Northwest Avalanche Center

Observation: Public

All Observations

Observation Details

Name:
Drew Lovell
Observation Date:
January 27, 2021
Submitted:
January 27, 2021
Zone or Region:
East North
Activity:
Skiing/Snowboarding
Location:
Lower Methow Valley

Observed Avalanches

Did you observe any avalanches? 
Yes
Avalanche Type:
Dry Loose (Sluff)
Size:
Size 1: Relatively harmless to people
Elevation:
7000'
Aspect:
SW
Comments:
See photo. Brief breaks of sunshine triggered minor Dry Loose activity on steep features, particularly where previous solar crusts exist. Small, but running fast and far on specific slopes and easily triggered with ski cuts.

Signs of Unstable Snow

Did you see shooting cracks? 
Yes, Isolated
Did you experience collapsing or whumpfing? 
Yes, Isolated

Observations

Our crew traveled northerly slopes between roughly 3000'-7000' today. The melt-freeze crust ( a remnant of the Jan.12-13 warm event) is weak and faceted, but supportable to skis. It offers fast, efficient travel, with the 15-20cm recent snowfall. Above approx. 5500', the series of light snowfalls since about Jan.20 have settled and bonded to the crust, and skiing becomes softer and deeper.
Isolated collapses were noted beneath the weight of a skier (see photo), within a specific elevation band around 5000', likely due to failure of faceted grains beneath the crust. No avalanches were triggered with this scenario, in spite of ski cuts on very steep, unsupported slopes below treeline. More interesting than alarming at present, but something to monitor, as incremental snowfalls continue to build slab structure Below Treeline.
This potentially- poor Below Treeline structure trends favorably away with elevation.
A profile at 6500' on a N aspect showed the following:
A total snow depth of 215cm. The Jan.12 crust (1cm thick, weak) down 45cm with a favorable bond to overlying snow.
Most recent storm snow 15-20cm (F hard) with a fair bond over 1mm near-surface facets and decomposing fragments (F+ to 4F hard)
The mid- and lower- snowpacks trend from 1F hard to P hard and present no concerns.
Overall, the snowpack Near and Above Treeline is strong, but the bond over previously scoured or wind-pressed surfaces should be monitored.
Dry Loose avalanches have potential to entrain, and run fast and far.

Media

Shallow, low-density dry loose activity, on a SW aspect observed at about 7000'.  Small, but running fast and far on a solar crust on steep terrain.
15-20cm low-density storm snow now overlies a melt-freeze crust from Jan.13, most-evident below about 5500' in the watershed.  The storm snow failed as a very low-cohesion slab in isolated areas below treeline, where facets have formed beneath the weak crust.  We experienced isolated collapses in these areas, but no avalanches occurred, likely due to the very low-density storm snow at present.  Incremental accumulations favoring east slope areas could slowly build more-legitimate slab structure over crusts and facets, potentially becoming reactive on steep, open terrain below treeline.
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