Wind slab
- All elevations
Small snowdrift accumulations are often still prone to triggering in steep terrain
Small snowdrift accumulations are often still prone to triggering in steep terrain
Small fresh and covered snowdrift accumulations of recent days are still prone to triggering in places. They increase in size and frequency with ascending altitude. One sole skier/boarder can trigger an avalanche in steep terrain. They are generally small-sized. In isolated cases avalanches can be triggered in the old snow by large additional loading. Such danger zones are mostly in extremely steep, usually shady terrain. Apart from the risks of being buried in snow, the hazards of being swept along and taking a fall need to be considered.
Fresh snow and fresh snowdrifts of the last few days have been able to settle further and increasingly consolidate. On shady slopes they lie atop cold, powdery layers of old snow. On sunny slopes, often atop melt-freeze encrusted old snowpack surfaces. Bonding to them and inside the new layers themselves is generally good, but worsens with ascending altitude. The old snowpack is well consolidated and stable. Weak layers beneath melt-freeze crusts at mid-level of the snowpack can ordinarily be triggered only be large additional loading.
It will be very sunny, temperatures will rise further, the zero-degree will ascend during the day to 2400 m. Temperature at 2000 m: -2 to +2 degrees. Brisk NE winds, slackening off this afternoon.
Tuesday and Wednesday will be quite sunny, temperatures will rise a further notch. Avalanche danger will continue to diminish.
Bulletin data: Avalanche Warning Service Vorarlberg (CC BY 4.0)