Register for an account and never miss a forecast again!
RegisterRegister for an account and never miss a forecast again!
RegisterJan 18th, 2020–Jan 19th, 2020
South Coast.
A mix of heavy snowfall, strong wind, and a transition to rain are expected to maintain a widespread natural avalanche cycle in the region on Sunday. Travel in avalanche terrain is not recommended.
Saturday night: Cloudy with continuing snowfall bringing 30-40 cm of new snow. Moderate to strong south winds.
Sunday: Cloudy with easing snowfall bringing 10-15 cm of new snow before transitioning to light rain. Moderate to strong south winds. Alpine temperatures increasing to +3 as freezing levels climb to 2200 metres by afternoon.
Monday: Cloudy with wet flurries or rain bringing about 10 cm of new snow to the alpine. Moderate south winds easing over the day. Alpine temperatures around 0 to -1 with freezing levels to 1500 metres.
Tuesday: Cloudy with wet flurries bringing about 10 cm of new snow to alpine and treeline. Moderate south winds. Alpine temperatures around -2 with freezing levels dropping from 1400 metres to 1000 metres over the day.
No avalanches from the current storm have yet been reported, but the ongoing storm has been forming a widespread new storm slab problem as new snow accumulates and forms slabs as a result of wind and rising temperatures. Active natural avalanche conditions are expected to have become increasingly widespread in areas that saw upwards of 25 cm of new snow by the end of the day Saturday.
A further rise in temperatures may allow for rain falling on snow late Sunday, which will further destabilize recent snow accumulations and promote wet loose avalanche activity.
2-day snow totals over the region are expected to reach 50-60 cm by the end of the day on Sunday. The new snow has buried wind-affected surfaces in exposed areas at all elevations and soft, low density snow in sheltered areas.
The new snow will 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.