Avalanche danger can rise quickly with afternoon warming and solar radiation. Be aware of changing conditions and overhead hazards.For more insight into spring danger ratings, check out this Blog Post.
Avalanche problems
Storm Slabs
N
NE
E
SE
S
SW
W
NW
Alpine
Treeline
Below treeline
Likelihood
Possible - Likely
Size
1–4
Recent storm snow may have formed storm slabs in some areas. Strong SW winds have formed stiffer wind slabs in leeward features.
Loose Wet
N
NE
E
SE
S
SW
W
NW
Alpine
Treeline
Below treeline
Likelihood
Unlikely - Possible
Size
1–2
Loose wet activity can be expected from steep features during periods of solar warming or rain. Isolated wet slabs may be possible under the same conditions where the recent storm snow is poorly bonded to the underlying crust.
Deep Persistent Slabs
N
NE
E
SE
S
SW
W
NW
Alpine
Treeline
Below treeline
Likelihood
Unlikely
Size
3–7
A deeply buried persistent weak layer still has the potential to produce very large avalanches and could be triggered by heavy triggers such as cornice falls or smaller avalanches stepping-down.
Confidence
Poor - Due to the number of field observations
Weather Forecast
Light precipitation is expected to continue on Monday. Light scattered precipitation with periods of sun is likely on Tuesday. Dry, sunny conditions are expected for Wednesday. Sun. Night/Monday: Precipitation 6-10mm, freezing level am: 800m pm: 1200m, ridgetop wind: moderate-strong STuesday: Cloudy with sunny breaks, scattered precipitation 1-3mm, freezing level am: 700m pm: 1100-1300m, ridgetop wind: light variableWednesday: Mostly sunny, convective flurries possible, freezing level am: 900m pm: 1400m, ridgetop wind: light variable
Avalanche Summary
Reports from Friday of sluffing from steep sun exposed terrain features and isolated slabs releasing from leeward features on ridgecrests. We are no longer receiving professional daily reports for the region so public observations are really appreciated right now. If you are out in the mountains, send your observations to [email protected]
Snowpack Summary
Highly variable spring conditions are being reported in the region. At lower below-treeline elevations the snowpack is typically wet and isothermal. It has not been refreezing overnight and is melting quickly. Between roughly 1000 and 1500m, the snowpack is undergoing daily melt-freeze cycles. The same conditions can be expected on sun-exposed slopes all the way to mountain-top. On higher elevation north-facing slopes, dry snow can be found. Recent strong S through W winds have scoured windward slopes and created wind slabs in leeward slopes. The early February crust/facet layer is typically down 1.5 to 2.5m. A smaller avalanche or a cornice fall may still have the potential to step down to this layer causing very large, destructive avalanches.