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...Avalanche Triggers...

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STRESS VS. STRENGTH


Snow on an incline is in a constant tug-of-war. Think of the slab as a "dinner plate" of snow on the slope. The forces that hold that snow slab in place include tension at the crown (top), compression at the stauchwall (bottom) and shear friction at the bed surface and flanks (sides). On the other side, the major force encouraging the slab to move is gravity.

Snow is said to be a "visco-elastic" substance, basically meaning that it can behave as a liquid or a solid. It's choice of behavior is determined by the rate of strain--i.e. the snowpack can withstand a much larger strain without avalanching if the load is applied slowly. Think of an elastic band or chewing gum on a cold day (other visco-elastic substances): they will stretch if pulled slowly, but will break if rushed.

Like the stretched elastic band, the snow slab will not break and will stay where it is as long as the strength of the forces holding it in place is greater than the stress of the forces pulling it downhill. Sometimes, this balance is very tenuous, indeed.

With this in mind, the idea of a "trigger" becomes crystal clear: a snowpack that is narrowly balanced between stress and strength can go one of two ways--either it will adjust to it's load over a period of time, or something abrupt will happen to tip the scale, causing an avalanche.

This "something" is called a trigger and can be natural or artificial. Professional avalanche workers cataloguing avalanche activity attempt to record the trigger whenever possible. The following are some examples of triggers and their recording codes:

 

Trigger: Artificial-Other...

ARTIFICIAL TRIGGERS:
Skier AS
Snowboarder AB
Explosive:
  Hand-Charge
  Artillery
  Avalauncher
 
AE
AA
AL
Cornice fall AC
Other: (examples of past artificial triggers)
  coyote
  elk
  snowmobiles
  climbers
  snowcats
AO

 

NATURAL TRIGGERS:
Snowfall N (Natural releases are generally not differentiated for record- keeping purposes)
Wind-loading
Rain
Rapid temperature increase
Tidal pull (controversial)

 

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