North Columbia

Avalanche problems that peaked during the warm spell should diminish on Monday, but not disappear.

Moderate -

Sunday night: Mainly cloudy with isolated flurries bringing a trace to 5 cm of new snow. Light southeast winds.Monday: Cloudy with scattered flurries bringing 2-6 cm of new snow, light rain below about 1500 metres. Light to moderate south winds. Alpine high temperatures around 0 with freezing levels to 1900 metres.Tuesday: Cloudy with flurries bringing 5-10 cm of new snow with light rain below about 1100 metres, continuing overnight. Light to moderate southwest winds. Alpine high temperatures around -2 with freezing levels to 1500 metres.Wednesday: A mix of sun and cloud with cloud decreasing over the day and 24 hour new snow totals of 10-30 cm. Light northeast winds. Alpine high temperatures around -1 with freezing levels around 1700 metres.

The wet loose avalanche cycle from last Sunday to Friday diminished as cooler, seasonal temperatures returned to the mountains on Saturday. Evidence of the cycle is widespread at all elevations, with recent avalanches up to size 3 found mostly on southeast to southwest aspects. A few large slab avalanches were also triggered on other aspects, with many of them running to valley bottom.Looking forward, avalanche problems will be split between lingering loose wet problems (areas of isothermal snow that haven't already avalanched) and isolated persistent slab problems on high north aspects. The latter may present as a large old wind slab that remains triggerable because it sits on an interface of preserved cold, faceted (sugary) snow. Small new wind slabs are expected to form gradually as new snow accumulates at higher elevations.

Forecast light new snow amounts will accumulate above a surface of melt-freeze crust in most areas above 1500 metres, with the exception of north aspects above 2000 metres, where it will bury settled and preserved dry snow. Below about 1500 metres, precipitation as rain will land on variably isothermal (slushy) and crusty surfaces. This moisture will promote isothermal conditions where they don't already exist. The remainder of the snowpack is generally consolidated and strong. Exceptions may exist on northerly aspects above 2000 m, where a gradually strengthening layer of faceted grains buried 40 to 60 cm deep may still be preserved below an overlying slab of old and hard wind-affected snow.