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6.4.4 Robinson Projection (-Jn -JN)

The Robinson projection, presented by Arthur H. Robinson in 1963, is a modified cylindrical projection that is neither conformal nor equal-area. Central meridian and all parallels are straight lines; other meridians are curved. It uses lookup tables rather than analytic expressions to make the world map ``look'' right6.3. The scale is true along latitudes $\pm$ 38$^{o}$. The projection was originally developed for use by Rand McNally and is currently used by the National Geographic Society. To use it you must enter

$\bullet$
The central meridian

$\bullet$
Scale along equator in inch/degree or 1:xxxxx (-Jn), or map width (-JN)

Again centered on Greenwich, the example below was created by this command:





pscoast -Rd -JN0/4.5i -Bg30/g15 -Dc -A10000 -Ggray -P > GMT_robinson.ps





Figure 6.24: World map using the Robinson projection.
\begin{figure}\centering\epsfig{figure=eps/GMT_robinson.eps}\end{figure}


next up previous contents index
Next: 6.4.5 Eckert IV and Up: 6.4 Miscellaneous Projections Previous: 6.4.3 Winkel Tripel Projection   Contents   Index
Paul Wessel 2004-10-01