Geographical Information Systems
Geog
481/506 Tu
Th 3:30-4:50pm
Fall
2011 Fillmore
170
Instructor: Ling Bian
LabA: Tue: 5-6:20pm, W145, Chunyuan diao
Office: 120 Wilkeson LabB: Thur:
6:30-7:50pm, W145, Tong Sun
Office hours: Tu Th
2-3pm or by appt. LabC:
Fri: 10-11:20am, W145, Tong Sun
Map Projections and Coordinate Systems
1. Map scale
Ratio between a distance on the map and the corresponding distance
on the earth. The distance on the map is always expressed as one, e.g.,
1:24,000.
Common map scales:
1:24,000
1:250,000
1: 1,000,000
Small scale and large scale
Spatial scales
map scale
resolution
extent
2. Coordinate systems
A system established in relation to (1) a starting point, then the
location of every other point can be stated in terms of (2) a defined direction
and (3) a distance in the direction.
(1) Spherical coordinate systems
Geographical coordinate systems:
Great and small circles
Meridians and parallels
Latitude
Measured northward or southward
from the equator to poles.
Ranging 0-90 degrees north or
south.
The
measuring units are degrees, minutes, and seconds.
The length of one degree
latitude is similar everywhere, 69miles/111km.
Longitude
Measured eastward or westward
from Prime Meridian at Greenwich,
England to the International Date Line
Ranging 0-180 degrees east or west.
The
measuring units.
Length of one degree
longitude reduces toward poles.
Reading latitude and longitude
19050' S: 19 degrees 50 minutes Latitude South
43050' W: 43 degrees 50 minutes Longitude West
(2) Rectangular coordinate systems
It converts earth's curved
surface onto a flat map surface
Origin, axes, and measuring
unit
The x value is given first
and called easting, then the y value is given and called northing
(i) UTM (Universal Transverse Mercator) coordinates
A rectangular coordinate system for the WORLD
Measuring unit: meter
Map projection: Universal Transverse Mercator
Zones: north-south columns of 6
degrees longitude wide,
labeled 1 to 60 eastward beginning
at the 180 degree meridian
Rows:
east-west rows of 8 degrees latitude high,
labeled from C to X (without I, O) beginning at 80 degree latitude
Quadrilaterals
The central meridian of a zone is
given the easting of 500,000m
and
the equator is given 0 northing for the northern hemisphere
Applications of the UTM system
(ii) State Plane coordinates
A rectangular coordinate system for the U.S.
Measuring unit: feet
Zones: The U.S. is divided into 120 zones. Zone boundaries follow state and county lines.
Projections: Each zone has its own projection system
Transverse Mercator for states of N-S extent
Lambert's conformal conic projection for states of E-W extent
The central meridian of a zone is given 2,000,000ft False Easting
False origin: it is established in
the south and west of the zone as 0,0
False easting, and false northing
Zones may overlap
Applications of the State Plane system
3. Topographic maps
Graphical representation of the shape and location of physical features
of land and other physical entities. Topographic maps identity elevation
of the land in contour lines.
A map series published by
USGS
It is bound by parallels
on the north and south, meridians on the east and west
The maps are created from
aerial photos
The features are topography,
vegetation, railroad, streams, roads, urban, etc.
Three coordinate systems
are marked, geographical, UTM, and State Plane
4. Datum
Geodetic datum:
are
established to provide positional control that supports surveying and mapping
projects.
They
cover large geographic areas, such as a country, a continent, or the whole
world.
North American Datum of 1927 (NAD27)
North American Datum of 1983 (NAD83)
Vertical datum:
is the zero
surface from which all elevations or heights are measured
5. Map projections
A means of converting coordinates on a curved surface to coordinates
on a plane.
Map projection vs. coordinate system
A classification of map projections
(1) Classification by conceptual methods
In theory, projections can be created by placing a globe in various
positions relative to a light source and a projection surface.
Cylindrical
Azimuthal
Conic
(2) Classification by distortions
The geometrical relationships on the sphere cannot be entirely duplicated
on a plane. Angles, areas, distances, and directions are subject to various
changes.
Conformal projections
It retains shapes about
a point
Equal-area projections
It retains correct relative
size
Equidistant projections
It retains uniform scale
in all directions but only from one or two points
Azimuthal projections
It retains correct directions
from one or two points
(3) Commonly used projections
Transverse Mercator: cylindrical
conformal
Lambert's conformal conic
6. Readings Chpt 2