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Map Projections

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Map Projections 3D-2D Transformation Process Geoid Earth as Sphere Most commonly used in cartography Primarily for small-scale maps Earth as Sphere Size 3D-2D ... – PowerPoint PPT presentation

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Title: Map Projections


1
Map Projections
2
3D-2D Transformation Process
  • Geoid
  • Reference Ellipsoid
  • Sphere of Equal Area
  • Reference Globe
  • Transformation
  • Map Projection

3
Earth as Sphere
  • Most commonly used in cartography
  • Primarily for small-scale maps

4
Earth as Sphere Size
  • 40 million meters in circumference
  • 20 million meters from Pole-to-Pole
  • 10 million meters from Equator to Pole
  • 1 Meter 1/10-million of the distance from the
    equator to the north pole as a line of longitude
    running through Paris France


5
3D-2D Transformation Process
  • Geoid
  • Reference Ellipsoid
  • Sphere of Equal Area
  • Reference Globe
  • Transformation
  • Map Projection

6
Reference Globe
A reference globe is where the size of the sphere
(or other shape) is reduced until it matches the
final scale desired for map making
7
3D-2D Transformation Process
  • Geoid
  • Reference Ellipsoid
  • Sphere of Equal Area
  • Reference Globe
  • Transformation
  • Map Projection

8
3D-2D Transformation Process
Projection selection and final transformation
from 3d-to-2d
Distorting inevitable
9
Tearing, Shearing Compression
10
Uncertainty Errors
  • Need to know where error is and how to control it
  • Which map is more accurate?
  • Conformal vs. Equal Area

11
  • Conformal correct proportions shape
  • Equal Area area relationships of all parts are
    maintained property of equivalence

12
Map Error Projections can Preserve
  • Shape
  • Scale preserved in all directions around a point
  • Preserves local angular relationship
  • Conformal Maps
  • Area (size)
  • Equal Area Maps
  • Distance (scale)
  • Equidistance Maps
  • Direction (azimuth)
  • Equidirection Maps

13
No map can be both Conformal Equal Area
14
3D-2D Transformation Process
  • Geoid
  • Reference Ellipsoid
  • Sphere of Equal Area
  • Reference Globe
  • Transformation
  • Map Projection

15
Flattening the globe Map Projections
Transforming a globe to a flat map requires
distortion of one kind or another
16
Map projectionsclassification by surface
  • Earth features are projected on to three kinds of
    developable surfaces
  • plane a flat plane touches the globe
  • cylinder a cylinder is wrapped around the globe,
    and unwrapped to a flat map
  • cone a cone is wrapped around the globe, and
    unwrapped to a flat map

17
Common planar projections
Light source
Gnomonic
18
Common projections
Cylindrical
Mercator
Peters
Equal-area cylindrical
19
Common projections
Conic
Albers equal-area
Lambert conformal
20
Projection surfaces
conic
planar (or azimuthal)
cylindrical
Can construct the appearance of each with geometry
21
Some mathematical projections
pseudocylindrical
pseudoconic
22
Why all the projections?
All have distortion of some kind, but each
serves a unique purpose or has a unique property
that is useful for a certain application
23
Distortion and accuracy on projections
  • Strategy compare the projection to a globe (an
    unprojected map)

Meridians converge
90
All distances are equal
Distances decrease
24
Some questions accuracy distortion on
projections
  • Can we compare one area to another accurately?
  • Are shapes correct?
  • Are directions from one place to another
    accurate?
  • Can we compare distances between places?
  • Which parts of the map suffer the most distortion?
  • Property aspects of the globe that aprojection
    preserves
  • Distortion aspects that the projection doesnt
    preserve

25
Some equal-area projections
Equal-area cylindrical
Albers equal-area
Mollweide pseudocylindrical
26
Conformal angles shapes (sort of) preserved
90
  • Shapes, in small areas near the middle of the
    projection, look the same on the map as they do
    on the globe
  • As on globe, all meridians parallels intersect
    at right angles

27
Directions are preserved azimuthal
Gnomonic
  • Angular measurement from one location to another
    is accurate
  • Straight lines are great circles

Not a great circle!
GOOD FOR Air navigation, radio signals or
radiation patterns
28
Distances are preserved equidistant
2000 miles
If measured on a line that passes through center
Not this line!
29
Area preserved equivalent or equal-area
1 million sq. miles
Important for maps where land area is important
30
Conformal projections and navigation
But the line isnt a great circle!
Mercator projection
  • With Mercator You can use a straight line from
    origin to destination to determine your compass
    bearing to the destination

31
Some examples of map types
Map purpose Critical Properties for the purpose Critical Properties for the purpose Critical Properties for the purpose Critical Properties for the purpose
Map purpose Conformal Equal-Area Equidistant Azimuthal
Navigation ü ü ü
Show distances ü
Large-scale reference ü
Teaching ü ü
Comparing regions ü ü
32
Four Key Projection Properties
Property of a projection how its true to the
globe
  • Equivalence Equal areas
  • Conformality Correct angles (rhumb lines
    straight lines)
  • Azimuthality Correct directions
    (great circles straight lines)
  • Equidistance Correct distances

Cant occur together!
33
Aspect
  • The orientation of the developable surface to the
    reference globe
  • Three aspects equatorial, transverse, and oblique

34
Equatorial Aspect
  • Globe axis parallel to developable surfaces axis
  • A normal aspect simple map graticule

35
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36
Oblique Aspect
  • Non-great circle or meridian used

37
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38
Transverse Aspect
  • Rotates the world 90 degrees
  • Good for showing areas with large N-S Extent
  • Where a meridian of longitude touches the the
    developable surface

39
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40
Secant Map Projections
Developable surfaces cuts through the reference
globe
41
Secant Variations
42
Meeting several needsCompromise projections
Miller
Robinson
43
The projection matrix
Projection properties
equivalent conformal equidistant azimuthal
cylindrical Peters Mercator Plate-Carree Mercator
conic Albers equal area Lambert conformal conic Simple conic Lambert conformal conic
planar Lambert azimuthal Stereographic Azimuthal equidistant Azimuthal equidistant
Projection surfaces
44
What part of a map has the least amount of
distortion?
45
What part of a map has the least amount of
distortion?
  • Where the projection surface touches the globe

Standard line
Standard point
Standard line
46
For what country or region would you choose these
surfaces?
47
Guidelines
Projection surfaces and orientations with areas
for which theyre suited
Planar roundish area, anywhere on earth
Conic or pseudoconic area in middle latitudes,
extensive east west
Cylindrical or pseudocylindrical area
extending along equator or a meridian
48
Keys to Choosing Projections
  • Whats the purpose of your map?
  • What types of accuracy (properties) are most
    important?
  • For maps of portions of the world What surface
    and orientation will best fit the area of the
    world youre mapping?

49
Quick Reading
  • Claudius Ptolemaeus (Ptolemy) Representation,
    Understanding, and Mathematical Labeling of the
    Spherical Earth
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