Title: Mapping and Projections
1Mapping and Projections
- Web resources
- Geographers Craft, Department of Geography,
University of Colorado at Boulder - particularly
Peter H. Danas part - http//www.colorado.edu/geography/gcraft/contents.
html - Laurie Garo, Map Projections module, in Virtual
Geography Department, U. of Texas at Austin
(hosted at U. of Colorado) - http//www.colorado.edu/geography/virtdept/content
s.html
2Map Projections
- Basic problem
- Earth is round
- Paper is flat
3Conformal
4Equivalent or Equal Area
5Equidistant
6Equidistant CylindricalMap from Carlo Futuri
7Solving the Problem
- How do you represent a curved surface on a flat
surface? - Bonehead way - just plot latitude vs. longitude
as cartesian rectangular coordinates - Projection - fit a flat surface around (or
through) a sphere, and trace the pertinent
information on it
8Unprojected map
9Types of projections
- Three main families
- Cylindrical - wrap sheet of paper around globe in
cylinder shape - Also pseudocylindrical - like cylindrical but the
sheet of paper bends inward at the poles - Conic - form sheet of paper into a cone and
insert globe - Also polyconic - multiple cones
- Azimuthal - place flat sheet of paper next to
globe project features out onto it
10Cylindrical Projection
11Cylindrical Projection
- Formed by wrapping a large, flat plane around the
globe to form a cylinder. - Transfer latitude, longitude, shapes onto
cylinder, then unfolded into a flat plane. - Typically used to represent the entire world
often projected from center of globe with equator
as tangent line - Most types show parallels and meridians forming
straight perpendicular lines.
12Cylindrical Projection
13Pseudocylindrical Projection
- Projection surface is not rectangular
- Instead, it curves inwards at the poles.
- Latitude lines are straight central meridian is
straight, but other meridians are curved (concave
toward the central meridian). - Often used for world maps
14Pseudocylindrical Projection
15Pseudocylindrical Projection
16Pseudocylindrical Projection
17Conic Projection
18Conic Projection
- Points from the globe are transferred to a cone
fit around the sphere. - Usually, the pointy end of the cone is directly
over the north or south pole, but you can do it
anywhere. - Can represent both hemispheres, but distortion
increases the farther along the cone you go
19Conic Projection
- Often used to project areas that have a greater
east-west extent than north-south, e.g., the
United States. - When projected from the center of the globe,
conic projections typically show parallels
forming arcs concave toward the North or South
pole, and meridians are either straight or curved
and radiate outwards from the direction of the
point of the cone.
20Conic Projection
21Equidistant Conic Projection
22Albers Equal Area Conic
23Polyconic Projection
- Complex projection, used originally by USGS for
quadrangle maps of U.S. - Uses an infinite number of cones applied to an
infinite number of tangents across a given
hemisphere - Reduces distortion, but harder to conceptualize
and produce
24Polyconic Projection
25Polyconic Projection(centered at equator, 90ºW)
26Azimuthal (Planar) Projection
27Azimuthal or Planar Projection
- Globe grid is projected onto a flat plane
- Plane is normally placed above the north or south
pole, so normally only one hemisphere, or a
portion of it, is represented - When projected from the center of the globe, a
typical polar azimuthal projection shows circular
latitude lines with radiating longitude lines
28Azimuthal Projection
29Azimuthal Projection
30Oblique Azimuthal Projection
Orthographic sort of means viewed from infinite
distance
31Types of projections
- Tangent
- Flat surface only touches globe along one
circular line (or at one point for Azimuthal) - Secant
- Flat surface passes through globe touches
surface at two circular lines (or in one circle
for Azimuthal) - Some projection is inward rather than outward
- Reduces distortion of large areas
32Tangent Projection
33Secant Projection
34Secant Projection
35Robinson Projection
36Goodes Interrupted Homolosine Projection
37Tissot indicators
- Tissots idea - to see the effects of distortion,
show what shape small circles on the surface of
the globe take after projection - This shows shape, scale, area, and other
distortions
38Tissot Indicators Mercator (Conformal)
Image from http//quantdec.com/tissot
39Tissot Indicators Peters Equal Area
Image from http//quantdec.com/tissot
40Tissot Indicators Azimuthal Equidistant
Image from http//quantdec.com/tissot
41Tissot Indicators
42Silly Projections
43Web sites to visit
- http//www.guilford.edu/geology/Geo340.html