
    Tamaño
    1–2
    Depending upon the inputs of heat from rain or sun this activity can be expected everywhere. Travelers must carefully monitor surface conditions and be clear of slopes before crusts break. Use extra caution if there is moist snow over buried crusts.

  • Wet Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Unlikely - Possible
    Tamaño
    1–2
    Shallow snowpack areas hold weak mid and lower layers. These areas will be more susceptible to failure with heating but have failed with large loads (such as cornices or loose avalanches) acting as the trigger.

Weather Forecast

None provided for the extended period however visitors may call Waterton Lakes National  Park Reception on weekdays at 403 859 2224 for more detailed information. Generally: watch freezing levels closely to determine where heating and weakening of the snowpack is likely by the sun and rain. If more snow arrives watch the bond to the surface crusts.

Snowpack Summary

A surface crust exists on all aspects and at all elevations. The strength of this crust varies with location as it freezes with cooling and weakens with heating. In thin snowpack areas weak layers persist that were created by earlier faceting of mid and basal snow. Weak moist snow may fail as point releases or as slabs over crusts or weak layers.

Avalanche Summary

With strong solar inputs a daily cycle of superficial LOOSE WET AVALANCHES spread to affect all elevations and aspects earlier this week.  This same heating also caused many CORNICE FAILURES. A few notable slabs were triggered by cornice failures (large loads) in THIN SNOWPACK AREAS where weak snow has developed in the mid and lower snowpack.

Confidence

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