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RegisterJan 11th, 2020–Jan 12th, 2020
Lizard-Flathead.
Reports suggest our low density snow is settling and bonding rapidly, with instability focused in wind affected areas. A steady supply of new snow and wind suggests more of the same for Sunday. Be prepared to dial back your terrain selection if snowfall exceeds forecast amounts.
Saturday: Cloudy with continuing flurries bringing 15-20 cm of low density new snow. Moderate southwest winds.
Sunday: Cloudy with continuing scattered flurries bringing 10-15 cm of new snow, increasing overnight. Light to moderate south winds. Alpine temperatures falling to about -15.
Monday: Mainly cloudy with easing flurries bringing about 5 cm of new snow, continuing overnight. Light to moderate southwest winds. Alpine high temperatures to about -17.
Tuesday: Cloudy with continuing flurries bringing 5-10 cm of new snow. Light to moderate southwest winds. Alpine temperatures around -18
Reports of avalanche activity over the week have been steady, with each substantial snowfall accompanied by observations of natural, skier triggered, and explosives controlled storm slabs generally reaching size 2 (large) with a few examples up to size 3 (very large). North to east aspects and higher elevations have figured most prominently in reports as a result of recent winds.
Notably, two larger recent results involved the weak basal snowpack by either stepping down to this layer or failing on its reloaded surface.
Looking forward, a continuing supply of low density snow and elevated winds are expected to maintain active avalanche conditions. Avalanche danger is expected to continue to be focused in exposed areas where wind redistributes new snow into deeper and more reactive slabs.
Another 30-40 cm of low density new snow fell in the region over Friday night, bringing storm snow totals from last week to 70-110 cm.
This recent snow is reportedly settling rapidly, with surface instabilities generally limited to the most recent accumulations, especially where winds have redistributed snow into reactive slabs in leeward features.
Several crusts layers exist in the mid to upper snowpack as a result of recent warming and rain events. These have not been identified as bed surfaces or failure planes in recent avalanche activity.
The bottom 10-20 cm of the snowpack consists of faceted snow and decomposing crusts. Although inherently weak, this basal layer has not been an active avalanche problem in our region for several weeks.