Jan 27 update
https://www.powderhighwaybackcountry.com/omega-blocked/
https://www.powderhighwaybackcountry.com/omega-blocked/
Temperatures have plunged recently, but the skiing is still fantastic. The big dump we had in early February and subsequent small inputs of precipitation have tapered off as this cold front moved in. The 50-60cm of storm snow has settled to 15 -30cm over top of the January 30 crust/ surface hoar/facet interface. Natural and human triggered avalanche activity has tapered off as well. The storm snow has faceted and there is little cohesion/slab properties in it, making for great skiing and decreased avalanche hazard as of late.
There is variable wind effect in the alpine around Rogers Pass. Features that would be subject to down flow (catabatic) wind effect have been affected. Solar aspects are skiing well, however you can feel the Jan 30 MFcr under the storm snow, which makes for fast skiing! With temps near -20, staying in the sun has been nice.
Snowpack Concerns
Outlook





People often ask when is the best time to ski in BC; well, it varies. This year January and February were cold and dry and March has provided some of the best powder skiing of the season. Consistent snowfall and reasonable freezing levels have yielded exceptional conditions again this week. However, the snowpack is still challenging. The unsettled weather has come with wind and periods of sun, which have created wind slabs in immediate lee features and melt freeze crusts on solar aspects.
After an incredible week of powder skiing, the temps sky rocketed and the rain fell. The weekend before last brought significant precipitation in mixed forms with elevated freezing levels, which yielded a significant avalanche cycle. Sadly, it claimed the lives of three people. Over the course of last week, the freezing levels remained high for the better part of the week, with peak heating occurring last Wednesday; this too yielded a large avalanche cycle. The rain soaked snowpack and persistent layers in the upper and mid pack were no match for the intense solar radiation.
After the late March warm-up, and ensuing precipitation, a ridge of high pressure established itself over the Powder Highway region; fortunately the storm system went out cold and deposited 20-30cm of storm snow above 1700m. The late March warm up and rain event caused a significant avalanche cycle and stressed the snowpack enough that stability improved significantly during the first week of April when temperatures cooled off.
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