Churfirsten and Rhine Valley
Flumserberg
Avalanche Problems
Wind slab
3-
Field notes
Look for fresh snow deposits on Slope facing downwind/ wind sheltered aspect. Snow deposits can attain several times average snow depth.EAWS glossary, in Usually a steep, elongated, eroded trench; typically prone to snowdrift accumulation.EAWS glossary and Rounded or elongated concavity; typically tending to accumulate snowdrift.EAWS glossary, and behind ridgelines and abrupt changes in terrain — these are where the wind has loaded the snow into slabs that are easy to trigger. Recent avalanches, shooting cracks under your weight, and Distinctive noise (resembling a “whumpf” sound) occurring when a weak layer beneath a slab collapses. The air of the weak layer is forced outside the snowpack, with the resulting whumpf sound being heard. The sound usually indicates an unstable situation and can be accompanied by surface cracking. A whumpf is a clear avalanche alert.EAWS glossary sounds are clear confirmations of the problem. The safest move is to avoid wind-loaded terrain entirely. NB wind signs alone don't always mean an avalanche problem exists, and the age of drifted snow is hard to judge.
Snowpack & Weather
Snowpack
On shady slopes, the new snow is falling on top of a faceted snow surface and sometimes also Transparent, frequently flat crystals forming on the snowpack when moist air settles on the surface. It forms most often during cold, clear, humid nights. Once it is blanketed by fresh fallen snow, surface hoar is one of the most critical weak layer. See also: www.snowcrystals.itEAWS glossary. Deeper layers are often relatively well consolidated in the extreme west of Lower Valais as well as in the north. South of a line from Rhône to the Rhine, the entire Snow deposited on the ground in a multiplicity of layers.EAWS glossary is often faceted and loose.
The snow depths in all regions are well below average for the time of year.
Weather review for Wednesday
It was sunny and cold in the mountains.
Fresh snow
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Temperature
At midday at 2000 m, between -13 °C in the north and -9 °C in the south
Wind
Northerly wind:
- Moderate to strong during the night on the Main Alpine Ridge and to the south of it
- Elsewhere light to moderate
Weather forecast to Thursday
Snowfall will set in overnight to Thursday in the west and north and will intensify as the day progresses. The snowfall level will increase from the west from low altitudes towards 1200 to 1400 m.
Fresh snow
From Wednesday evening to Thursday afternoon, the following amounts will fall above 1800 m:
- Northern Alpine ridge west of the Reuss, Valais excluding southern Goms: 15 to 30 cm
- Western Jura, remaining northern flank of the Alps, remaining northern Alpine ridge, Gotthard region, northern Grisons: 5 to 15 cm
- Elsewhere less, dry on the central part of the southern flank of the Alps
Temperature
Pronounced rise in temperatures from the west. At midday at 2000 m, between -2 °C in the west and -8 °C in the east
Wind
Increasingly strong to storm-force westerly to northwesterly wind at high altitudes
Outlook to Saturday
Intense precipitation will fall until Saturday morning, especially in the west and north. The snowfall level in the north will temporarily rise towards 1700 m overnight to Friday and then fall again to low altitudes. The snowfall will be accompanied by a storm-force westerly wind. The intensity of the precipitation will decrease on Saturday. A total of 50 to 80 cm of new snow is expected in the west and north, with up to 1 metre in the extreme west of Lower Valais and northern Lower Valais.
On Friday, danger level 4 (high) is expected to be reached across a widespread area in Valais as well as in some regions on the western part of the northern flank of the Alps and on the northern Alpine ridge west of the Reuss. The avalanche danger will also increase significantly on the remaining northern flank of the Alps and in northern Grisons. In the regions exposed to heavier precipitation, naturally triggered avalanches, including increasingly very large ones, are to be expected. In southern Valais in particular, where the structure of the Snow deposited on the ground in a multiplicity of layers.EAWS glossary is weak, avalanches can sometimes sweep away the entire Snow layers deposited from earlier precipitation, prior to fresh fallen snow. Old snow layers consist of metamorphosed snow crystals.EAWS glossary. Due to the low snowfall level, avalanches can carry along a lot of new snow even at intermediate altitudes and advance into the valleys along usual avalanche paths. However, exceptionally large run-out zones are unlikely. Exposed parts of transportation routes may be at risk.
As the day progresses on Saturday, natural avalanche activity is expected to decrease as the snowfall subsides. However, the avalanche danger is expected to remain high (danger level 4).