Title: An Advanced Shape of Country Classifier
1An Advanced Shape of Country Classifier
The Extraction of Surface Features from DEMs
- Lee P. Herrington
- State University of New York
- College of Environmental Science Forestry
- Gerald Pellegrini
- Advanced Development, BAE Systems
2Overview
- What is shape of country
- What is it used for
- Previous methods
- Our method
- Need and method of smoothing the DEM
- Analytic method
- Results Conclusions
3What is Shape Of Country?
- The low resolution classification of a DEM into
general features - Peaks, ridges, saddles
- Pits, valleys
- Various classes of side hills
- Saddle, convex, concave, planar, etc
- Do NOT want high resolution bumps dips in the
terrain!
4Scale of SOC
5Shape of Country(SOC)
- The TIN is a first approximation of SOC
- For our purposes we needed the following
categories of SOC.
Description
Class
Description
Class
Concave upward
Concave hillside
Cell ht gt than surround
Peak
Convex upward
Convex hillside
Cell htlt than surround
Pit
curve orthog 2 - curve
Saddle
Line of adjacent peaks
Ridge
Hillside w/ no curvature
Flat sur
Line of adjacent pits
Valley
Surface no slope or curvature
Flat
Intersection of ridge and valley
Saddle pt
6Uses of SOC
Tractability estimate When SOC combined
with DEM Surficial Geo Got 80-90 correct
classification in Adirondack mts.
- Estimation of
- Soil physical properties
- Chemical properties
- Soil moisture content
- Expert systems
- Forest harvesting
- Hydrologic studies
- Engineering
7Overview
- What is shape of country
- What is it used for
- Previous methods and results
- Our method
- Need and method of smoothing the DEM
- Analytic method
- Results Conclusions
8Previous Methods for SOC
- Usually hierarchical methods based on
relationships between adjacent cells of a DEM - A peak would be defined as a cell surrounded by
cells of lower elevation - A valley was a line of adjacent cells that had
cells of higher elevation on either side - Etc.
9Previous Methods for SOC
Pit or Peak
Ridge or valley
10A 30 M DEM (unsmoothed)
Approximate Drainage path
11Hierarchical classification
12Comparison
?
A
A
13Where we are going
14Overview
- What is shape of country
- What is it used for
- Previous methods
- Our method
- Need and method of smoothing the DEM
- Analytic method
- Results Conclusions
15Smoothing the DEM
- Usual average filtering using 3x3 and 5x5 kernels
- Did not work
- Filter roll off was not sharp enough and too much
short wavelength information leaked
16Roll off?
Sharp cutoff filter
1
Average Filter Roll off
Energy passed
Leakage
0
Spatial frequency (1/wavelength)
17Smoothing the DEM
- Usual average filtering using 3x3 and 5x5 kernels
- Did not work
- Filter roll off was not sharp enough and too much
short wavelength information leaked - Implemented a sharp roll off filter using the
Fourier Transform actually the FFT - FFT transforms data in the spatial domain (DEM)
into the spatial frequency domain
18Domain idea
19Domain idea
20Surfaces as summations of sinusoids
Summation of sinusoids
Elevation
1 2 3
Distance ?
Spatial Frequency Domain
Distance domain
21Domain Change
- From the Distance domain
- To the Spatial frequency domain
- And back
- How?
22Fourier to the rescue!
- The FOURIER TRANSFORM is a mathematical process
used to convert between domains - You dont want to see the equations!!!
- The FAST FOURIER TRANSFORM or FFT is digital
processing technique that makes the Fourier
Transform practical - Goes both ways
- Space to frequency FFT, frequency to space FFT-1
23 Fourier Transform
INVERSE TRANSFORM
24Distance Domain
Raw 30m DEM (vertical Exaggeration )
25Processing
FFT
Raw 30m DEM
26Smoothed 30m DEM, Classified
Resulting Smoothed 30 m DEM (with SOC classes)
27Same information content!
Spatial Frequency domain
Distance domain
28OK, we have a smoothed DEM
- Now we need to create a classification of the
surface - And this is really Gerrys contribution
29Analytic (Continuous) Method
- Pass a 3x3 kernel over the DEM fitting a
polynomial surface to the 9 points - This yields a mathematical description
- Slope, aspect, and curvature (profile and plan
- Identify basic features based on above
- Construct terrain features based on comparison of
properties of each cell
30Zevenbergen Thorns polynomial
31The problem
- Eigenvalue analysis used to generate the 1st
estimate of shape - BUT!
- Grid features may not be aligned with major SOC
features - If a ridge line does not pass exactly through the
center of a cell then the cell will be seen as a
side hill
32Alignment Problem
Fitted surface
elevation
All cell classed as side hills at center of the
cell
distance
33Solution
- Mathematically determine if there is a change in
slope within the pixel from the equation fitted
to the 3x3 kernel - If so, generate new eigenvalues
- Use a table lookup routine based on both the
original and recalculated eigenvalues to classify
the cell
34Analysis Flow Chart
35Overview
- What is shape of country
- What is it used for
- Previous methods
- Our method
- Need and method of smoothing the DEM
- Analytic method
- Results Conclusions
36Results
- Smoothing and analysis technique applied to
- Analytic surfaces
- Real world DEMs
- It worked!
37Analytic Saddle
Saddle surface
Classification
38 30m DEM
39Conclusions
- A combination of
- Smoothing with a sharp cutoff filter in the
spatial frequency domain - The use of a continuous analytic fitting process
- The determination of the actual location of the
feature within a cell
40Conclusions
- A combination of this technique in with
hierarchical processing and analysis of the
original DEM may be a route to even better
classifications.