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Gudauri

Icon for Avalanche Hazard: Considerable

Natural avalanches are possible, human-triggered avalanches are likely. Small avalanches in many areas, or large avalanches in specific areas, or very large avalanches in isolated areas.

The next few days will be very warm. Wind slabs have formed near ridges. Wet snow or windslab avalanches - or a rider who hits the 'sweet spot' - could set off a buried weak layer, resulting in potentially large and dangerous slides. It might be spring, but unstable snow still persists around the Gudauri area. Be conservative in your decisions for the next few days.

Forecast issued at: ⁨27 March 2024 22:00⁩

Forecast valid until: ⁨29 March 2024 22:00⁩

Forecaster: ⁨Manu Greer⁩

Forecast Area

High Alpine

> 2600m

Icon for Avalanche Hazard: Considerable Elevation Hazard Diagram high-alpine considerable

3 Considerable

Dangerous avalanche conditions. Careful snowpack evaluation, cautious route-finding and conservative decision-making essential.

Alpine

2000m - 2600m

Icon for Avalanche Hazard: Considerable Elevation Hazard Diagram alpine moderate

2 Moderate

Heightened avalanche conditions on specific terrain features. Evaluate snow and terrain carefully; identify features of concern.

Sub Alpine

< 2000m

Icon for Avalanche Hazard: Considerable Elevation Hazard Diagram sub-alpine moderate

2 Moderate

Heightened avalanche conditions on specific terrain features. Evaluate snow and terrain carefully; identify features of concern.

Avalanche Problems

Persistent Slab

Problem Type Persistent Slab Icon
Problem Type
Aspect/Elevation
Aspect/Elevation
Avalanche Size
Avalanche Size
Likelihood
Likelihood
A slab formed over a persistent weak layer.

Crusts with weak, sugary snow above and below them have been seen in the upper and mid snowpack (below the recent new snow layers). These have failed easily in snow tests. Whumphing has been observed at various aspects and elevations. Large avalanches could be started by a smaller surface avalanche, a heavy load - like a group of skiers or someone jumping - or by an unlucky rider hitting the 'sweet spot' (often an area where the slab is shallow). These problems will be worse at high elevations and in areas where the snowpack is shallower.

Sensitivity The specific avalanche problem type is difficult to trigger with a human rider.
Distribution Specific areas, with common characteristics. Evidence for instabilities exists, but it is not obvious and finding it requires careful observations.
Time of Day All day
Trend No change
Confidence Moderate

Wind Slab

Problem Type Wind Slab Icon
Problem Type
Aspect/Elevation
Aspect/Elevation
Avalanche Size
Avalanche Size
Likelihood
Likelihood
A cohesive layer of snow (a slab) formed by the wind drifted snow.

SW, W and NW winds have moved the fresh snow, expect build-ups near ridges and avoid these areas - a windslab avalanche could break a deeper layer resulting in a much larger release.

Sensitivity The specific avalanche problem type is reactive to human rider triggers. Easy to trigger with ski cut.
Distribution Specific areas, with common characteristics. Evidence for instabilities exists, but it is not obvious and finding it requires careful observations.
Time of Day All day
Trend No change
Confidence Low

Loose Wet

Problem Type Loose Wet Icon
Problem Type
Aspect/Elevation
Aspect/Elevation
Avalanche Size
Avalanche Size
Likelihood
Likelihood
A type of loose snow avalanche composed of wet or moist snow.

When the new snow is hit by sun, or when cloud traps in the heat, loose snow avalanches are likely from mid-morning to late afternoon, especially in steep rocky areas. A rising freezing level will increase the problem. These slides may also be the trigger for a larger slab avalanche on slopes below. Stay out from under steep sunny faces if you see evidence of snow movement, for example 'rollerballs'.

Sensitivity The specific avalanche problem type is reactive to human rider triggers. Easy to trigger with ski cut.
Distribution Specific areas, with common characteristics. Evidence for instabilities exists, but it is not obvious and finding it requires careful observations.
Time of Day All day
Trend No change
Confidence Moderate

Recent Avalanches and Snowpack

Recent avalanche activity:

27 March - multiple size 2 windslabs seen on Lomisa - Miketi ridge E and NE, 2000 - 2900 m, some involved deeper layers.

26 March - multiple large slabs on Sadzele W and NW aspects 2900 - 3200 m, triggered by expolsives - including three size 3 slides.

25 March - Multiple size 3 slabs, N aspect along the ridge E of Arakhveti on or near Mujukhi.

21 March - Natural size 3 storm slab, SW aspect, in Kobe Valley next to the waterfall, likely triggered by loose wet avalanche. Several size 1 to 2 slab avalanches on W and SE aspects with some evidence of step-down between layers.

Glide slabs are active on multiple aspects (more commonly E, S and W), some up to size 3. These are more likely in warm weather but can release at any time - if you see cracks in the snow, do not stop under these areas!

Snowpack:

Around 80 cm of new snow fell between early Friday 22nd and Monday 25th. The new layer is becoming more stable due to mild temperatures, but the previous snowpack has crusts with and weak facet layers in the upper half. Whumphing and failures in snow tests have been seen recently. Wind from SW and W has formed slabs near ridges in sheltered areas. Cornices in some locations are getting large (particularly on Lomisa Ridge); treat them with respect.

Weather

Sunny the next two days with some cloud on Thursday, winds mostly light from the W quarter. Warm temps - freezing levels 2400 m - 2650 m.

Disclaimer

Our avalanche forecasters are internationally qualified and experienced professionals, and data is provided by skilled observers. We encourage you to make your own observations and decisions, without relying solely on our forecast, since any forecast is a generalised 'best guess', and in certain cases it might be inaccurate. We can not be held liable for any actions you take in the backcountry that may result in injury, loss or death.