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Geography 360 Principles of Cartography

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Title: Geography 360 Principles of Cartography


1
Geography 360Principles of Cartography
  • May 1517, 2006

2
Outlines Isarithmic map
  • Two kinds of isarithmic map
  • Isometric map from the true point data
    (continuous fields)
  • Isopleth map from the conceptual point data
    (statistical surface)
  • Three interpolation methods
  • Regular control points to gridded surface (e.g.
    IDW, Kriging)
  • Irregular control points to triangulated surface
    (e.g. triangulation)
  • Map display of interpolated data (2.5D map
    display)
  • Vertical view contour, hypsometric tint
  • Oblique view fishnet map, block diagram
  • Physical model

Reading Slocum chapter 14 15
3
What is isarithmic map?
  • It depicts continuous smooth phenomenon
  • Temperature, elevation, rainfall, average day of
    sunshine, barometric pressure, depth to bedrock,
    earths topography, and statistical surface

4
  • 1. Two kinds of isarithmic map

5
Two kinds of data
  • True point data
  • Data is actually measured at the point location
  • e.g. The location of weather station for
    temperature map
  • This kind of map is called isometric map
  • Conceptual point data
  • Data is collected over areas, and the map is
    constructed by interpolating given values at the
    centroid of areas
  • e.g. The location of census tract for murder rate
    map
  • This kind of map is called isopleth map

6
Data types and isarithmic form
Dent 1999
7
How isopleth map is created
Image source Electronic reading Nyerges
8
Isometric or isopleth map?
  • Think how data is collected

Current temperature in the US
Voting behavior in the US
9
Isometric or isopleth map?
Toxic level
Demographic trends
Image source www.gis.com
10
Depicting population distribution in different
map types
  • Dot map total count in a large-scale mapping
  • Proportional symbol map total count in a
    small-scale mapping, where the point location is
    conceptual (e.g. state centroid)
  • Choropleth map standardized data of population
    (e.g. population density or cohort), where the
    goal is to compare between enumeration units
  • Isopleth map standardized data of population,
    where the goal is to reveal overall trends,
    screening effects of arbitrary enumeration unit
    boundary

11
Phenomenon, data, mapWorld, data structure, map
displayElevation, DEM, shaded relief
  • Toxic level map
  • Phenomenon toxic level
  • Data point data of toxic level at sample points
  • Map isometric map showing continuous fields of
    toxic level
  • Demographic trends map
  • Phenomenon elderly persons ( population over
    60)
  • Data point data of population density at the
    centroids of enumeration units (the smaller the
    better)
  • Map isopleth map showing statistical surface of
    demographic trends

The process of transformation from point into
surface?
12
  • 2. Three spatial interpolation methods

13
Spatial interpolation
  • We will call the data points (either true or
    conceptual) from which isarithmic maps are
    constructed control points (not a common term,
    but only for clarity purpose)
  • Spatial interpolation basically estimates unknown
    values from known values at control points
    guesswork generates a continuous surface from
    sampled point values (which are discrete data)
    because we know the phenomenon mapped is
    continuous
  • Is it valid to apply spatial interpolation to
    discrete phenomenon?
  • Figure 14.1 see how the manual spatial
    interpolation works (it illustrates a linear
    method)
  • Figure 14.4 see how different interpolation
    methods yield different-appearing maps how can
    we decide which method works the best given data?

14
Location of weather stations
Surface map constructed from inverse distance
method
Surface map constructed from Kriging
15
Spatial interpolation
  • There are two ways to represent continuous
    surface - one is a regular or gridded form, and
    the other is an irregular form
  • Regular control points to gridded surface
  • Inverse Distance Weighted (IDW) z f (h) where
    h is distance to control points
  • Kriging z f (h, v) r where v is the
    semivariogram model, and r is the residual (i.e.
    difference between model and observed value)
  • Irregular control points to triangulated surface
  • Triangulation z value is calculated from
    Delaunay triangle

16
Inverse Distance Weighted (IDW)
  • As the distance increases, you will inversely
    weight the values

Image source Bolstad 2005
See p. 274 for formula
17
Kriging
  • Similar to IDW in that
  • A grid is overlaid on top of control points, and
    the goal is to derive values at a grid point from
    control points
  • Values at a grid are determined by values at
    nearby control points weighted by inverse
    distance
  • Different from IDW in that
  • It builds the model of spatial autocorrelation
    from known values (called semivariogram), and
    the weights are determined such that observed
    values are best fitted into the specified model
  • By model-fitting mechanism, the estimated values
    are supposed to reflect the spatial structure of
    given data it also provides the way to validate
    the weights (e.g. standard error of the estimate)

18
Triangulation
  • Unlike IDW and Kriging, triangulation honors
    control points
  • Triangulation helps determine the edge from which
    values are interpolated
  • So how do we determine the best edges to work on?
  • It works this way (see Figure 14.3B at p. 274)
  • Draw Thiessen polygon from control points
  • Thiessen polygon equally divides the area of
    influence to each control point
  • Connect control points at neighboring Thiessen
    polygons to result Delaunay triangle
  • Delaunay triangle minimizes the length of edges
    formed by control points
  • Compare imaginary triangle IDE to ICE which is
    smaller?

19
Thiessen polygon
  • Creates an area of equal influence given point
    locations

20
Discussion review questions
  • Which spatial interpolation method do you think
    can handle discontinuity? (e.g. lake as flat
    plane instead of U-shaped gutter)
  • Which spatial interpolation method do you think
    will produce inconsistent results depending on
    parameters chosen (e.g. control points
    considered) compared to others?
  • Which spatial interpolation method do you think
    is considered a optimal method?

21
Which method to choose?
  • Triangulation honors the control point data, and
    can handle discontinuity (e.g. ridge, lake)
  • Pros it works well when control points are
    critical points
  • Cons angular contour
  • Inverse distance fast, simplicity of method
  • Pros easy to understand
  • Cons deterministic method (no uncertainty
    handling mechanism)
  • Kriging most rigorous method provided that the
    model is properly specified
  • Pros stochastic method (uncertainty handling),
    reflects overall spatial structure of data
  • Cons complexity of method, sensitive to model
    specification

22
Spatial interpolation in ArcGIS- Creating the
right surface map -
  • Spatial Analyst
  • Create contour from DEM
  • Be aware of a wide array of parameters to choose
    from
  • Geostatistical Analyst
  • Provides exploratory tools for choosing the right
    parameters or models, including cross validation
    methods

23
Image capture from Spatial Analyst
24
  • 3. Map display of interpolated data

25
2.5D vs. 3D phenomenon
  • So far we have worked on 2D map display of
    spatial entities (no height dimension)
  • Now we move on to 3D map display of spatial
    entities
  • What we commonly refer to as 3D map display can
    depict two categories as follows
  • 2.5D phenomenon (e.g. elevation) z value is
    single-valued Color plate 14.1 depicts height
    above a zero point
  • Z value is replaced by a single value of the
    theme mapped
  • e.g. Prism map showing population density
  • True 3D phenomenon (e.g. geological profile) z
    value is multi-valued Color plate 4.1 depicts
    geological materials underneath the earths
    surface
  • Different values can be assigned to each (x,y,z)
  • e.g. geological materials vary by (x,y,z)

Read Slocum p. 57
26
Displaying the interpolated data
  • Vertical view
  • From Gods eye view 90
  • Contour lines (Figure 14.16A)
  • Hypsometric tints (Figure 14.16B)
  • Hill shading (shaded relief) (Color plate 15.3,
    Color plate 15.2C)
  • Oblique view
  • From Birds eye view 090
  • Fishnet map (Figure 14.16C)
  • Block diagrams (Figure 15.17)
  • Physical model

27
Contour lines
  • Each contour line depicts the same elevation

28
Hypsometric tint
  • Space between contour lines is color-coded
  • Can be either classed or unclassed

29
Hill shading (shaded relief)
  • Illuminate earths topography with imaginary
    light source

Cardinal direction of light source? What do you
think determines the reflectance values of pixel
in digital image?
30
Which map display is this?
31
Oblique view
  • Fishnet map Block diagram

32
Oblique view
  • Fishnet map Fishnet map draped image

33
Physical model
  • 3D map representation of 3D
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