Today was a real "storm in progress" day - a good day to avoid all avalanche terrain. By 5:30 PM, there was 12-18" (30-45cm) of new snow being blown around by gusty W winds. Isolated wind slabs existed in middle elevation terrain. Snowpack tests produced some unstable results in shady terrain on weak, faceted snow about 2 feet below the surface. The new snow appeared to be bonding fairly well to moist crusts on more southerly aspects. There were some density changes within the new snow that could create failure layers for wind slabs at upper elevations. I left before the earthquake hit.
Snowing S1-5 (half an inch to 2 inches per hour) from 3-5:30 PM. 12-18" (30-45cm) storm snow with drifts to 2 feet thick at middle elevations. Wind was actively transporting snow.
8600' E-NE (see photo): HS=180cm 45cm storm snow, razor crust and FC under that, then series of crusts+FC and mixed forms to subtle dirty FC layer 70cm down: ECTP16, 110cm on dirty FC; ECTN11, 135cm on razor cruts/FC at recent interface; ECTN4, 160cm mid-storm layer.
9000' NW: HS=182cm 37cm storm snow, interfaces and crusts and FC below that were there but not as well developed as in 8600' E-NE pit location: ECTN3, 168cm on mid-storm layer; ECTN12, 145cm on old/new interface FC; ECTN16, 135cm on FC (3/14?); no break or shear on dirty FC layer at 120cm (62cm down from surface)
Problem | Location | Distribution | Sensitivity | Size | Comments |
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Persistent Slab |
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Unknown |
Layer Depth/Date: 60-75cm Comments: The facets that formed in early to mid-March exist here. We'll see if they become a problem like in the western Smoky Mtns (Headwaters, Frenchman Ck, Smiley Ck, Beaver Ck) - I don't trust them for now, guilty until proven innocent. |
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Wind Slab |
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Layer Depth/Date: 40-60cm Comments: Drifts and small slabs were forming in places that typically don't see much wind affect. Wind slabs are likely the primary problem at upper elevations. |
I stayed out of avalanche terrain. The hazard was building while I was out from 3-5:30 PM.