Terrain Susceptibility Kyle Renner GIS in Water Resources 2015

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Presentation transcript:

Terrain Susceptibility Kyle Renner GIS in Water Resources 2015 Avalanche Risk Terrain Susceptibility Kyle Renner GIS in Water Resources 2015

Avalanche Definition and Facts ‘a rapid flow of snow down a sloping surface as a result of snowpack failure.’ Failure occurs when load (weight of snowpack) exceeds strength Avalanches are expected in every mountain range, every winter season Avalanches kill more than 150 people worldwide annually Slab avalanches can reach speeds of 80 miles per hour within 5 seconds and are the most destructive form of avalanche.

Major Avalanche Types Loose Slab Powder

Avalanche Factors Weather Snow Conditions Terrain Temperature Recent Snowfall Wind Snow Conditions Snowpack depth Terrain Slope Slope Profile – Curvature Aspect Land Cover

Current Risk Assessment Methods North American Public Avalanche Danger Scale (US) Used primarily by recreationalists, must be updated by recreation managers

Forecast Model, Limited Coverage

A new perspective: Terrain Analysis An analysis of terrain conditions that lead to an avalanche given appropriate weather and snow conditions. Can be used to identify at risk locations by planners, developers, or managers. Example: a home owner wishes to insure a home, insurance company can cite the location of the house within an at risk area for an increase in insurance costs. A model that incorporates Slope, Aspect, Curvature, and Land Cover.

Slope, Aspect, Curvature, Land Cover Shallow slopes require more weight to cause failure (<25°) Steep slopes struggle to accumulate snow (>60°) Aspect influences temperature, a colder snowpack = prone to failure Northern Slopes receive less sunlight, maintain colder snowpack Convex slopes create tension zones in the snowpack Barren land coverage lacks friction capabilities Dense land coverage provides anchor points to increase snowpack strength

Model Inputs Elevation Data: 3D Elevation Program (3DEP), USGS National Map, Elevation Available in various formats – 1/3 arc-second seamless DEM recommended Available at http://nationalmap.gov/elevation.html Land Cover Data: National Land Cover Database (2011) Spatial Resolution of 30 meters 16- class land cover classification based on Landsat satellite data. Available at http://www.mrlc.gov/nlcd2011.php Also available through ArcGIS Server: Landscape 5 Area of Interest: County, State, or any other usable polygon *Data must be orthogonal in order to work correctly Decision-tree classification of 2011 Landsat satellite data

Tools Elevational Data will be the input raster in several tools Slope Tool- the rate of maximum change in the z-value (elevation). Expressed as degrees ranging from 0 to 90. Aspect Tool- identifies the downslope direction of the maximum rate of change. (Slope Direction) Curvature Tool- curvature is the second derivative of the surface, or the slope of the slope. Optional output curvature types are profile curvature, the direction of the maximum slope, and the plan curvature is perpendicular to the direction of the maximum slope.

Reclassifications All four layers reclassified to a value of between 0 and 3. A value of zero corresponds to a extremely unlikely chance of a slide occurring in the given conditions (example: open water land classification). A value of three indicates an extremely likely chance of a slide occurring, such as in the case of a slope between thirty and forty-five degrees or over barren land. Values of one or two will indicate low or moderate risk.

Land Classification Reclassification Table Value Open Water Dwarf Scrub (Alaska Only) 2 Perennial Ice/Snow 3 Shrub/Scrub Developed, Open Space Grassland/Herbaceous Developed, Low Intensity Sedge/Herbaceous Developed, Medium Intensity Lichens (Alaska Only) Developed, High Intensity Moss (Alaska Only) Barren Land Pasture/Hay Deciduous Forest 1 Cultivated Crops Evergreen Forest Woody Wetlands Mixed Forest Emergent Herbaceous Wetlands Legend and Description available at http://www.mrlc.gov/nlcd11_leg.php

Slope, Aspect, and Curvature Reclassification Between 30-45 degrees – 3 (high risk) Below 25 degrees, Above 60 degrees – 1 (low risk) Aspect: Northern – 3 (high risk) Eastern – 2 (moderate risk) Southern, Western – 1 (lower risk) Curvature Convex – 3 (more likely) Concave – 1 (less likely)

Risk = Σ[ slope + aspect + curvature + land-cover ] The following equation will then be utilized using Map Algebra: Risk = Σ[ slope + aspect + curvature + land-cover ] -or- Risk = (0.4)(slope reclassification) + (0.15)(aspect reclassification) + (0.2)(curvature reclassification) + (0.25)(land cover reclassification) An output raster displaying the ‘Avalanche Risk Scale’ A value of 0 indicates no risk A value of 1 indicates low risk A value of 2 indicates moderate risk A value of 3 indicates extreme or high risk Importance Coefficient

Limitations and Assumptions This model predicts only the terrains impact on avalanche risk. Appropriate weather and snow conditions are necessary for a slide. This model’s coefficients are estimated using prior research to gauge importance of the contributors (variables). This model has an arbitrary reclassification based upon prior knowledge and choice upon whether a certain condition would have no, low, moderate, or extreme risk of contributing to a slide Spencer Logan, Forecaster, Colorado Avalanche Information Center- subjective rating and descriptors are the best way researchers have found to quantify avalanche risk. The observational data is not available to attempt to model risk in a statistically valid way.

Case Study – Lake County, Colorado Inputs- Lake County Boundary shapefile obtained from 2010 Census Data 2011 National Land Cover Dataset 1/3 Arc-Second DEM available from USGS, Lake County

Process

Results

Further Work, Additional Research Setting an appropriate threshold for the avalanche risk scale can produce an at risk area This area can be used as an input for other tools such as the D-Infinity Avalanche Runout tool http://hydrology.usu.edu/taudem/taudem5/help53/DInfinityAvalancheRunout.html Displays the area of the avalanche path Upon the acquisition of appropriate data, a regression analysis could be ran to determine appropriate coefficients Further research could be conducted to provide better reclassification guidelines Better coding and understanding of computer language

QUESTIONS?