snow mechanics / avalanche dynamics

25
©2000-2002 Mike Snow Mechanics/Avalanche Dynamics

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Page 1: Snow Mechanics / Avalanche Dynamics

©2000-2002 Mike Laney

Snow Mechanics/Avalanche Dynamics

Page 2: Snow Mechanics / Avalanche Dynamics

©2000-2002 Mike Laney

Objectives – can you:

• describe how gravity, temperature and slope angle affect the snow pack over time?

• identify potential stress points in the snow pack?

• describe differences between point and fracture initiation?

Page 3: Snow Mechanics / Avalanche Dynamics

©2000-2002 Mike Laney

Triangle factors interact dynamically to produce avalanches

Snow

Snow

pack

pack W

eather

Weather

TerrainTerrain

Page 4: Snow Mechanics / Avalanche Dynamics

©2000-2002 Mike Laney

Avalanches occur when the strength of the snow pack is overcome by stress to

produce failure.

Stress Strength

Page 5: Snow Mechanics / Avalanche Dynamics

©2000-2002 Mike Laney

Snow Pack Stress

Page 6: Snow Mechanics / Avalanche Dynamics

©2000-2002 Mike Laney

Factors that add/reduce stress• Add stress or

weaken strength*– Loading– Slope angle– Contour– Diurnal temp.

change– Free water flow– Metamorphism

(faceting)

• Reduce stress or add strength*– Surface Friction– Settlement– Anchors– Metamorphism

(rounding)– Internal motion

(deformation)

Page 7: Snow Mechanics / Avalanche Dynamics

©2000-2002 Mike Laney

Gradual loading increases settlement. Rapid loading leads to brittle failure

Page 8: Snow Mechanics / Avalanche Dynamics

©2000-2002 Mike Laney

Rapid Loading Awakens the Dragon

Page 9: Snow Mechanics / Avalanche Dynamics

©2000-2002 Mike Laney

Microclimate Loading Can Be Extreme

Page 10: Snow Mechanics / Avalanche Dynamics

©2000-2002 Mike Laney

Energy exchange (as heat)

Page 11: Snow Mechanics / Avalanche Dynamics

©2000-2002 Mike Laney

Internal motion

Page 12: Snow Mechanics / Avalanche Dynamics

©2000-2002 Mike Laney

Stress Points

• Isolated anchors• Contour changes• Rock interfaces• Sun lines

• Pillows• Slab Margins• Brush

Page 13: Snow Mechanics / Avalanche Dynamics

©2000-2002 Mike Laney

Contour stress

Page 14: Snow Mechanics / Avalanche Dynamics

©2000-2002 Mike Laney

Rock Rock InterfacesInterfaces

Page 15: Snow Mechanics / Avalanche Dynamics

©2000-2002 Mike Laney

Anchors

Page 16: Snow Mechanics / Avalanche Dynamics

©2000-2002 Mike Laney

Anchors get covered

Page 17: Snow Mechanics / Avalanche Dynamics

©2000-2002 Mike Laney

Avalanche Dynamics

• Loose Snow Releases• Wet Snow Releases• Slab Releases

Page 18: Snow Mechanics / Avalanche Dynamics

©2000-2002 Mike Laney

Loose Avalanche Release

Page 19: Snow Mechanics / Avalanche Dynamics

©2000-2002 Mike Laney

Consequential factors

Page 20: Snow Mechanics / Avalanche Dynamics

©2000-2002 Mike Laney

Slush /Wet

Release

Page 21: Snow Mechanics / Avalanche Dynamics

©2000-2002 Mike Laney

Slab Release

Slab?• Consolidated

snow• Cohesive new

snow

Weak Layer?• Graupel• Surface Hoar• Rime• Facets• Crusts

Trigger?•Rapid loading

•Rapid Temperature Change

Page 22: Snow Mechanics / Avalanche Dynamics

©2000-2002 Mike Laney

The trigger is the event that tips the balance between strength and stress.

Stress Strength

Stress Relief

Page 23: Snow Mechanics / Avalanche Dynamics

©2000-2002 Mike Laney

Page 24: Snow Mechanics / Avalanche Dynamics

Avalanche Characteristics by Climate Zone

Factors Maritime Intermountain ContinentalAltitude 4,000-7,000 7,000-11,000 10,000-14,000

Cumulative Snowfall

600” + 400” 250”

Storm Snowfall Many 12”+ Some 12”+ Few 12”+

Temperature Seldom<0oF <0o & >32oF <32oF

Wind Moderate Strong Very strong

Usual Type of Avalanche

Slab (damp-wet) Slab (damp-dry) Slab (dry)

Release Direct Direct Often Delayed

Example Squaw Valley, CA

Alta, UT Berthoud Pass, CO

Page 25: Snow Mechanics / Avalanche Dynamics

©2000-2002 Mike Laney

Recap: Strength vs. Stress

• Properties of snow• Stress• Strength factors• Stress relief