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CS 128/ES 228 - Lecture 13a 1 Surface Analysis

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Surface Analysis . Network Analysis. Given a network What is the shortest path from s to t ? What is the cheapest route from s to t ? How much “flow” can we get through the network? What is the shortest route visiting all points?. - PowerPoint PPT Presentation

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Page 1: Surface Analysis

CS 128/ES 228 - Lecture 13a 1

Surface Analysis

Page 2: Surface Analysis

CS 128/ES 228 - Lecture 13a 2

Network Analysis Given a network

What is the shortest path from s to t? What is the cheapest route from s to

t? How much “flow” can we get through

the network? What is the shortest route visiting all

points?

Image from: http://www.eli.sdsu.edu/courses/fall96/cs660/notes/NetworkFlow/NetworkFlow.html#RTFToC2

Page 3: Surface Analysis

CS 128/ES 228 - Lecture 13a 3

Network complexitiesShortest path EasyCheapest path EasyNetwork flow MediumTraveling salesperson

Exact solution is IMPOSSIBLY HARD but can be approximated

All answers learned in CS 232!

Page 4: Surface Analysis

CS 128/ES 228 - Lecture 13a 4

When is an Elevation NOT an Elevation? When it is rainfall, income, or any

other scalar measurement

Bottom Line: It’s one more dimension (any dimension!) on top of the geographic data

Page 5: Surface Analysis

CS 128/ES 228 - Lecture 13a 5

How do we display a map with “elevation”?

Choropleth map

Contour map

Surface map

Page 6: Surface Analysis

CS 128/ES 228 - Lecture 13a 6

Choropleth maps Show areas of equal “elevation” in a

uniform manner

Are usually “exact” approximations (through aggregation)

Subject to classification issues

Often intimately connected to queries

Page 7: Surface Analysis

CS 128/ES 228 - Lecture 13a 7

Simple uses of choroplethsOrdinal

Population

Per capita income

Crop yield

Categorical

Soil type

Political party control

Primary industry

Page 8: Surface Analysis

CS 128/ES 228 - Lecture 13a 8

Display issues for choropleths Classification

Type

Number of intervals

Colors

Page 9: Surface Analysis

CS 128/ES 228 - Lecture 13a 9

How do we select choropleth regions?

Based on existing polygons

Based on dissolved polygons

Based on nearest points

Page 10: Surface Analysis

CS 128/ES 228 - Lecture 13a 10

A Choropleth you built

Page 11: Surface Analysis

CS 128/ES 228 - Lecture 13a 11

More complex queries using choropleths Time series data

Population change % of land in agricultural use

Computation driven Total spending power = Average income x population Average wheat yield = Total yield / Acreage of farms

Page 12: Surface Analysis

CS 128/ES 228 - Lecture 13a 12

Basic model for “computed choropleths” Create new attribute data (usually

within attribute table; sometimes with selection layer)

Set the display to key off that new data

Choose remaining display options

Page 13: Surface Analysis

CS 128/ES 228 - Lecture 13a 13

A riddle (sans funny punch line) What is the difference between a

choropleth map and a 2-D query such as “how many points are in this polygon”?

A fine (boundary) line

In truth, it is a matter of style of output.

Page 14: Surface Analysis

CS 128/ES 228 - Lecture 13a 14

Review of surface approximation “dimensions” Local vs. Gradual

Exact vs. Approximate

Gradual vs. Abrupt

Deterministic vs. Stochastic

Page 15: Surface Analysis

CS 128/ES 228 - Lecture 13a 15

Thiessen polygons Local

Exact

Abrupt

Deterministic

Page 16: Surface Analysis

CS 128/ES 228 - Lecture 13a 16

More sophisticated surface generation (trend surface)

Use a “least squares”-

like technique

to fit a surface to the data

Page 17: Surface Analysis

CS 128/ES 228 - Lecture 13a 17

Trend Surfaces

Global Approximate (in most cases) Gradual Deterministic

Better quality obtained by using higher order surface, but takes longer

Page 18: Surface Analysis

CS 128/ES 228 - Lecture 13a 18

Inverse distance interpolation

Value of a point is related to the sum of the values of all other points divided by their distance from the given point

Page 19: Surface Analysis

CS 128/ES 228 - Lecture 13a 19

Inverse distance

Global (but effectively local)

Approximate (but close to exact)

Gradual Deterministic

Can use different functions, e.g. inverse distance squared

Page 20: Surface Analysis

CS 128/ES 228 - Lecture 13a 20

Spatial moving average

Global (but heavily local)

Approximate (but close to exact)

Gradual

Deterministic

Page 21: Surface Analysis

CS 128/ES 228 - Lecture 13a 21

“Realistic” surface modeling Requires approximating

“Show the impression, not the data”

Often involves slope and aspect

Commonly used for shading maps

Page 22: Surface Analysis

CS 128/ES 228 - Lecture 13a 22

Building “shade” Shaded maps intrinsically include a

“camera” and a “direction”

For “perspective”, color is determined using the dot product (trigonometry alert) of the value of the normal (aspect) and the camera vector (line of sight)

Page 23: Surface Analysis

CS 128/ES 228 - Lecture 13a 23

Some shaded surfaces

Image from: Burrough & McDonnell, Principles of Geographic Information Systems, p. 192

Page 24: Surface Analysis

CS 128/ES 228 - Lecture 13a 24

Where has all the rainfall gone?

Image from: Burrough & McDonnell, Principles of Geographic Information Systems, p. 194

Page 25: Surface Analysis

CS 128/ES 228 - Lecture 13a 25

It’s not calculus Much analysis is done through “cellular”

computation

Conway’s game of Life is an example

http://www.bitstorm.org/gameoflife/

Use the gradient to move “cells” of water to show flow and/or flooding

Page 26: Surface Analysis

CS 128/ES 228 - Lecture 13a 26

More complex models To compute the irradiance, I, use the

following formula

I = [cos0cos + sin0sincos(0-A)]S0

x exp(-T0/ cos0)

where S0 is the exatmospheric solar flux, 0 is the solar zenith angle, etc.

Page 27: Surface Analysis

CS 128/ES 228 - Lecture 13a 27

Thoughts on surface analysis Surface analysis is handy, but

requires Moderately complex database queries,

or Moderately complex mathematics

Fortunately, much of this is “built-in” through wizards (e.g. buffer wizard)

Page 28: Surface Analysis

CS 128/ES 228 - Lecture 13a 28

Some thoughts on surface generation “There are three kinds of lies: lies, damned lies

and statistics” Benjamin Disraeli, popularized by Mark Twain

“Anyone can lie with statistics” Anonymous

“A picture can lie more effectively than words” Anonymous