3d and surface/terrain analysis in partnership with: with support from: nsf due-0903270 prepared by:...

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3D and Surface/Terrain Analysis in partnership with: With support from: NSF DUE-0903270 Prepared by: George McLeod Geospatial Technician Education Through Virginia’s Community Colleges (GTEVCC)

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3D and Surface/Terrain Analysis

in partnership with:

With support from:

NSF DUE-0903270

Prepared by:

George McLeod

Geospatial Technician Education Through Virginia’s Community Colleges (GTEVCC)

Digital Terrain Models• A digital terrain model is a model providing a

representation of a terrain relief on the basis of a finite set of sampled data

• Terrain data refers to measures of elevation at a set of points V of the domain plus possibly a set E of non-crossing line segments with endpoints in V

D

Data Sampling

• Regular

• Irregular

Sampling effects resolution

Our three Primary terrain Models

• Digital Elevation Models (DEMS) – aka Regular Square Grids (RSGs)

• Triangulated Irregular Networks (TINS) – aka Polyhedral terrain models

• Contour Maps – aka “topo” maps

The Data…

LIDAR (LIght Detection And Ranging)

DEM

TIN

• Terrain mapping• Land surface is 3-D • Elevation data or

z-data is treated as a cell value or a point data attribute rather than as a coordinate.

Introduction to the Data

• Digital Elevation Model (DEM)– Gridded array of elevation points obtained from a

variety sampling methods

DEMsA constant function can be associated with each square (i.e., a constant elevation value). This is called a stepped model (it presents discontinuity steps along the edges of the squares)

D

• The function defined on each square can also be a bilinear function interpolating all four elevation points corresponding to the vertices of the square

• Triangulated Irregular Network (TIN)– Series of non-overlapping triangles– Elevation values are stored at nodes– Sources: DEMs, surveyed elevation points, contour

lines, and breaklines– Breaklines are line features

that represent changes of the land surface such as streams, shorelines, ridges, and roads

TINs

• Example of a TIN based on irregularly distributed data

Data for Terrain Mapping and Analysis

• Triangulated Irregular Network (TIN)– Not every point in DEM is used– Only points most important– VIP (Very Important Points) algorithm– Maximum z-tolerance algorithm– Delaunay triangulation: all nodes are connected to

their nearest neighbor to form triangles which are as equi-angular as possible.

Tins vs. Grids

• Needs larger storage capacity

• Computationally difficult

• Flexibility of data sources

• Can add points

• Better display

• More efficient

• Needs smaller storage capacity

• Computationally simpler

• Fixed with a given cell size

• Cannot add sample points

• Raster display

• Less efficient

DEM TIN

Contour Mapping• Contouring is most common

method for terrain mapping• Contour lines connect points

of equal elevation (isolines)• Contour intervals represent the

vertical distance between contour lines.

• Arrangement of contour lines reflect topography

Digital Contour Maps

Contours are usually available as sequences of points

A line interpolating points of a contour can be obtained in different waysExamples: polygonal chains, or lines described by higher order equations

Digital Contour Maps: properties

They are easily drawn on paper

They are very intuitive for humans

They are not good for complexautomated terrain analysis

Contour Profile Mapping• Vertical profile shows changes in elevation along a line, such as a hiking

trail, road or stream.

Cartographic Terrain Mapping• Hill shading is also known as a shaded relief or simply shading• Attempts to simulate how the terrain looks with the interaction between sunlight

and surface features.• Helps viewers recognize the shape of land-form features on a map.

Hillshading

• Four factors control the visual effect of hill-shading– Sun’s azimuth is direction of incoming light (0 to

360°)– The sun’s altitude from horizon (0-90°)– Surface slope (0-90°)– Surface aspect (0 to 360°)

Hypsometric Tinting• Hypsometric tinting

– Applies different color symbols to represent elevation or depth zones.

Methods of Analysis • Slope measures the rate of change of elevation at a surface location

• Aspect is the directional measure of the slope (degrees- 4 or 8 directions)

• Hillshade, refer to previous slides

• Line of sight refers to the straight line visibility from an observer to a feature

• Viewshed analysis refers to the areas of the land surface that are visible from an observation point or points.

• Watershed analysis refers to an area that drains water and other substances to a common outlet.

• Area and volume calculations

Connectivity Function Example:Viewshed Analysis

Image Source: Chrisman, Nicholas.(2002). 2nd Ed. Exploring Geographic Information Systems. p 198. fig. 8-14.

Line of Sight Analysis

Slope

Aspect

Hillshade

Setting a hypothetical light source and calculating the illumination values for each cell in relation to neighboring cells. It can greatly enhance the visualization of a surface for analysis or graphical display.

Azimuth 315°, altitude 45°

Viewshed• Viewshed identifies the cells in an input raster that can be seen from one or

more observation points or lines.• It is useful for finding the visibility. For instance, finding a well-exposed places

for communication towers

hillshaded DEM as background

Surface Area and Volume

Application: Environmental Impact Analysis

3D landscape model impact on natural beauty

Application - Flood Risk

3D height data changing water levels-danger areas

The 3rd Dimension: Height Analysis – combining several methods together

• Contours • Hill shading • Spot height symbols • Cliff & slope symbols • Viewpoint symbols

3D Terrain Analysis: Summation

• GIS does not always provide exact answers to problems, but by identifying trends based on geography, GIS can reveal patterns that can help us make informed decisions.

• A GIS can improve decision-making; it cannot make decisions for us.