Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–1.5
Wind slabs will be most likely be isolated to immediate lees of ridgecrests and roll-overs in wind exposed alpine terrain.
Minimize exposure to large looming cornices weakening with daytime warming and solar radiation. Cornice fall could trigger a slab on the slope below.
Isolated pockets of wind slab may be found in immediate leeward features in the alpine.
Wind slabs will be most likely be isolated to immediate lees of ridgecrests and roll-overs in wind exposed alpine terrain.
Cornices become weak with daytime warming. Cornice falls are dangerous in their own right and they can also trigger slabs on slopes below. Their large mass can trigger deeper slabs on buried crusts in the upper snowpack that a single rider wouldn't trigger on their own.
Wet loose avalanches may occur on steep solar aspects and at elevations where air temperature rises above freezing. Below treeline, loose wet avalanches are possible where snow did not refreeze overnight.
Tuesday Night: Clear. Ridgetop wind light to moderate from the South and freezing levels 1200 m.
Wednesday: Mix of sun and cloud with light snow 5 cm. Ridgetop wind moderate from the southwest. Alpine temperatures near -4 and freezing levels 1700 m.
Thursday: Mix of sun and cloud with flurries. Ridgetop wind moderate from the West. Alpine temperatures near -7 and freezing levels 1400 m.
Friday: Cloudy. Ridgetop wind moderate to strong from the South. Alpine temperatures near -5 and freezing levels 1600 m.
On Tuesday, wet loose pinwheels were reported from steep solar aspects.
On Monday, several wet loose natural avalanches were reported up to size 2 on solar slopes. Cornices have been reactive in the last few days both to explosives and naturally, occasionally triggering wind slabs on slopes below.
The weather pattern is spring-like and fairly benign. Get after it early before daytime warming kicks in and solar radiation weakens the snowpack and cornices.
Remember to stay well back from ridgetops that might be corniced and to avoid slopes with overhead cornice exposure especially under the current conditions where recent rapid growth and daytime warming has made them large and fragile.
The convective nature of Sunday's storm resulted in greatly variable snowfall amounts through the region, as much as 50 cm around Golden and 5-20 cm elsewhere. The recent snow was accompanied by strong southwest wind and may have formed isolated pockets of wind slab on leeward slopes at upper elevations. Reports indicate that the new snow is bonding well to underlying surfaces which include wind-affected snow in the alpine or crust on solar aspects and below 1900 m. Below this elevation and on solar aspects the new snow dusts crusty surfaces down to 1500 m. Below 1500 m, the moist snowpack is quickly diminishing.
A widespread crust layer from the mid-March warm spell can be found 30-60 cm deep, and a small surface hoar and facets have been observed at this depth on some isolated north-facing slopes. Reports suggest the snow is generally well bonded to these layers but isolated instances of large solar-triggered slab avalanches running on the crust have been observed. Deeper layers are strong and have been unreactive over the past few weeks.