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RegisterMar 1st, 2021–Mar 2nd, 2021
Northwest Inland.
Strong southwest wind will howl on Tuesday building fresh wind slabs on northeast slopes. Forecast snowfall amounts vary across the region. If you see more than 25 cm in your riding area bump the avalanche danger up to HIGH and expect to see storm slabs on all aspects.
Monday Night: Snow 10-20 cm amounts vary across the region. Ridgetop wind strong from the southwest and alpine temperatures near -10. Freezing levels valley bottom.
Tuesday: Snow 5-10 cm with some sunny periods. Ridgetop wind strong from the South and alpine temperatures near -6. Freezing levels 900 m.
Wednesday: Snow 5-10 cm. Ridgetop wind mostly light but gusty from the southwest. Alpine temperatures near -4 and freezing levels 900 m.
Thursday: Cloudy with some flurries. Ridgetop wind strong from the southwest. Alpine temperatures near -1 and freezing levels 1100 m.
No new reports on Monday.
On Sunday, a few natural wind slab avalanches were reported up to size 2 at treeline and in the alpine on northeast and northwest aspects. Wind slabs were also easily triggered on leeward slopes by the weight of a skier. Numerous loose wet avalanches were observed from steep terrain features.
On Saturday, we received some fantastic MIN reports showing significant wind effect and wind loading at upper elevations. Natural avalanches were reported as well as a skier-triggered slab size 1.5.
Thank you for the MIN reports!!
Reactive wind and storm slabs are the primary concerns for the forecast period. Loose-dry sluffing will likely be seen from steep terrain features.
Up to 25 cm of recent snow fell by Monday morning. Fresh winds slabs may be reactive on leeward slopes, while touchy storm slabs may be found in isolated wind-sheltered locations. This brings 50 to 80 cm of snow on a variety of old snow surfaces consisting of hard wind-affected snow in exposed terrain and weak, faceted snow or surface hoar crystals in sheltered terrain. It may take some time for the snow to bond to these old surfaces.
Basal faceted snow remains part of the snowpack structure in much of the region. Once we see a substantial warm-up, we'll be thinking about the potential for the reactivation of basal layers.