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Understanding Map Projections

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equator<br />

The parallel of reference that defines the origin of latitude<br />

values, 0° north or south.<br />

equatorial aspect<br />

A planar projection that has its central point at the<br />

equator.<br />

equidistant projection<br />

A projection that maintains scale along one or more lines<br />

or from one or two points to all other points on the map.<br />

equivalent projection<br />

A projection on which the areas of all regions are shown<br />

in the same proportion to their true areas. Shapes may be<br />

greatly distorted (Snyder and Voxland, 1989). Also known<br />

as an equal-area projection.<br />

false easting<br />

A linear value added to the x-coordinate values, usually to<br />

ensure that all map coordinates are positive. See false<br />

northing.<br />

false northing<br />

A linear value added to the y-coordinate values, usually to<br />

ensure that all map coordinates are positive. See false<br />

easting.<br />

flattening<br />

A measure of how much a spheroid differs from a sphere.<br />

The flattening is the ratio of the semimajor axis minus the<br />

semiminor axis to the semimajor axis. Known as ‘f’ and<br />

often expressed as a ratio. Example: 1/298.3. Also known<br />

as the ellipticity.<br />

Gauss–Krüger<br />

A projected coordinate system used in Europe and Asia<br />

that divides the area into six degreewide zones. Very<br />

similar to the UTM coordinate system.<br />

geocentric latitude<br />

Defined as the angle between the equatorial plane and a<br />

line from a point on the surface to the center of the<br />

sphere or spheroid.<br />

geodesic<br />

The shortest distance between any two points on the<br />

surface of a spheroid. Any two points along a meridian<br />

form a geodesic.<br />

geodetic latitude<br />

Defined as the angle formed by the perpendicular to the<br />

surface at a point and the equatorial plane. On a spheroid,<br />

the perpendicular doesn’t hit the center of the spheroid in<br />

the equatorial plane except at the equator and the poles.<br />

geographic coordinate system<br />

A reference system that uses latitude and longitude to<br />

define the locations of points on the surface of a sphere<br />

or spheroid.<br />

geographic transformation<br />

A method that converts data between two geographic<br />

coordinate systems (datums). Also known as a datum<br />

transformation.<br />

Global Positioning System<br />

A set of satellites operated by the U.S. Department of<br />

Defense. Ground receivers can calculate their location<br />

using information broadcast by the satellites.<br />

GPS<br />

See Global Positioning System.<br />

graticule<br />

A network of lines representing a selection of the earth’s<br />

parallels and meridians (Snyder and Voxland, 1989).<br />

great circle<br />

Any circle on the surface of a sphere formed by the<br />

intersection of the surface with a plane passing through<br />

the center of the sphere. The shortest path between any<br />

two points lies on a great circle and is therefore important<br />

to navigation. All meridians and the equator are great<br />

circles on the earth defined as a sphere (Snyder and<br />

Voxland, 1989).<br />

Greenwich prime meridian<br />

The prime meridian located in Greenwich, England.<br />

grid<br />

A network of lines representing a selection of a projected<br />

coordinate system’s coordinates.<br />

HARN<br />

See High Accuracy Reference Network.<br />

102 • <strong>Understanding</strong> <strong>Map</strong> <strong>Projections</strong>

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