North Columbia

Give the snow time to settle and stick to conservative terrain where there is more than 25cm of new snow. Check for how the new snow is bonding to older crusts below. Reduce your exposure to sunny slopes if the sun makes an appearance.

Moderate - Due to the number of field observations

We're looking at unsettled weather with cooling temperatures until the next system arrives on Friday.WEDNESDAY: Sunny with cloudy periods and isolated flurries. Moderate west winds 20-50 Km/hr. Freezing level to 1400 metres with alpine high temperatures around -5. THURSDAY: Cloudy with sunny periods and flurries in the afternoon. Winds becoming light westerly. Freezing level dropping to 700 metres with alpine high temperatures of -6.FRIDAY: Cloudy with flurries (5-10cm snow). Light north / west winds. Freezing level 500 metres with alpine high temperatures around -9.

A widespread natural avalanche cycle to size 2.5 was reported on Tuesday, all aspects at tree line and in the alpine.  On Monday, backcountry skiers triggered a size 2 wind slab near the Asulkan cabin on a northeast aspect near 2050m. The slab's thickness varied from 40-60cm. See the MIN report for more details. On Saturday we received reports of several wind slabs and storm slabs to size 2.5, mostly on northerly aspects above 2200m. Also on Saturday, a wet loose size 1.5 avalanche injured a skier in Glacier National Park on a west aspect near 2000m.

New amounts of (heavy) snow varied widely on Tuesday, ranging from 18 to 38 cm. Winds have been moderate to strong from the south / east. Wind slabs from late last week (thanks to south / east winds) remained reactive throughout the weekend on immediate lee features. Isolated pockets of surface hoar (buried March 18th) have been reported between old storm snow layers on shaded aspects at higher elevations and may be found approximately 45-70 cm below the surface. New snow amounts taper with elevation and below 1800 m, reduced accumulations have buried a supportive crust on all aspectsDeeper persistent weak layers from January and December are generally considered dormant, but could wake up with a surface avalanche stepping down, large cornice fall, or a human trigger in a shallow or variable-depth snowpack area. These layers consist of sun crust, surface hoar and/or facets.