Lawinenlagebericht

Northwest Inland

Apr 23 – 26, 2021Avalanche Canada
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Archiviert · abgelaufen 5 years ago

Lawinengefahr

Sun
Mon
Hochgebirge
1 · Gering
Waldgrenze
1 · Gering
Unterhalb
1 · Gering

Kernpunkte

Final forecast for the season! Stay alert to changing conditions during the heat of the day and adjust your travel plans accordingly. Back off slopes if the surface becomes moist or wet with daytime warming. 

Lawinenprobleme

  • Loose Wet

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Unlikely - Possible
    Größe
    1–1.5

     Wet loose avalanches become increasingly likely during the heat of the day.  

Confidence

High -

Weather Forecast

  

FRIDAY NIGHT: Few clouds / Light, northeast ridgetop wind / alpine low temperature -8 / Freezing level 700 m.

SATURDAY: Sunny / Light, northeast ridgetop wind / alpine high temperature 3 / Freezing level 1500 m.

SUNDAY: Sunny / Light, northeast ridgetop wind / alpine high temperature 4 / Freezing level 1700 m.

MONDAY: Sunny / Moderate, northwest ridgetop wind / alpine high temperature 4 / Freezing level 1700 m.

Avalanche Summary

No new avalanches were reported in this region on Thursday.

NOTE: Observations are very limited during this time of year.

Snowpack Summary

The snowpack has been undergoing a melt-freeze cycle with successive days of warm sunny weather. Strong solar radiation and warming can initiate wet loose avalanches as the snow loses cohesion. Cornices are large and looming along ridgelines. Sun and warm temperatures can increase the chances of cornice failures, especially when temperatures remain above zero overnight. Check out the Forecaster's Blog for information on how to manage these spring conditions. 

The snowpack is overall strong and settled in most areas, however, sustained warming can increase the likelihood of large avalanches failing on deeply buried weak layers. This is most likely to occur on steep, rocky alpine slopes with a shallow or thin to thick snowpack.

Terrain and Travel

  • As surface loses cohesion due to melting, loose wet avalanches become common in steeper terrain.
  • Back off slopes as the surface becomes moist or wet with rising temperatures.

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