Snowdrift accumulations still trigger-sensitive, esp. on steep shady slopes at high altitude
Avalanche danger above the timberline is MODERATE, below that altitude danger is low. In all aspects, small-to-medium slab avalanches can be triggerd by minimum additional loading in places. Danger zones occur mostly near ridgelines and behind protruberances in the landscape, esp. on W/N/NE facing slopes, caution also urged near treelines and in forest clearances. Size and frequency of danger zones tend to increase with ascending altitude. Above 2000m, releases can fracture down to more deeply embedded layers inside the snowpack and grow to larger size. Small glide-snow and loose-snow avalanches can trigger naturally. Avalanche danger above 2000m is MODERATE, below that altitude danger is low. Slabs, mostly small-sized, can be triggered even by minimum additiional loading both near to and distant from ridgelines and behind protruberances in the landscape on north, northwest and south facing slopes. If they fracture down to more deeply embedded layers in the snowpack the releases can grow to medium size. Isolated glide-snow avalanches reaching medium size are possible at any time of day or night.
Snowpack
Often hardened snowdrift masses lie atop an expansively metamorphosed, loosely-packed snowpack surface with near-surface faceted crystals. Near surface crusts are weak layers of faceted, expansively metamorphosed crystals. Particularly in shady, shallow-snow zones there is snow which is rewarding to skiers, it is faceted, expansively metamorphosed powder which is settling increasingly with rising temperatures. In general, too little snow on the ground for this juncture of the season.
Tendency
Snowdrift problem receding further. Snowdrift problem stabilizing increasingly.
Danger level
2400m
Avalanche Problem
Wind slab
2400m
Be careful of fresh snowdrifts.
Freshly generated snowdrift accumulations are small-sized yet still often prone to triggering, particularly in gullies and bowls along the Salzburg border, such danger zones are easy to recognize. Avalanches can in isolated cases fracture down to more deeply embedded layers in the old snopwack and then grow to medium size. On shady slopes and in high alpine zones the likelihood of triggering is higher. Caution urged especially in seldom-skied terrain.
Snowpack
dp.6: cold, loose snow and wind dp.1: deep persistent weak layer
Freshly generated snowdrift accumulations lie deposited particularly above 2400m were depositedon W/N/E facing slopes. More deeply embedded inside the old snowpack are faceted, expansively metamorphosed weak layers, esp. on shady wind-protected slopes. Clear skies are forecast, with low temperatures and low air moisture. Thus, the snowpack will expansively metamorphose during the nocturnal hours. The snowpack is highly diverse even over small areas.
Tendency
Gradual decrease in avalanche danger
Danger level
2000m
Avalanche Problem
Wind slab
2000m
Snowdrift accumulations: assess them with caution
Small-area avalanche prone locations in the form of snowdrift accumulations, esp. in wind-loaded steep terrain, in gullies and bowls, and behind protruberances in the landscape, on shady slopes often triggerable above the treeline by one sole skier and then possibly growing to medium size. However, the danger zones are easy to recognize for the practiced eye, thus, should be circumvented. In high-alpine regions the danger zones occur more frequently and the risks are greater. On steep shady slopes at high altitudes where the snow is shallow and in transitions from shallow to deep snow, slab avalanches can be triggered. A cautious route selection is imperative. At lower altitudes, isolated small avalanches are possibly triggered in extremely steep terrain. Naturally triggered small loose-snow avalanches are possible on extremely steep sunny slopes.
Snowpack
Moderate-to-strong southerly winds have generated fresh snowdrift accumulations, they lie deposited on shady steep slopes atop weak layers and are prone to triggering. Elsewhere, the snowpack is stabilizing. The near-surface layers are still generally loosely-packed, except where winds have had their effect. There are lots of wind crusts and, on south-facing slopes, a shallow surface crust. More deeply embedded layers inside the snowpack are unlikely to trigger, at most where the snow is shallow and on very steep shady slopes. Particularly in sunny aspects, glide cracks are opening again on steep grassy slopes.
Tendency
Snowdrifts increasingly stabilizing
Danger level
2000m
Avalanche Problem
Wind slab
2000m
Fresh snowdrifts deposited on soft layers
Avalanche danger above 2000m is moderate, below that altitude danger is low. Snowdrift accumulations are problematic. Small slab avalanches can be triggered even by one sole skier. Danger zones occur in steep ridgeline terrain on W/N/E facing slopes and in wind-loaded gullies and bowls. Give consideration to the risks of being swept alone and forced to take a fall.
Snowpack
In northern aspects snowdrifts have been deposited atop an irregular snowpack and can be prone to triggering, particularly if the old snowpack in shady regions is expansively metamorphosed. At high altitudes, in addition, trigger-sensitive intermediate layers in the uppermost part of the snowpack have persisted. Larger fractures over wide surfaces are unlikely. On south-facing slopes there is little snow on the ground, usually encrusted in the early morning hours, then softening later on. In wind-exposed terrain, the snowpack surface is wind-pressed; on shady slopes there is still loosely-packed zone atop a stable old snowpack fundament in wind-protected zones.
Tendency
Avalanche danger levels are expected to recede again.
Danger level
2000m
Avalanche Problem
Wind slab
2000m
Persistent weak layer
2000m
Snowpack
Tendency
Danger level
1800m
Avalanche Problem
Wind slab
1800m
Persistent weak layer
1600m
With the south wind on shady slopes fresh, poorly bonded snowdrift on top of surface hoar!
The avalanche danger above 1.800 m is moderate. In shady areas slab avalanches can be triggered by small additional loads. These avalanches are usually small but can reach medium size in some places. Danger spots are usually located in shady northwestern to eastern expositions especially in transitions from little to much snow, in entries to steep gullies and bowls and behind ridgelines. The danger areas increase with height.
Snowpack
Due to mild sunny weather the snow cover got soft in sunny high-altitude slopes. On shady slopes driftsnow-which formed during precipitation Wednesday-is prone to triggering in some places. Also du to south winds there can driftsnow formed again which is poorly bonded to the predominantly existing surface hoar. In addition persistent weak layers are there for a longer period due to low amounts of snow and faceted snow layers and crusts which are weakening the snow base.
Tendency
Due to cooling tension within the snowdrift are persistent.
Danger level
2000m
Avalanche Problem
Wind slab
2000m
Snowdrift accumulations still trigger-sensitive, esp. on steep shady slopes at high altitude
Avalanche danger above 2000m is MODERATE, below that altitude danger is low. Slabs, mostly small-sized, can be triggered even by minimum additiional loading both near to and distant from ridgelines and behind protruberances in the landscape on west to north to northeast-facing slopes, but caution is also urged near the treeline and in forest clearances. In isolated cases, triggerings can fracture down to more deeply embedded layers in the snowpack the releases can grow to medium size. Isolated naturally triggered glide-snow and loose-snow avalanches are possible at an time of day or night.
Snowpack
Often hardened snowdrift masses lie atop an expansively metamorphosed, loosely-packed snowpack surface with near-surface faceted crystals. Near surface crusts are weak layers of faceted, expansively metamorphosed crystals. Particularly in shady, shallow-snow zones there is snow which is rewarding to skiers, it is faceted, expansively metamorphosed powder which is settling increasingly wit rising temperatures.
Tendency
Avalanche danger levels decreasing further. Snowdrift problem is receding slightly.
Danger level
Little snow on the ground.
Avalanches are hardly possible in gullies and bowls. Only little snow is on the ground.
Snowpack
The old snowpack is expansively metamorphosed, with a loosely-packed surface with surface hoar and faceted crystals
Tendency
No significant change expected in avalanche danger levels
Danger level
1800m
Avalanche Problem
Persistent weak layer
1800m
Caution: weak layers in the old snowpack
Weak layers in the old snowpack can in isolated cases on shady slopes be triggered even by one sole skier. Caution urged esp. in transitions into gullies and bowls above 1800m and at the foot of rocky cliffs and behind protruberances in the landscape. Avalanches are mostly small-sized. Apart from the risks of being buried in snow masses, the dangers of being swept along and forced to take a fall need to be taken into condideration.
Snowpack
Olderr snowdrift accumulations blanket a weak old snowpack, esp. on wind-protected shady sloppes. The snowpack will expansively metamorphose during the nocturnal hours. The snowpack is highly diverse even over small areas. Below 1600m very little snow on the ground.
Tendency
No change expected in avalanche danger levels
Danger level
Avalanche Problem
Persistent weak layer
Snowpack
Tendency
Danger level
Snowpack
Tendency
Danger level
2000m
Avalanche Problem
Persistent weak layer
2000m
Caution urged towards the risks of taking a fall
Avalanche danger is low. Locally, weak layers in the old snowpack can be problematic. Small slab avalanches can be triggered in isolated cases by large additional loading, which happens more likely in places with little snow. Avalanche prone locations occur in extremely steep ridgeline terrain in W/N/E aspects as well as at entries into gullies and bowls. Dangers of being swept away and of taking a fall outweigh those of being buried in snow masses.
Snowpack
The snowpack is stable by and large. At high altitudes, foehn winds have generated shallow snowdrifts on north-facing slopes. In addition, trigger-sensitive intermediate layers in the uppermost part of the snowpack have persisted. Fracture propagation is unlikely. On south-facing slopes there is little snow on the ground, mostly encrusted in the morning hours before softening up later on. In wind-exposed terrain the surface is wind-pressed, on shady slopes with little wind there is still loosely-packed snow.
Tendency
Avalanche danger levels will remain low.
Danger level
2000m
Avalanche Problem
Wind slab
2000m
Snowdrifts at high altitudes still prone to triggering in places
Particularly in ridgeline zones and in very steep gullies and bowls, small-area freshly generated snowdrift accumulations are evident, mostly small sized but prone to triggering. Esp. on shady high-altitude slopes they can be triggered even by one sole skier. Danger zones tend to increase in frequency with ascending altitude, evaluate these with high caution wherever falls are possible. Naturally triggered small loose-snow avalanches are naturally triggerable on extremely steep sunny slopes.
Snowpack
Moderate-to-strong southerly winds have generated fresh snowdrift accumulations, they lie deposited on shady steep slopes atop weak layers and are prone to triggering. Elsewhere, the snowpack is stabilizing. The near-surface layers are still generally loosely-packed, except where winds have had their effect. There are lots of wind crusts and, on south-facing slopes, a shallow surface crust. More deeply embedded layers inside the snowpack are unlikely to trigger, at most where the snow is shallow and on very steep shady slopes. Particularly in sunny aspects, glide cracks are opening again on steep grassy slopes.
Tendency
Snowdrifts increasingly stabilizing
Danger level
treeline
Avalanche Problem
Wind slab
Treeline
Only isolated danger spots due to snowdrift in shady areas.
The avalanche danger is low. In some danger spots slab avalanches can be triggered by small additional loads. These are in general small. Danger spots are located in in shady slopes and steep areas adjacent to ridgelines, in high-altitude entries into gullies and bowls and behind terrain edges. In case of triggered avalanches risk of injuries is more likely than risk of being buried.
Snowpack
The winter so far-which was cold and without lots of snow- reflects the composition of the snowcover. The snow base is formed by a succession of crusts in which weak layers and faceted snow is found. In shady slopes small amounts of older snowdrift and now with the south wind blown-in snow. On sunny slopes the snow cover has settled.
Tendency
No significant changes.
Danger level
treeline
Avalanche Problem
Persistent weak layer
Treeline
Danger of taking a fall outweighs that of being buried in snow
Avalanche danger is low. Particularly on very steep shady slopes above the timberline, slab avalanches can be triggered in isolated cases by minimum additional loading. Releases are mostly small-sized. Apart from th danger of being buried in snow masses, the risks of being swept along and forced to take a fall need to be taken into consideration.
Snowpack
Mostly shallow snowdrift masses lie deposited on shady slopes, often atop a weak, heavily faceted and expansively metamorphosed layer of old snow.
Tendency
No significant change in avalanche danger levels anticipated
Danger level
2000m
Avalanche Problem
Wind slab
2000m
Isolated danger zones in gullies and bowls
Older snowdrift accumulations are generally small-sized, triggerable only in isolated cases, esp.on wind-protected shady slopes above 2000m, esp. in transitions into gullies and bowls and at the foot of rocky cliffs and behind protruberances in the landscape. Apart from the risks of being buried in snow masses, the danger of being swept along and forced to take a fall require consideration.
Snowpack
dp.1: deep persistent weak layer
The older snowdrifts blanket a weak old snowpack. The snowpack is highly diverse even over small areas. Only little snow on the ground from region to region below 1600m. Clear nighttime skies are forecast, with low temperatures and low air moisture. Thus, the snowpack will expansively metamorphose during the nocturnal hours. The snowpack is highly diverse even over small areas. Below 1600m very little snow on the ground.
Tendency
No significant change in avalanche danger levels i expected
