1. The Round Earth to Flat Map: Map Projections for Designers SP 240 Cartography Alex Chaucer

2. Spatial Information Technology Center The Size and Shape of the Earth Geodesy – the science of earth measurement Geoid – term used to describe the shape of the earth, means earth-shaped Ellipsoid – geometrical solid with major and minor axis to represent the shape of the earth Clarke Ellipsoid of 1866 – was the reference ellipsoid for establishing a datum Geodetic Reference System (GRS80) – reference ellipsoid used for NAD 83 datum

3. Spatial Information Technology Center Coordinate Geometry for the Cartographer Cartesian coordinate geometry – the system of intersecting perpendicular lines on a plane that contains two principal axes. Digitizing – specifying the locations of geographical points on a map in plane Cartesian space, usually by electronic means. Geoferencing – when cartographers specify Cartesian coordinates into their geographic reference points, or when other source documents (air photos, remotely sensed images) are referenced to a common coordinate system

4. Spatial Information Technology Center Earth Coordinate Geometry Latitude – location on the earth between the equator and the north and south poles, identifying the parallel passing through the position. Longitude – position east or west of the prime meridian; designation is by identifying the meridian passing through the position. Meridian – half of a circle intersecting the earth from pole to pole is a meridian. Prime Meridian – has the angular designation of 0 degrees. Global Positioning System – a “constellation” of 21 high altitude satellites (called NAVSTARS) that beam radio signals to earth-based receivers. The receivers can then take the signals and give latitude, longitude, elevation, and precise time.

5. Spatial Information Technology Center An Introduction to Map Projections for the Designer Map projection – the systematic arrangement of the the earth’s spherical or geographic coordinate system onto a plane; a transformation process. Map Scale = map distance earth distance

6. Spatial Information Technology Center Surface Transformation and Map Distortion It is impossible to render the spherical surface of a globe to the flat map without some degree of tearing, shearing, or compression. http://www-personal.umich.edu/~sarhaus/darcy.jpg

7. Spatial Information Technology Center Surface Transformation and Map Distortion You can’t spread out a basketball onto a flat surface – it’ll tear!

8. Spatial Information Technology Center Surface Transformation and Map Distortion Distortion is not significant when mapping small areas. But it is a significant design problem when portraying the whole earth or continents. At these scales, area, shape, distance or direction must be compromised.

9. Spatial Information Technology Center Map Projection Properties Equal Area Mapping - all mapped areas have the same proportional relationship to the areas on the Earth that they represent http://www.colorado.edu/geography/gcraft/notes/mapproj/mapproj_f.html

10. Spatial Information Technology Center Map Projection Properties Conformal Mapping (or orthomorphic) – the scale of a map at any point on the map is the same in any direction, the projection is conformal. Meridians (lines of longitude) and parallels (lines of latitude) intersect at right angles. Shape is preserved locally on conformal maps. http://www.colorado.edu/geography/gcraft/notes/mapproj/mapproj_f.html

11. Spatial Information Technology Center Map Projection Properties http://www.colorado.edu/geography/gcraft/notes/mapproj/mapproj_f.html Equidistance Mapping - A map is equidistant when it portrays distances from the center of the projection to any other place on the map.

12. Spatial Information Technology Center Map Projection Properties http://www.colorado.edu/geography/gcraft/notes/mapproj/mapproj_f.html Azimuthal Mapping - Direction A map preserves direction when azimuths (angles from a point on a line to another point) are portrayed correctly in all directions.

13. Spatial Information Technology Center Determining Deformation and Its Distribution over the Projection Scale Factor – a ratio representing the transformation of a projection based on that of a reference globe < 1 – Compression has taken place > 1 – Stretching has taken place

14. Spatial Information Technology Center Patterns of Deformation There are 3 basic developable projections (based on 3 surfaces) Plane Cylindar Cone Azimuthal Cylindrical Conic And even ones that are generated mathematically are classified into one of these families. Some are different enough and they are classed as… Pseudoazimuthal, pseudocylindrical, and pseudoconic!!

15. Spatial Information Technology Center Tangent? Secant? http://www.clas.ucsb.edu/staff/lee/Secant%20and%20Tangent%20lines.gif

16. Spatial Information Technology Center Plane/Azimuthal – tangent and secant http://www.colorado.edu/geography/gcraft/notes/mapproj/mapproj_f.html

17. Spatial Information Technology Center Cylindrical – tangent and secant http://www.colorado.edu/geography/gcraft/notes/mapproj/mapproj_f.html

18. Spatial Information Technology Center Conic – tangent and secant http://www.colorado.edu/geography/gcraft/notes/mapproj/mapproj_f.html

19. Spatial Information Technology Center Others?? Pseudocylindrical projections resemble cylindrical projections, with straight and parallel latitude lines and equally spaced meridians, but the other meridians are curves. http://www.colorado.edu/geography/gcraft/notes/mapproj/mapproj_f.html

20. Spatial Information Technology Center Credits Many of these great maps came from: http://www.colorado.edu/geography/gcraft/contents.html http://www.colorado.edu/geography/gcraft/notes/mapproj/mapproj_f.html