Register for an account and never miss a forecast again!
RegisterRegister for an account and never miss a forecast again!
RegisterJan 9th, 2021–Jan 11th, 2021
Yukon.
Avoid ridge crest & rock outcroppings in the alpine where you're most likely to trigger hard slabs. Softer slabs at treeline may rest on buried surface hoar making them surprisingly touchy. More snow and wind is on the way which is expected to exacerbate the wind slab problem.
Quite a bit of snow and wind in store for the forecast period. We’ll be watching these snowfall amounts closely.
SATURDAY NIGHT: Freezing level at valley bottom, strong south wind, 2 to 5 cm cm of snow possible.
SUNDAY: Overcast, freezing level at valley bottom, strong south/southeast wind, 2 to 10 cm possible during the day with another 2 to potentially as much as 15 cm Sunday night.
MONDAY: Overcast, freezing level at valley bottom, strong south/southwest wind, 5 to 15 cm of snow possible.
TUESDAY: Overcast, freezing level at valley bottom, strong south/southeast wind, 5 to 20 cm of snow possible.
We received word of a snowmobile triggered wind slab avalanche north of Log Cabin that occurred on Thursday. Sounds like everyone is okay, but the avalanche occurred at treeline in relatively benign terrain which speaks to the reactivity of fresh wind slabs that may rest on surface hoar.
Firm slabby snow can now be found in almost all wind exposed terrain. The predominant wind has been from the south but some north wind snuck in Thursday night meaning wind affected snow can be found on all aspects.
In terrain around treeline there may be fresh wind slab sitting on surface hoar that is capable of producing large human triggered avalanches. See this MIN report that has a snow profile that features surface hoar down 40 cm below the surface.
A buried crust formed in early December can be found 60-100 cm below the surface, but most reports suggest the snow is quite well-bonded to this crust.
The lower snowpack is strong around White Pass, but there is potential for a generally thinner and weaker snowpack structure to exist in inland areas such as the Wheaton Valley.