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Understanding Map Projections

Understanding Map Projections

Understanding Map Projections

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STEREOGRAPHIC<br />

PROPERTIES<br />

Shape<br />

Conformal. Local shapes are accurate.<br />

Area<br />

True scale at center with distortion increasing with<br />

distance.<br />

Direction<br />

Directions are accurate from the center. Local angles<br />

are accurate everywhere.<br />

Distance<br />

Scale increases with distance from the center.<br />

The central meridian is 0°, and the latitude of origin is 90° S.<br />

DESCRIPTION<br />

This projection is conformal.<br />

PROJECTION METHOD<br />

Planar perspective projection, viewed from the point<br />

on the globe opposite the point of tangency.<br />

Stereographic projects points on a spheroid directly<br />

to the plane. See Double Stereographic for a<br />

different implementation.<br />

LIMITATIONS<br />

Normally limited to one hemisphere. Portions of the<br />

outer hemisphere may be shown, but with rapidly<br />

increasing distortion.<br />

USES AND APPLICATIONS<br />

The oblique aspect has been used to map circular<br />

regions on the moon, Mars, and Mercury.<br />

All meridians and parallels are shown as circular arcs<br />

or straight lines. Graticular intersections are<br />

90 degrees. In the equatorial aspect, the parallels<br />

curve in opposite directions on either side of the<br />

equator. In the oblique case, only the parallel with<br />

the opposite sign to the central latitude is a straight<br />

line; other parallels are concave toward the poles on<br />

either side of the straight parallel.<br />

POINT OF CONTACT<br />

A single point anywhere on the globe.<br />

LINEAR GRATICULES<br />

Polar aspect—All meridians.<br />

Equatorial aspect—The central meridian and the<br />

equator.<br />

Oblique aspect—Central meridian and parallel of<br />

latitude with the opposite sign of the central latitude.<br />

Supported map projections• 87

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