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Coordinate Systems and Map Projections

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1 Coordinate Systems and Map Projections
Cartography Coordinate Systems and Map Projections

2 Properties of a Globe Parallels are always parallel to each other and always evenly spaced along meridians and decrease in length poleward Meridians converge at both poles and are evenly spaced along parallels Distance between meridians decrease poleward Parallels and meridians always cross at right angles.

3 Space View

4 Earth’s Dimensions

5 Latitude

6 Longitude

7 Prime Meridian

8 Earth’s Circles

9 Spherical Coordinates

10

11 Geographic Coordinate Systems

12 Projections and Coordinate Systems
Geographical coordinate system – are locations on the map or lat/long Projected coordinate system – locations that have been changed from spherical coordinates to planar (Cartesian) coordinates

13 Projections

14 Map Projection How to represent a curved globe on a flat surface?
The globe is the only true map, but scale problems force us to use projections for larger scales Unfortunately, this can lead to distortion - such as misrepresenting the Great Arc

15 Why project at all? We have to. Flat paper maps Flat computer screen
Measuring distances and areas in degrees is not a desirable thing to do.

16 From Round to Flat It is necessary to use a Projection
Two primary questions to decide which one: Is the intended use to preserve equivalence (Equal Area) or its true shape (Conformal) Only one can be preferred and the other will suffer or lose its relationship.

17 Flattening Earth

18 Nature of Projections Modern Cartography and most GIS programs compensate mathematically for these distortions (Equivalence and Conformality). Projection is used because originally these maps were a globe projected and traced on a surface. Or wires where used to represent latitude (parallels) and longitude (meridians)

19 Projection Surfaces – “developable”

20 Projection Family Family refers to the developable surface Plane =
Cylinder = Cone =

21 Figure 3.1

22 Figure 3.2

23 Figure 3.3

24 Figure 3.4

25 Cylindrical Projections

26 Cylindrical Cylindrical - whole earth – true shape – from Gerardus Mercator (AD 1569), distortion in size towards poles, but useful in navigation because true bearings are given, but distance is skewed

27 Cylindrical projections
Transverse cylindrical Cylindrical

28 Developable Surface – Cylinder

29 Figure 3.7

30 Projections Mathematical projection of lines on a sphere to a flat piece of paper Cylindrical projection Courtesy of ESRI, Inc.

31 Cylindrical Projection

32 Cylindrical

33 Miller Cylindrical

34 World Time Zones

35 Planar projection Planar - used for state or smaller sized areas, where curvature of the earth can be ignored – usually circumpolar maps.

36 Orthographic Projections
Polar Oblique

37 Figure 3.6

38 Planar Projection

39 Gnomonic Illustrating the difference between Mercator and Gnomic
Great Circles – the most direct route between two points Rhumb Line – lines of constant direction

40 Rhumb and Circle

41 Rhumb and Circle

42 Conic Projections

43 Conic Projection Conic - used for continent sized maps, the distortion is less that with plane or cylindrical

44 Conic projections Standard parallels Tangent conic Secant conic

45 Developable Surface- Cone

46 Conic Projection

47

48

49 Mid Latitude Projections
Albers equal-area Conic, equal area with two standard parallels Areas are proportional and directions are true in limited areas Used in the United States and other large countries with a larger east-west than north-south extent

50

51 Special Projections Mercator
Straight meridians and parallels that intersect at right angles Scale is true at the equator or at two standard parallels equidistant from the equator Navigation – all straight lines on the map are lines of constant azimuth

52

53 Special Projections Gall-Peters Who’s the creator?
Reaction to the Mercator projection, which showed European dominance Mercator distorts area Peters argues that his portrays distances correctly, which it does not De-emphasizes area distortions at polar areas

54 Gall-Peters

55 Figure 3.20

56 Figure 3.21

57 Figure 3.22

58 Figure 3.23

59 Figure 3.24

60 Figure 3.25

61 Datums and Coordinate Systems

62 Geodesy and Datums Shape of the Earth

63 Figure 2.2

64 Figure 2.3

65 Table 2.1

66 Table 2.2

67 Figure 2.4

68 National or Global Datums
Surface against (or with) which horizontal or vertical positions may be defined A datum is a reference surface -

69 Horizontal Survey Benchmarks

70 1981 Survey Network

71 Earth’s Dimensions

72 There are two axes are called the
Isaac Newton (1670) suggested the earth would be flattened at the poles, due to centrifugal force Thus, the radius along the axis of rotation would be less than through the equator There are two axes are called the a) semi-major axis (through the equator) b) semi-minor axis (through the poles)

73 Earth’s is Flattened - an Ellipsoid
Two radii: r1, along semi-major (through Equator) r2, along semi-minor (through poles)

74 The Earth is NOT an Ellipsoid (only very close in shape)
The Earth has irregularities in it - These deviations are due to differences in the gravitational pull of the Earth

75 Geoidal Earth Surface where the strength of gravity equals that at mean sea level Highest point on geoid m above elliposid (New Guinea) Lowest point on the geoid m below ellipsoid (south of India)

76 Geoid earth The Geoid is a measured surface (not mathematically defined) Found via surface instruments (gravimeters) towed behind boats, planes, or in autos Or, from measurements of satellite paths May be thought of as an approximation of mean sea level

77 Example of Ellipsoid/Geoid Relationship
Earth’s surface Ellipsoid Geoid

78

79

80 Spheroids and Datums The earth is not a sphere so a spheroid more accurately matches the Earth Spheroids parameterize a coordinate system in a datum Datum = a set of control points NAD27 NAD83 WGS1984

81 Datums Common Datums North American 1983 or NAD83
Sphere Spheroid Geoid Datum Common Datums North American 1983 or NAD83 North American 1927 or NAD27 World Geodetic System 1984 or WGS84 Global Reference System 1980 or GRS80

82 p3 p1 p2 h1 h2 h3 Datum height

83 Figure 2.5

84 Typical datum offset Roads in NAD83 Photo in NAD27 DOBA?

85 Specifying Projections
The type of developable surface (e.g., cone) The size/shape of the Earth (ellipsoid, datum), and size of the surface Where the surface intersects the ellipsoid The location of the map projection origin on the surface, and the coordinate system units

86 Projection Case Case refers to the number of tangents, or standard parallels tangent secant azimuthal cylindrical conic

87 Transverse or Equatorial
Projection Aspect Aspect refers to the location of tangency Normal or Polar Oblique Transverse or Equatorial

88 Defining a Projection – LCC (Lambert Conformal Conic)
The LCC requires we specify an upper and lower parallel A spheroid A central meridian A projection origin origin central meridian

89 Projections – developable surfaces
Cylindrical Conic

90 Projections in ArcMap

91 Projected Coordinate Systems
Projections are a systematic rendering of geographic coordinates Geometric – planar/ cylindrical/ conic Gnomonic Orthographic Stereographic Mathematical – defined by formulas Distortion patterns – tangent and secant

92 Projection parameters
False easting False northing Latitude of origin 0,0 Central meridian

93 Properties of a coordinate system
GCS/Datum/Spheroid Map units Central Meridian False easting False northing Reference latitude Standard parallels Different projections may have different types of parameters used.

94 Distortion All map projections introduce distortion
Type and degree of distortion varies with map projection When using a projection, one must take care to choose one with suitable properties

95 Types of distortion Area Shape Distance Direction

96 Projection distortions
Mercator Equidistant Conic Distorts distance and area Preserves direction and shape Distorts direction and shape Preserves distance and ~area

97 Compromise projections
Robinson Distorts all four properties a little

98 Table 3.1

99 Table 3.2

100 Projection Surface Rays “traced” from a source, through a globe to the projection surface All map projections cause distortion We control distortion by choosing the surface, and projection center

101 Distortion Varies Across Map

102 Projections in ArcMap Data may be projected or unprojected
Converts all data on the fly to the coordinate system chosen for the data frame Relies on correct coordinate system definitions for each layer

103 Coordinate Systems Defined for a data layer, including
Geographic coordinate system Spheroid/ellipsoid on which the lat/long values are based The datum on which the GCS is based Projection parameters (if any)

104 Coordinate systems Unprojected Projected Has GCS and datum defined
Map units are decimal degrees Has no projection in CS definition Projected Has GCS and datum defined Map units usually are feet or meters Has projection in CS definition GCS_WGS_1984 World_Robinson

105 Extents The extent of a spatial data set indicates the range of x-y values present in the data Stored map units

106 Values in this range indicate units of degrees and thus a GCS
CS Definitions Values in this range indicate units of degrees and thus a GCS Unprojected coordinate system

107 Large values usually indicate a projected coordinate system
CS Definitions Large values usually indicate a projected coordinate system Projected coordinate system

108 Note on terminology “Projection” has two definitions
The mathematical transformation applied to convert a spherical coordinate system to a planar coordinate system (used in this text) The complete coordinate system definition of a GIS data set, including the geographic coordinate system, datum, and projection (used by some, including older ESRI materials)

109 On the fly projection in ArcMap
Source Layers Data frame World in GCS_WGS84 Robinson_WGS_84 Latlon in GCS_WGS84 Input layers have any CS Set data frame to desired CS

110 Map units Source Layers Data frame
Decimal degrees Meters Decimal degrees On-the-fly projection is a temporary change in the CS for display only. Stored x-y values and units are unchanged.

111 Setting the data frame coordinate system

112 Modifying the properties of the selected data frame coordinate system
Set: Central Meridian False easting False northing Map units Spheroid Datum

113 Understanding units Be careful not to confuse The stored map units
Property of the file’s CS X-Y values are saved in the spatial data file Can’t be changed The data frame map units Determined by the data frame CS Changed by changing the data frame CS properties The display units Set by the user to any desired units Affects only the x-y location readout and measurements

114 Stored map units 1. Add file to ArcMap 2. Set data frame CS

115 Managing coordinate systems
Three typical operations Examine a layer’s CS information Define a CS for a layer with unknown or incorrect CS Convert a layer to a different CS

116 Examine the CS (ArcMap)
Right-click layer and open properties The extent is given in map units, not the units of the data frame CS. Click Source tab to read CS information

117 Examine the CS (ArcCatalog)
Click Shape in Fields tab Read coordinate system definition Right-click layer to open properties Examine details or define CS

118 Defining the CS Places a label on the data set, specifying the CS of the coordinates already stored inside. It is imperative that the definition match the stored units. Knowing the correct CS may require contacting the person who created the data. GCS_NAD1983 ROADS ,44.628 ,44.653 ,44.73

119 Two ways to define a CS Set the CS in the Properties in ArcCatalog
Use the Define Projection tool in ArcToolbox

120 Define CS in Properties
Click Shape in Fields tab Read coordinate system definition Right-click layer to open properties Examine details or define CS

121 Define the CS in ArcToolbox

122 Convert a layer to a new CS
Creates a new spatial data file Does not destroy or change the original file Recalculates each x-y point into the new coordinate system and units Labels the new file with the new CS Wells.shp ,44.628 ,44.653 ,44.732 Wells.shp 445678,654321 445021,650001 444823,649200 Project Units in decimal degrees Units in meters

123 Two ways to project Use the Project tool in ArcToolbox
Export the data in ArcMap

124 Using a tool

125 Project tool

126 Export in ArcMap Set the data frame coordinate system to the desired output CS Export and choose to use the data frame CS TIP: You can project a coverage without an ArcInfo license this way!

127 CAUTION! DO NOT confuse This is a very common mistake
Projecting Defining a projection This is a very common mistake It is also a dangerous one At best you won’t be able to display the data At worst you may corrupt a data file forever

128 Define Projection only changes the label of the coordinate system
Project changes the label AND the xy coordinate values UTMZone13_ NAD1983 GCS_NAD1983 Roads.shp ,44.628 ,44.653 ,44.732 Roads.shp 445678,654321 445021,650001 444823,649200 Project

129 Faulty reasoning I want to display ROADS and STATE together in UTM
UTM Zone13 STATE 445678,654321 445021,650001 444823,649200 I want to display ROADS and STATE together in UTM ROADS is in GCS I need to open ArcCatalog and change the ROADS to UTM GCS_NAD1983 ROADS ,44.628 ,44.653 ,44.732 Result: A data set with a mislabeled CS.

130 Result of faulty reasoning
ArcMap sees label and says “I don’t have to reproject it to UTM on-the-fly” UTM Zone13 STATE 445678,654321 445021,650001 444823,649200 UTM Zone 13 ROADS ,44.628 ,44.653 ,44.732 y Data frame CS: UTM Zone 13 . x 0,0

131 Correct reasoning I want to display roads and state together in UTM
GCS_NAD1983 I want to display roads and state together in UTM Just let ArcMap project on-the-fly OR use the Project tool to convert roads to UTM, creating a new file. ROADS ,44.628 ,44.653 ,44.732 UTM Zone13_ NAD83 STATE 445678,654321 445021,650001 444823,649200

132 Employment of Map Projections
Carefully consider: Projection properties – is it suited (Equivalence? Conformal?) Deformational properties – acceptable? Benefit the shape? Projection center – can it be centered? Familiarity – for users? for designers? Cost – economical? available?

133 Base Map Compilation Manual base map rules (works with GIS)
Map purpose Use objective evaluation Avoid personal bias Determine what elements typify the character of the area Strive for uniformity (if you generalize, make sure it evenly done)

134 Accuracy and Reliability
Map accuracy = the degree of conformance to an established standard Is your source map a: Basic map – from an original survey Derived map – compiled from basic maps The further you get from the basic map the better the chance of error Map copyright – check for and honor copyright to avoid trouble


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