Avalanches Flashcards
What is an avalanche?
They are flows which move under the influence of gravity
They can be channelized or unconfined
In this sense, they are similar to pyroclastic flows, debris flows, etc.
Effects of Avalanches
Direct effects:
Impact
Burial
Indirect effects:
Tsunamis generated if an avalanche enters a lake
The Path of an Avalanche
3 parts:
Starting Zone
Track
Run out Zone
Avalanches follow the topography, usually form and are pushed through gulleys
How avalanches occur
Shear Strength: Internal resistance to movement
Shear Stress: Force causing movement parallel to the slope, increases with slope angle
Safety Factor= (Shear Strength/Shear Stress)
If the safety factor is less than one, the slope is unstable and prone to failure
Gravity:
Gp is the gravity that right angles the slope
Gs is the gravity that parallels the slope
As slope angle increases, Gp decreases and Gs increases
Once Gs exceeds shear strength, the mass fails
Two types of initial failure
Loose Snow Avalanche: Loose snow running over the slope, less dangerous
○ Snow is dilute
Slab Avalanche: More dangerous
○ Snow is denser, less mixing with atmosphere
Avalanches are more likely to form at a 35 degree slope
Structure of an Avalanche
→ Head is twice the height of the rest of the avalanche
○ Its mixing with the air form the atmosphere (slows it down)
○ Material is flowing form the body to the head, making it denser
→ Different parts of the flow are moving at different velocities, the head is moving fastest
→ Also there is a vertical difference in snow density
○ The lower portion is usually denser and more hazardous
○ The upper portion is more dilute, but still turbulent
Two Types of Avalanches
Flow avalanches: Originate from slab failure Slower than powder avalanches Granular Flow Extremely dense Freezes upon settling because of particle movement which heats it up Do not flow around obstacles
Powder Avalanches
Originate form loose snow failure
Velocities can exceed 360 km/hr
Composed of a mixture of air and snow which makes it less dense
Turbulent Flow
Flow around obstacles because upper more dilute portion acts as a fluid
Causes of Avalanches
Most triggers for avalanches involve human activities (skiing, snowboarding, ice climbing)
The number of fatalities from avalanches has been increasing
Dry slabs and leeward slopes are most prone to avalanches, where an overhanging cornice indicates leeward exposure
If you aren’t found within 20-30 minutes, your chances of survival decrease significantly
Mitigation
Avoid steep slopes, gullies
Close high-hazard areas to reduce risk and vulnerability
Set off explosive charges to artificially induce avalanches and remove the source material (unstable snow)
Use reforestation to stabilize slopes and snow
Use of defense structures