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Cylindrical projections are a class of projections in which the surface of projection is a cylinder whose axis intercepts the centre of the generating sphere. The native coordinate system is such that the polar axis is coincident with the axis of the cylinder. Meridians and parallels are mapped onto a retangular grid. The projection is therefore described directly by formulae which return x, and y. All cylindricals have
x - r0, | (34) |
and this may be inverted as
- . | (35) |
The requirement for conformality of cylindrical projections is
= , | (36) |
and since
r0 | (37) |
the general solution is
y r0lntan , | (38) |
and this is the basis of Mercator's projection.
Let an oblique coordinate system be denoted by (,), and let the coordinates of the pole [??? (0,0)] of the native coordinate system in the oblique system be (,). The meridian of the oblique system defined by = will be projected as a straight line segment; suppose it overlies the native meridian of = in the same sense of increasing or decreasing latitude (to distinguish it from the native meridian on the opposite side of the pole), then the Euler angles for the transformation from (,) to (,) are
(,,) = ( - 90o,, - 90o). | (39) |
In the general case the radius of the cylinder is r0, where r0 is the radius of the generating sphere, and the point of projection is distant r0 from the centre of the sphere. If 0 the point of projection moves around a circle of radius r0 in the equatorial plane of the generating sphere depending on the meridian being projected. The case < 0 is allowable, however - .
...diagram...
It is straightforward to show that
x | = | - r0, | (40) |
y | = | r0sin , | (41) |
For = 0, where the point of projection is at the centre of the generating sphere, the effect of is to scale the projection uniformly in x and y.
The equations for x and y are invertible as follows:
= | - , | (42) | |
= | arg(1,) + sin-1 , | (43) |
where
= . | (44) |
Limits for the perspective cylindrical projections are determined by the value of rather than which mainly affects the relative scaling of the x and y axes.
The requirement for conformality of perspective cylindrical projections is
[( + ) - ]cos2 + ( + - 2)cos - = 0. | (45) |
For = 0 the projection is conformal at the equator for all values of . For = 1 the projection is conformal at latitudes = cos-1, and this is the basis of Gall's projection.
In this simplest case of a perspective cylindrical projection the point of projection is at the centre of the generating sphere and the cylinder intersects the equator.
= | 0, | (46) | |
= | 1, | (47) | |
x | = | - r0, | (48) |
y | = | r0tan, | (49) |
= | - , | (50) | |
= | tan-1 . | (51) |
Limits: diverges at latitudes
= 90o.
Conformal at latitude
= 0o.
This projection, which is conformal at latitudes = 45o, minimizes distortions in the equatorial regions.
= | 1 | (52) | |
= | /2 | (53) | |
x | = | - r0, | (54) |
y | = | r01 + tan , | (55) |
= | - , | (56) | |
= | 2tan-1 . | (57) |
Limits: none.
Conformal at latitudes
= 45o.
This perspective projection is a specific instance of a subclass of non-perspective equal area cylindrical projections. See also generalized equal area cylindrical projections.
= | , | (58) | |
= | 1, | (59) | |
x | = | - r0, | (60) |
y | = | r0sin, | (61) |
= | - , | (62) | |
= | sin-1 . | (63) |
Limits: none.
Conformal at latitude
= 0o.
Each of the non-perspective projections discussed here has
x = - r0 , | (64) |
and inverse
= - . | (65) |
Also known as Cartesian projection, this projection is easy to construct and take measurements from.
y | = | r0 , | (66) |
= | - . | (67) |
Limits: none
Conformal at latitude
= 0o.
This is a conformal projection with the useful property that lines of constant bearing (rhumb lines) are projected as straight lines. Consequently, it has been widely used for navigational purposes.
y | = | r0lntan , | (68) |
= | 2tan-1e . | (69) |
Limits: diverges at latitudes
= 90o.
Conformal at all points.
Parallels are spaced so as to make the projection equal area, and scaled so as to make it conformal at latitudes = . The area of a region on the projection is 1/cos2 times larger than that of the corresponding region on the generating sphere. The case with = 1 is Lambert's projection.
y | = | r0, | (70) |
= | sin-1 . | (71) |
Limits: none.
Conformal at latitudes
= .