next up previous contents index
Next: 6.3.8 Miller Cylindrical Projections Up: 6.3 Cylindrical Projections Previous: 6.3.6 Cylindrical Equidistant Projection   Contents   Index

6.3.7 General Cylindrical Projections (-Jy -JY)

This cylindrical projection is actually several projections, depending on what latitude is selected as the standard parallel. However, they are all equal area and hence non-conformal. All meridians and parallels are straight lines. The requirements to define this projection are:

$\bullet$
The central meridian

$\bullet$
The standard parallel

$\bullet$
Scale in inch/degree or as 1:xxxxx (-Jy), or map width (-JY)

While you may choose any value for the standard parallel and obtain your own personal projection, there are four choices of standard parallels that result in known (or named) projections. These are listed in Table 6.1.


Table 6.1: Standard parallels for some cylindrical projections.
Projection name Standard parallel
Lambert 0$^{o}$
Behrman 30$^{o}$
Trystan-Edwards 37$^{o}$24' (= 37.4$^{o}$)
Peters (Gall) 45$^{o}$


For instance, a world map centered on the 35$^{o}$E meridian using the Behrman projection can be obtained by running the command:





pscoast -R-145/215/-90/90 -JY35/30/4.5i -B45g45 -Dc -A10000 -Slightgray -W0.25p -P > \
    GMT_general_cyl.ps





Figure 6.19: World map using the Behrman cylindrical projection.
\includegraphics[]{eps/GMT_general_cyl}

As one can see there is considerable distortion at high latitudes since the poles map into lines.


next up previous contents index
Next: 6.3.8 Miller Cylindrical Projections Up: 6.3 Cylindrical Projections Previous: 6.3.6 Cylindrical Equidistant Projection   Contents   Index
Paul Wessel 2006-01-01