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Ticino Sopraceneri

Untere Maggiatäler

Wed 10 Dec

Avalanche Problems

Low (1) Dry avalanches · all day
Dry snow level 1 No distinct problem 1
All aspects
above 2200m
Only a little snow is lying. Individual Locations delineated by aspect or altitude where avalanches can trigger and people or objects are at risk.EAWS glossary for dry avalanches are to be found in extremely steep terrain. Even a small avalanche can sweep people along and give rise to falls.
Field notes

SLF uses this label when no single problem dominates the assessment, often on lower-danger days. It doesn't mean conditions are safe: any avalanche type is still possible, and normal caution applies. On stable days this is usually a signal to enjoy the mountains with general awareness; on less-stable days where the assessment is still inconclusive, it's a signal to be cautious specifically because there's no clear pattern to follow.

Source: SLF Avalanche Bulletin Interpretation Guide

Snowpack & Weather

Snowpack

The last few day’s new and drifted snow has stabilised well. However, this snow is lying on sometimes weakly bonded old snow. Snowpack layer in which the crystals are poorly bonded and the layer has the potential to fail. Typical crystals in dry weak layers causing avalanches are : precipitation particles; surface hoar; faceted crystals; hollow crystals; graupel. Generally >1mm in size, loose grains with few bonds Wet weak layers can be formed by all snow crystal/grain types.EAWS glossary in the Snow deposited on the ground in a multiplicity of layers.EAWS glossary are located in particular on northern and sometimes on eastern slopes above around 2400 m. On the northern flank of the Alps, they are sometimes directly beneath the new and drifted snow layers and sometimes also in the middle of the snowpack. In inneralpine regions and in northern Grisons, they are sometimes also in the lower part of the snowpack.

The Snow deposited on the ground in a multiplicity of layers.EAWS glossary has been moistened by rain below 2400 m and is saturated up to around 2100 m. Isolated Avalanche of wet snow masses. Flowing more slowly than dry avalanches; usually for shorter runout distances, however with greater impact on obstacles due to higher snow density.EAWS glossary are possible with the sunshine and rising temperatures during the daytime. Isolated gliding avalanches are still possible.

Weather review for Tuesday

After a mostly clear night, conditions were mainly sunny in the mountains during the day.

Fresh snow

-

Temperature

At midday at 2000 m, between +8°C in the north and +5°C in the south.

Wind

Mostly light to moderate from southwesterly directions

Weather forecast to Wednesday

After a mostly clear night, conditions will be sunny and mild.

Fresh snow

-

Temperature

At midday at 2000 m, around +4°C

Wind

Light to moderate southwesterly

Outlook

After a sometimes cloudy night, there will be some sunny intervals on Thursday. Friday will be mainly sunny after a clear night. Temperatures will remain mild with a light to moderate southwesterly wind.

The danger of dry avalanches is decreasing, although only very slowly in areas with a persistent Snowpack layer in which the crystals are poorly bonded and the layer has the potential to fail. Typical crystals in dry weak layers causing avalanches are : precipitation particles; surface hoar; faceted crystals; hollow crystals; graupel. Generally >1mm in size, loose grains with few bonds Wet weak layers can be formed by all snow crystal/grain types.EAWS glossary problem. The danger of wet avalanches follows a daily cycle and increases slightly over the course of the day. On steep grassy slopes, isolated glide-snow avalanches are possible.

Source

SLF

Issued

9 Dec 16:45 UTC

Valid until

10 Dec 16:00 UTC

Next update

10 Dec 16:00 UTC

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