Notes
Outline
Incorporating Landslide Probability into Forest Operations Planning
Finn Krogstad
University of Washington
Landslides are hard to predict
Soil, rain, vegetation, topography,...
Landslide models give “hazard”
Rearranging gives:
SHALSTAB - Critical Rainfall
dSLAM  - Factor of Safety
LISA - Probability of Landslide
which are all correlated with landsliding
A simpler approach
Classifying hillslopes by
local slope and curvature:
SMORPH - Hazard
 This is not what we need to know
Hazard based management says:
Slope 1 is less stable than slope 2.
What we really want to know:
Is plan 1 better than plan 2?
Is plan 1 okay?
Surface Erosion is also Complicated
Soils
Storms
Traffic
Vegetation
Slope
...
This Doesn’t Prevent Modeling
Input road properties
Output erosion
The Trick:
Average over variability
Explicitly
WEPP
Implicitly
SEDMODL
USLE
We need to do the same thing with Landslides.
Averaging Over Landslides
Use observations of landsliding on similar hillslopes to estimate landslide fraction or ‘probability’
p = #landslides / #hillslopes
(if #hillslopes is large)
Averaging Over Landslides
What is a ‘Hillslope’?
Slides/Acre
Slides/Hectare
Slides/Grid square
What is ‘similar’?
Topography
management
Estimating Probability
Each hazard and activity
phn=Lhn/Hhn
Predicting Future Landsliding
If
pmr=Lmr/Hmr
Then
Lmr=pmr*Hmr
How many more landslides
If you add a spur road and harvest:
What is the landslide probability before?
What is the landslide probability after?
The difference is due to management activity.
The sum is the expected number of landslides.
Probability of Individual Outcomes
Combining Independent Events
Pr(A or B)
Combining any number of independent events
Watersheds Accumulate
Landslides Flow Downhill:
Pr(blowout at X)=Pr(landslide upslope of X)
Limited Complexity of Ratios
Bigger table: more cells: more uncertainty
More dimensions:  More uncertainty
Continuous vs. Discrete Hazard
Many hillslope have continuous properties
Slope
age
retention
contributing area
soil cohesion
root reinforcement
...
Logistic Regression
Regression is a powerful tool:
      y=a+bx+e
Probability takes [0,1] values
Computers handle the math
Logistic Approach
Fitting parameters from past landslides
Allows prediction of future landslides
Conclusion
Current landslide models poorly guide management decisions.
If we consider average landsliding:
Estimate from past landsliding
Predict future:
landscape average landslide numbers
probability of local event
Logistic regression adds flexibility