Sky was consistently OVC, with one or two very brief sun breaks in the afternoon. Snow was at S1 in the morning dropping to S-1 after 13:00. Winds were mostly calm in the BTL and NTL zones where we travelled, with light gusts out of the NW. We did not observe any wind transport ATL in terrain that we could see.
3-4 old, D1 wet loose slides likely occurring during the warming event on 2/12 observed.
On a similar aspect and elevation to the slide that occurred on nearby Shoulda Coulda Woulda on 2/11, we found that with hard force the snowpack broke on same layer of weak snow above the MLK Crust(CT26 RP, down 91cm). While these rounding facets were on the smaller side (1cm layer of .75mm facets), they still produced a result. This means that while the snowpack is "healing", there are still weaknesses that in the right terrain — shallow spots with weak points, near rocks for example — could still be triggered to create a large slide, while unlikely.
We also got a break in the snowpack on the 2/12 crust (CT17 BRK, down 33cm) which can tell us that that new snow in the past few days is bonding moderately well to the old snow surface.
Problem | Location | Distribution | Sensitivity | Size | Comments |
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Persistent Slab |
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Weak Layer(s):
Jan 15, 2023 (MFcr)
Comments: Small facets exist above the MLK crust that are could create a slide surface for the upper snowpack. This layer is getting deeper and deeper into the snowpack, and getting hard to trigger, however it could still be possible to trigger in shallow spots with weak points, like in rocky terrain. |
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Wind Slab |
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Comments: While we did not see any new wind slab formation given the inputs today, there was evidence of past wind loading mostly ATL, on leeward sides of ridges. |