Alpes du Sud
Devoluy
Day Risk Profile
Avalanche Problems
Wind slab + Persistent weak layers + No distinct problem
3
Field notes
Wind slab
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.
Persistent weak layers
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 are very challenging to recognise. 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 and shooting cracks are typical when present, but you can have a serious weak layer with no warning signs at the surface. Knowledge of how the Snow deposited on the ground in a multiplicity of layers.EAWS glossary has evolved is essential. SLF's travel advice is direct: travel conservatively, avoid terrain where the consequences of being caught are large, and treat the history of weather and snow as more important than what you can see today. Read the full bulletin.
No distinct problem
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.
Avalanche Activity
NOUVELLES INSTABILITÉS EN FORMATION DANS LA NEIGE VENTÉE
peu probables le matin. Ils se multiplient à haute altitude sous l'effet du vent, puis des chutes de neige. Encore rares l'après-midi, ils deviennent
nombreux en soirée, de taille moyenne, à grande.
le manteau neigeux n'est que modérément stabilisé en altitude. Ces instabilités se situent en orientations ouest, nord et est, au-dessus de 2000
m d'altitude. Un skieur peut les déclencher, parfois à distance, et générer des avalanches de taille moyenne (taille 2) . Peu nombreuses lundi matin, elles se multiplient en
cours de journée, et sont le plus souvent d'Direction in which a slope faces as indicated by compass direction of the fall line; i.e. a north slope faces in a northerly direction.EAWS glossary dur. Le fort vent de sud favorise la formation de nombreuses instabilités superficielles, qui reposent sur une couche de neige
récente, faisant office de couche fragile temporaire. Plus rarement, un large départ linéaire de grande taille est possible, en cas de sollicitation de couche fragile persistante
plus profondément enfouie.
En versants bien ensoleillés, et sous 2000 m environ, le risque est limité, le manteau neigeux a pris de la cohésion avec le redoux.
Outlook
Increasing avalanche danger
Snowpack & Weather
Snowpack
Situation avalancheuse typique
neige ventée couche fragile persistante
Déclenchements provoqués : le manteau neigeux n'est que modérément stabilisé en altitude. Ces instabilités se situent en orientations ouest, nord et est, au-dessus de 2000
m d'altitude. Un skieur peut les déclencher, parfois à distance, et générer des avalanches de taille moyenne (taille 2) . Peu nombreuses lundi matin, elles se multiplient en
cours de journée, et sont le plus souvent d'Direction in which a slope faces as indicated by compass direction of the fall line; i.e. a north slope faces in a northerly direction.EAWS glossary dur. Le fort vent de sud favorise la formation de nombreuses instabilités superficielles, qui reposent sur une couche de neige
récente, faisant office de couche fragile temporaire. Plus rarement, un large départ linéaire de grande taille est possible, en cas de sollicitation de couche fragile persistante
plus profondément enfouie.
En versants bien ensoleillés, et sous 2000 m environ, le risque est limité, le manteau neigeux a pris de la cohésion avec le redoux.
Départs spontanés : peu probables le matin. Ils se multiplient à haute altitude sous l'effet du vent, puis des chutes de neige. Encore rares l'après-midi, ils deviennent
nombreux en soirée, de taille moyenne, à grande.
Outlook
km/h 70 km/h 120 km/h
Tendance du mardi 03 février
Indice de risque fort
sque en hausse après les chutes de neige
la nuit. Risque a minima marqué, mais
que fort non exclu.