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RegisterJan 17th, 2020–Jan 18th, 2020
South Coast.
Rapid and continuous loading of new snow, strong wind, and rising temperatures are expected to bring a widespread natural avalanche cycle to the region this weekend. Travel in avalanche terrain is not recommended.
Friday night: Cloudy with increasing snowfall bringing 15-20 cm of new snow by morning. Moderate southeast winds increasing to strong south by morning.
Saturday: Cloudy with continuing snowfall bringing 20-30 cm of new snow cm of new snow, continuing overnight. Strong south winds shifting southwest. Alpine high temperatures reaching -2 as freezing levels rise to 1300 metres by afternoon.
Sunday: Cloudy with continuing snowfall bringing a final 10 cm of new snow and 2-day snow totals to about 60 cm. Precipitation ending in light rain, with rain increasing again overnight. Moderate to strong south winds. Alpine temperatures reaching +1 as freezing levels rise to 1900 metres by afternoon and continue to rise overnight.
Monday: Cloudy with light rain, possible wet flurries in the alpine. Moderate south winds becoming light and shifting southeast. Alpine temperatures around 0 with freezing levels to 1700 metres.
MIN reports from Wednesday on the North Shore described quite touchy conditions, with 5-15 cm-deep storm slabs triggering easily with skier traffic on steep slopes. Similar conditions are expected to have persisted through Thursday.
Looking forward, the coming storm is expected to form a widespread new storm slab problem as new snow accumulates and forms reactive slabs as a result of wind and rising temperatures.
Up to 50 cm of new snow is expected to accumulate over the region by the end of the day on Saturday. This will bury wind-affected surfaces in exposed areas at all elevations and soft, low density snow in sheltered areas.
The new snow is expected to bring snow totals from the past week to about 170 cm. Collectively, all this snow rests on a hard melt hard melt-freeze crust below 1500 m and on previously wind-affected snow at higher elevations.
In some areas a weak layer of surface hoar exists above this crust. Recent snowpack tests on the North Shore have given variable, sometimes quite sudden results at this interface, particularly where this combination of crust and surface hoar was identified.