Front Range =========== Current Keywords: CONSIDERABLE, MODERATE, avalanche cycle, avalanche danger, cornices, crust, crusts, facet, faceted, facets, settle, weak layer, weak layers, wind drifts, windslab, windslabs Issued 12/26/2008 3:43 PM by Spencer Logan Weather Discussion The Christmas storm will begin to wind down this afternoon. The southwest flow is weakening. Snow will continue through the night, but the driver will be cold air wedging its way in from the north. The Aspen zone and the northern side of the North San Juan zone will see the most benefit of this combination, but we're talking additional inches of snow, not feet. Flow turns northerly and brings in a cold, dry airmass that will supress snowfall by mid-day Saturday. The snow free break might be short. Snow may return Saturday in the form of a weak, unorganized system on northwesterly to westerly flow. Weather Forecast Fields Friday Night Saturday Saturday Night Temperature (°F) -5 to 0 5 to 10 0 to 5 Wind Speed (mph) 15 to 25 20 to 30 20 to 30 Wind Direction WNW NW WNW Sky Cover Mostly Cloudy MC Mostly Cloudy MC Mostly Cloudy MC Snow (in) 1 to 4 0 to 1 0 to 1 Snowpack Discussion The Christmas storm was the latest in a series. Once again the Front Range was on the margins. We picked up a few inches of snow Thursday night and Friday. The storm, like previous storms in the series, was sufficient for a widespread avalanche cycle. Instead, each storm pushed the snowpack close but not over the breaking point. Snow-free days allowed the snowpack to settle in and partially adjust to the load. At a minimum you can expect sensitive wind drifts and cornices formed in the storm snow. You will find them on northwest, north, northeast, and east aspects near and above treeline. Popping out a new windslab may get older weak layers to fail, too. There is a stack of recent windslabs from the earlier storms. There are deeper weak layers of concern. You can find layers of faceted snow near hard crusts in some areas, and a weak layer of basal facets throughout the zone. An ice crust within the basal facet layer has been particularly problematic. The areas where you can trigger an avalanche on one of these old, deep layers is slowly decreasing, but you can still trigger a large, dangerous avalanche if you find the right slope. Use all of your avalanche skills to evaluate the snowpack on each and every slope before you cross it. Remain skeptical of slopes that face north through east even if they initially appear to be stable. Avalanche Danger The avalanche danger for the Front Range zone is CONSIDERABLE on NW-N-NE-SE aspects near and above treeline and MODERATE on other aspects. Below treeline the danger is MODERATE on all aspects.