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Understanding Map Projections

Understanding Map Projections

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SINUSOIDAL<br />

Distance<br />

The scale along all parallels and the central meridian<br />

of the projection is accurate.<br />

LIMITATIONS<br />

Distortion is reduced when used for a single land<br />

mass rather than the entire globe. This is especially<br />

true for regions near the equator.<br />

The central meridian is 117° E.<br />

DESCRIPTION<br />

Also known as Sanson–Flamsteed.<br />

As a world map, this projection maintains equal area<br />

despite conformal distortion. Alternative formats<br />

reduce the distortion along outer meridians by<br />

interrupting the continuity of the projection over the<br />

oceans and by centering the continents around their<br />

own central meridians, or vice versa.<br />

USES AND APPLICATIONS<br />

Used for world maps illustrating area characteristics,<br />

especially if interrupted.<br />

Used for continental maps of South America, Africa,<br />

and occasionally other land masses, where each has<br />

its own central meridian.<br />

PROJECTION METHOD<br />

A pseudocylindrical projection where all parallels<br />

and the central meridian are straight. The meridians<br />

are curves based on sine functions with the<br />

amplitudes increasing with the distance from the<br />

central meridian.<br />

LINEAR GRATICULES<br />

All lines of latitude and the central meridian.<br />

PROPERTIES<br />

Shape<br />

No distortion along the central meridian and the<br />

equator. Smaller regions using the interrupted form<br />

exhibit less distortion than the uninterrupted<br />

sinusoidal projection of the world.<br />

Area<br />

Areas are represented accurately.<br />

Direction<br />

Local angles are correct along the central meridian<br />

and the equator but distorted elsewhere.<br />

Supported map projections• 83

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