GEOGRAPHIC INFORMATION SYSTEMS
Lecture 08: Map Projections
Earth Ellipsoid and Horizontal Datums (cont’d)
Components of a Geographic Coordinate System
Recognize that there are three components to a geographic coordinate system.
1) the units of the coordinate system (decimal degrees)
2) the orientation of the coordinate system (Prime Meridian and north is up)
3) the datum (provides a reference framework for the coordinate system)
a) the ellipsoid shape (defined by the semi-major and semi-minor axes and the flattening ratio)
b) the ellipsoid origin (a reference point that defines how the ellipsoid is aligned to the geoid)
- ellipsoid can be aligned to a land-based benchmark (e.g. the benchmark in NAD_27)
- or the ellipsoid can be Earth-centered, as in the case of NAD_83 and WGS_84
As a side note, for Geographic Coordinate Systems, ArcMap assumes that the Equator is 0°, north is up, latitude
varies from +90° to -90°, and longitude varies from +180° to -180° (as opposed to 0° to 360°)
Geographic Coordinate System North American 1927 (GCS NAD27)
1) Angular Units: Degrees
2) Prime Meridian: Greenwich
3) Datum: North American Datum of 1927 (NAD_27)
Ellipsoid: Clarke 1866 Ellipsoid
Semi-major axis: 6,378,206.4 m
Semi-Minor axis: 6,356,583.8 m
Flattening Ratio: 1/294.978698214
Ellipsoid Origin: NAD_27 benchmark on Meades Ranch, Kansas
Geographic Coordinate System North American 1983 (GCS NAD83)
1) Angular Units: Degrees
2) Prime Meridian: Greenwich
3) Datum: North American Datum of 1983 (NAD_83)
Ellipsoid: Geodetic Reference System of 1980 (GRS_80)
Semi-major axis: 6,378,137.0 m
Semi-Minor axis: 6,356,752.3141 m
Flattening ratio: 1/298.257222101
Ellipsoid Origin: Earth-centered
Geographic World Geodetic Reference System of 1984 (very similar to GCS NAD83)
1) Angular Units: Degrees
2) Prime Meridian: Greenwich
3) Datum: World Geodetic Reference System of 1984 Datum (WGS_84)
Ellipsoid: World Geodetic Reference System of 1984 Ellipsoid (WGS_84)
Semi-major axis: 6,378,137.0 m
Semi-Minor axis: 6,356,752.314245 m
Flattening ratio: 1/298,257.223563
Ellipsoid Origin: Earth-centered
Copyright© 2015, Kevin Mulligan, Texas Tech University
Coordinate Systems in ArcMap
- when we add a layer to ArcMap, the coordinate system information for the data layer is displayed in the
Layer Properties dialog box > Source tab
- in this case, counties,shp is using the GCS_North_American_1983 (the GCS referenced to NAD_83)
- in ArcMap, it is also important to recognize that the data frame will take on the coordinate system properties
of the first layer that is added
- in the Data Frame Properties dialog box > Coordinate System tab, we see that the data frame properties have
taken on the coordinate system of the counties.shp layer
Copyright© 2015, Kevin Mulligan, Texas Tech University
Map Projections
Distortion in Maps
- all maps have some distortion in either: 1) area, 2) shape, 3) distance or 4) direction
- the purpose of a map projection is to minimize the distortion in one or more of these properties
- which map projection is most suitable depends upon:
1) the purpose of the map (e.g. navigation, atlas, general reference)
2) the area being mapped (including the size, shape and latitude)
- the term “map projection” stems from the fact that the globe (latitude and longitude) is being
projected mathematically onto a flat surface
Classes of Map Projections
- there are four general classes of map projections
- cylindrical projections, pseudo-cylindrical projections, planar projections and conic projections
1) Cylindrical projections
- geographic grid is mathematically projected onto a cylinder
- cylinder touches the globe (minimize distortion) along a standard parallel or two standard parallels
- can be used for world maps but often have severe distortion at high latitudes
- best used to map low latitude tropical regions where the distortion in minimized
- transverse cylindrical projections touch the globe (minimize distortion) along a central meridian
Copyright© 2015, Kevin Mulligan, Texas Tech University
2) Pseudo-cylindrical projections
- pseudo-cylindrical projections are loosely based on a cylindrical projection but
modified to make the world look correct or minimize the distortion in area on a world map
- most widely used in atlases – where the look of the map and relative areas are important
3) Conic projections
- touches the globe along a standard parallel or two standard parallels in the mid-latitudes
- not suitable for world maps (but can be used to map individual continents)
- most often used to map mid-latitude regions (e.g. US, Europe, Russia, China)
- also widely used to map US states (e.g. we most often use a conic projection to map Texas)
4) Planer projections
- touches the globe at either pole or along a high-latitude standard parallel
- not suitable for world maps (but can be used to map the northern or southern hemisphere)
- most often used to map high-latitude regions (e.g. the Arctic and Antarctic)
- lines of longitude radiate from the pole
Copyright© 2015, Kevin Mulligan, Texas Tech University
GIST 3300 / 5300
Geographic Information Systems
Map Projections
Map Projections
- getting the spherical Earth onto a flat map
- minimizing the distortion on maps
Types of Map Projections
- cylindrical
- pseudo-cylindrical
- planer
- conic
Geographic Information Systems
Ellipsoids and Datums (cont’d)
Components of a Geographic Coordinate System
- recognize that there are three components to a GCS…
1) the units of the coordinate system (decimal degrees)
2) the orientation of the coordinate systems (north is up)
3) the datum (provides a reference framework for the GCS)
- there are two components to a datum
a) ellipsoid (defined by the flattening ratio)
b) origin (a reference point for the coordinate system)
Geographic Coordinate Systems (examples)
GCS North American 1927
GCS North American 1983
GCS WGS 1984
Geographic Information Systems
Map Projections
- it is physically impossible to accurately represent a spherical
surface (the Earth) on a flat piece of paper (a map)
- there will always be some distortion in either:
1) shape
2) area
3) distance
4) direction
Geographic Information Systems
Map Projections
Greenland, 2,166,000 km2
United States, 9,826,630 km2
Canada, 9,984,670 km2
Geographic Information Systems
Map Projections
Antarctica 14,000,000 km2
United States, 9,826,630 km2
Geographic Information Systems
Map Projections
- the purpose of a map projection is to minimize the distortion in
one or more of the four map properties
- either shape, area, distance, direction
- which map projection is most suitable, depends upon:
1) the purpose of the map
- e.g. navigation or general reference
2) the area being mapped
- including the latitude, size and shape of the area
- the term map projection stems from the fact that the globe (lat and long)
is being projected mathematically onto a flat surface
Geographic Information Systems
Map Projections
- there are four general classes of projections
1) cylindrical projections
- Earth projected onto a cylinder
2) pseudo-cylindrical projections
- Earth projected onto a pseudo-cylinder
3) conic projections
- Earth projected onto a cone
4) planer projections
- Earth projected onto a flat plane
Geographic Information Systems
Map Projections
Cylindrical Projections
- standard parallel(s) along a line of latitude
One standard parallel
Two standard parallels
Geographic Information Systems
Map Projections
Transverse Cylindrical Projection
- standard meridian along a line of longitude
Geographic Information Systems
Map Projections
Conic Projections
- standard parallel(s) along a line of latitude
Geographic Information Systems
Types of Map Projections
Planer Projections
- standard parallel along a line of latitude or at the pole
Geographic Information Systems