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RegisterDec 24th, 2019–Dec 25th, 2019
South Columbia.
Avalanche activity has slowed over the last 48 hours, but the recent cycle was so large and destructive that conservative terrain selection remains prudent. It's nearly impossible to trust a snowpack that has recently produced size 3.5 avalanches.
We’re entering a rather quiet weather period with coolish temps and no significant snowfall expected, at least through boxing day. The region should see winds pick up later in the week and there is potential for a small shot of snow Thursday night.
CHRISTMAS EVE: Freezing level at valley bottom, light variable wind, no significant precipitation expected.
CHRISTMAS: Scattered cloud cover, freezing level near valley bottom, light northwest wind, no significant precipitation expected.
BOXING DAY: Scattered cloud cover in the morning building to overcast by sundown, freezing level at valley bottom, moderate to strong south/southwest wind, trace of snow possible during the day, potential for 5 to 10 cm by Friday morning.
FRIDAY: Broken cloud cover, freezing level at valley bottom, moderate to strong west/southwest wind, trace of snow possible during the day.
The recent storm was a significant one, and there is a great deal of uncertainty at this time as to how quickly the snowpack will gain strength. Avalanche occurrences are beginning to taper, but recent avalanches have been very large. Patience and conservative terrain selection is the name of the game right now.
Avalanche activity on Monday was sharply reduced from the previous days, but there was still a size 2.5 avalanche triggered by a snowcat on a NE facing slope at 2500 m. A small skier controlled avalanche was also reported from a northeast facing slope at 2300 m.
Between Thursday and Sunday there were numerous reports of natural, human and explosive triggered avalanches up to size 3.5. Many of these were triggered remotely.
The South Columbias have seen 60-100 cm of new snow since Thursday night. Storm slabs are likely widespread and may be reactive to human triggering.
There is anywhere from 100-160 cm of snow on top of a widespread layer of large, feathery surface hoar crystals. This layer is suspected to have been responsible for numerous recent avalanches and it may continue to be reactive to human triggers.
A weak layer that formed in late November is now over 160 cm deep. This is the layer of concern relating to the listed persistent slab avalanche problem. The weak layer may present as surface hoar, a crust, facets or a combination, depending on elevation and aspect.