--- title: "avalanche" tags: - --- link: https://www.youtube.com/watch?v=-luspmL_f1o - Lower risk - Avoid avi terrain - safety gear - what to consider - using a guide Reducing risk - total avoidance (dont go backcountry at all) - avoidance lite (avoid all avalanche terrain) - recognising risk, accepting it, minimizing exposure - use bulletin avoidance - stay in bounds/on piste - use low angle slopes - steep: 30-45 degrees minimize exposure to risks - know if you are in avalanche terrain - maps, guidbooks, photos - clinometers - _quality_ level 1 course Use the bulletin forecast - low - moderate : natural avalanches not likely, man made avalanches possible if you ski in the wrong spot - considerable: if you ski in the wrong spot, human triggered avalances are likely no overhead hazard: not below a large face or something avalanche problem: - persistent weak layer - wind drifted snow whumpfs under skis: collapsing snow, avalanches likely ## Video 2 link: https://www.youtube.com/watch?v=1r0YIgdjm6M lots of different types of avalanche. loose vs slab, wet vs dry. usually: strong snow over weak snow. strong: often wind effect: ltighly bonded grains weak: light snow with no wind and cold clear nights important: slope angle ## Snowpack tests link: https://www.youtube.com/watch?v=OvwhuP4qtQg - compression test - locating instabilities near surface - 30(upslope not horixontal) x30cmx110cm () - ![](https://i.imgur.com/ebmXC6M.png) - tap 10 times with finger tips - mark factures as easy - level column - tap 10 times with finger tips from elbow - level - tap with hand or fist from shoulder - ![](https://i.imgur.com/2sCLTuz.png) - ![](https://i.imgur.com/YT6hWpT.png) - facture types video: http://vimeo.com/30996756 - deep tap test - similar to compression test but tests only for weak persistent layer relatively deep in the snowpack - extended column test - same as compresion test but 90cm wide not just 30cm - ![](https://i.imgur.com/itugyJ1.png) - rutschblock test - ![](https://i.imgur.com/FnocAmt.png) - propagation saw test - shovel shear test - hand shear test equipment - shovel - probe - snow saw - ruler - cord ## uptracking and route selection link:https://www.youtube.com/watch?v=RAXgSoSUD3Y avalanche triangle: snowpack, terrain, weather. terrain - ![](https://i.imgur.com/31KOLSD.png) - 5 red flags: "natures freebies" - recent avalanches - shooting cracks - recent wind loading - recent snow - thaw, snow snails - debris in creeks snowpack - ![](https://i.imgur.com/huT2fni.png) weather - ![](https://i.imgur.com/7zMk1mx.png) alptruth - ![](https://i.imgur.com/EIoOczr.png) stay far apart so you dont all get trapped. uptracking - ![](https://i.imgur.com/fs8b8Vm.png) - use google earth steepness - ![](https://i.imgur.com/TNsm8Wd.png) - caltopo - hill map 100 with hand vs 1 snow pit human factor - familiarity: assuming this are safe because they have been in the past - acceptance: allowing desire for acceptance (of others) to override decision making process - consistency: fear of appearing indecisive, - expert halo: deferring automatically to the expert - tracks/scarcity:allowing desire to have your day out to influence decisions **develop a routine** ## Weather and snowpack: slab avalanche formation avalanches are about timing: know when to go terrain is like a railway track: safe or not safe snowpack - can the snow slide - layered snowpack - ingredients - slope - slab - weak layer - trigger - also - initiation - propagation - weak layers - new snow - storm - wind - direct-action: hours-days - persistent weak layer - depth hoar - surface hoar - near-surface facets - persisten: weeks-months - temp changes during storm can create instabiliies - upside down: cold then warms up - right side up: warm then cools - ![](https://i.imgur.com/7zoi5Z7.png) - weak layers between storms - more persitent hazard - depth hoar - easy to see when you dig deep enough - fall apart in hands - sugary - ![](https://i.imgur.com/TvBlaC0.png) - deep in the snowpack - forms the base of the snowpack - forms early season - formed by thin early season snowpack and cold temps - ![](https://i.imgur.com/bPduxfH.png) - creates vapour pressure gradient / temperature gradient - ground is about 0 degrees c - surface is similar to air temp e.g., -10c - 10c per m gradient - with a shallow snowpack and the same temps. the gradient is higher, causing _faceting_ creating sugary crystals - deeper snowpack lessens the gradient - less rapid vapour transfer - - near surface facets - hard to see - small grains with sharp angles - develop near surface during cold clear nights and warm sunny days - surface hoar - frozen dew - large feathery crystals - deposition of moisture on snow surface - ![](https://i.imgur.com/pvsVjwG.png) - ![](https://i.imgur.com/g3zwefO.png) weak ≠ unstable (weak + slab + steep) loading - new snow - rate of loading is important - 2 feet overnight is bad - 2 feet over a week is good - wind - can be 10 times faster than from sky - cornices - large drifts - harder snow - rain - adds weight and stress and destabilises looking at weather: - bullseye data - recent loading - recent avalances - shooint cracks - rapid warming - collapsing ![](https://i.imgur.com/qrlmp8g.png) snow pits only give you one data point spatial variability exists snow on the ground in always changing strong over weak = BAD rapid change = BAD