Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Regions
South Coast.
Recent winds have developed pockets of windslab at higher elevations.
Confidence
Poor - Due to the number and quality of field observations
Weather Forecast
Clearing overnight with no precipitation. Clear on Tuesday with light Southwest winds and alpine temperatures around -12. Clear on Wednesday with a chance of a temperature inversion bringing near freezing temperatures to the alpine with light winds. Valleys should remain around -10.
Avalanche Summary
No new reports of avalanches. Please let us know what you're seeing out there at [email protected].
Snowpack Summary
There are few actual observations from the region to start the season. This is based mostly off weather station data and the weather forecast. Most areas experienced heavy rain last week up to 2000 m, or even higher. Higher elevations may have continued to see wet snow accumulate, and possibly a lot of it. Rapid cooling early on Friday has probably left a new rain crust near the surface, but in some areas it's already buried by 10-15 cm of light snow. A weak layer of facetted snow on a crust may be lurking deeper in the snowpack. However, it's possible this weakness was 'flushed' out with the recent heavy precipitation. There's limited recent info on this weakness so I recommend digging to confirm the existence of the layer, its depth, and to test its strength.
Problems
Wind Slabs
Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind slabs that form over a persistent weak layer (surface hoar, depth hoar, or near-surface facets) may be termed Persistent Slabs or may develop into Persistent Slabs.