#ski #sport #avalanche

idea

There are three types of avalanches:

  1. Slab - well bonded snow on top of a weak layer. 95% of skier triggered avalanches, 98% of deaths
  2. Loose snow - loose snow releases at a point and snowballed.
  3. Glide snow - loss of friction to the ground, not triggered by humans.

Slabs are usually formed by

There are twice as many avalanches on north face than south, due to delayed settlement. East facing are also bad. However in wet condition, things reverse, since the hot snow get wetter and will result in wet avalanches. During prolonged cloudy situations, there's little difference.

3/4 of avalanches happen on slopes between 35 and 45 degrees (+2d on maritime climate). Steepness is a much better predictor than terrain shape[1]. Past 45 risk decreases.

Evaluation is danger + consequence.

Danger is evaluated using --/-/0/+ on:

Consequences are calculated with: --/-/0/+ on:

Always avoid high consequence

During ascent:

During descent:

10 commandments

  1. Go one by one
  2. Have an escape route planned. If avalanche triggers, keep a 45d angle to escape, keep your altitude as snow below you can't burry you.
  3. Don't go first (try to go on tested terrain)
  4. Don't trust a cornice
  5. Obsess over consequences
  6. Start small (use a practice slope to test the snow)
  7. Communicate
  8. Have a belay rope
  9. Be equipped
  10. Terrain terrain terrain

wind slabs

Wind slabs are the worst. Wind loads snow much faster, and errodes it, making for a cohesive slab that can easily trigger. It overloads the pack.

They are recognisable because of their chalky white aspect, pillow on the snow, harder consistence, sound hollow, they feel slabby. If you encounter one, stop and turn around. Go to a safe spot and investigate

slabs

Slabs are made of

Weak layers are usually made of

Knowing that these exist makes you suspicious when they get burried under new snow.

Snow does not like rapid change, such as temperature, new snow, rain,...

Rapid change is usually the recipe for a slab. Increase in temperature or rain adds stress on weak layers because of percolation, and create wet slabs.

Storm slabs form due to new snow, and usually settle within a day

signs

Pole test

Bury your pole to feel for weak layers. Potentially use the handle side for hard snow. If hard then soft, it's the sign of a slab. Stop and investigate.

track test

Go above the track, then try to trigger a mini slab to see how the snow handles

Compression tests

Perform on surface, then deep (DCT). dug a pit. Isolate column of 30cm by 30cm. Cut the back. Perform tests.

Shovel sheer

Indicates where in a snowpack a sheer fracture could happen

If fracture happens at the bottom, repeat deeper. If fracture happens at different level on both test, or effort is different, repeat elsewhere.

Note effort required to fracture: easy, medium, hard.

Hand sheer

Same as shovel sheer, but with hand and easy to do. Isolate a 30x30 colum, 40cm deep.

Note fracture level and effort required.

Rutschblock (Rouge block)

Perform on at least 25deg and preferably 30deg and steeper. Isolate a block 2m * 1.5m upslope. If using a cord or saw, build a trapeze to make sure. If digging sides it doesnt matter. Reach below any weak layer (e.g 1.5m deep). Place 2 probes on top 2 corners and use a cord to cut, or use ski poles / skis, or dig.

Result vary on loading step. Score depends when the layer slides.

  1. Slides during isolation
  2. Tester gently steps on block with skis, within 35cm from upper wall.
  3. Bent legs without jumping
  4. Jump on same spot
  5. Jump again on the same compacted spot
  6. Step another 35cm to approx mid block with skis, jump 3 times.
  7. Didn't slide. Release type:

references

[1]: Bruce Temper / avalanche essentials