On the other hand, many projections are only distantly inspired by geometric principles. For instance, Mercator's cylindrical projection can't be visualized as a perspective process unless:
In all three cases the complexity negates the usefulness of a perspective model.
Indeed, many projections have simply no geometric or physical interpretation, and are described purely by mathematical formulae. I.e., the cartographer devises a spherical-to-flat mapping according to some desirable but arbitrary property or constraint.
Perspective or not, a projection can be defined by two sets of mapping equations:
|Coordinate transformations defined by mapping relations|
Usually those relations are not functions, as the same point on the sphere may be represented by several points on the map. Instead of Cartesian distances, plane polar coordinates (radius , angle ) can be used, being in fact easier to express for many projections.
Although not generally presented here, inverse mapping makes possible calculating the geographic location given a point on a map or an aerial/satellite photograph. Thus, it is relevant to several problems, like interactive mapping applications which, when the user clicks on the map, respond depending on which building, street, city or whatever is georeferenced there. It is of course important for reprojecting, i.e., converting an already projected map to other projections, and translating between different geographic databases.
Even those without an interest in mathematics could get a fresh insight on the geographical sciences by understanding a projection formula or two; however, the reader can instead skip ahead to the main projection groups.
The next sections sketch the actual process for deriving mapping formulae for a few projections:
The shape of the map is defined beforehand for all but the Winkel, Kavrayskiy VII and (depending on the approach) Sanson-Flamsteed projections, where it is a consequence of the projections's constraints. Only Mollweide's, Craster's, azimuthal equal-area and Winkel derivations require basic calculus, numerical methods, or both.
Instead of commonplace degrees, minutes and seconds of arc, in cartographic mathematics any angles including latitude and longitude are more usefully measured in radians, since the length of a circular arc — thus distances along a great circle — can be directly calculated by its radius multiplied by the angle in radians. E.g., a straight angle of 180° is equivalent to radians; all points at latitudes 60°N and 60°S are units away from the Equator. Northern latitudes and eastern longitudes are arbitrarily considered positive angles; e.g., 45°S is expressed as .
Both forward and inverse mapping require a scaling factor, which determines but must not to be confused with the map's scale or scale factor: while the scaling factor is a single constant, the scale and scale factor unavoidably change depending on location and direction across the map. Equations included here express the scaling factor with the constant , which is a small non-negative fraction of the Earth's actual radius.