The Mercator projection is a cylindrical map projection that origins from the 16th century. It is widely recognized as the first regularly used map projection. It is a conformal projection in which the equator projects to a straight line at constant scale. The projection has the property that a rhumb line, a course of constant heading, projects to a straight line. This makes it suitable for navigational purposes.


Conformal cylindrical

Available forms

Forward and inverse, spherical and ellipsoidal

Defined area

Global, but best used near the equator





Input type

Geodetic coordinates

Output type

Projected coordinates


proj-string: +proj=merc


Applications should be limited to equatorial regions, but is frequently used for navigational charts with latitude of true scale (+lat_ts) specified within or near chart’s boundaries. It is considered to be inappropriate for world maps because of the gross distortions in area; for example the projected area of Greenland is larger than that of South America, despite the fact that Greenland’s area is \(\frac18\) that of South America [Snyder1987].

Example using latitude of true scale:

$ echo 56.35 12.32 | proj +proj=merc +lat_ts=56.5
3470306.37    759599.90

Example using scaling factor:

echo 56.35 12.32 | proj +proj=merc +k_0=2
12545706.61     2746073.80

Note that +lat_ts and +k_0 are mutually exclusive. If used together, +lat_ts takes precedence over +k_0.



All parameters for the projection are optional.


Latitude of true scale. Defines the latitude where scale is not distorted. Takes precedence over +k_0 if both options are used together.

Defaults to 0.0.


Scale factor. Determines scale factor used in the projection.

Defaults to 1.0.


Longitude of projection center.

Defaults to 0.0.


False easting.

Defaults to 0.0.


False northing.

Defaults to 0.0.


See proj -le for a list of available ellipsoids.

Defaults to “GRS80”.


Radius of the sphere given in meters. If used in conjunction with +ellps +R takes precedence.

Mathematical definition

Spherical form

For the spherical form of the projection we introduce the scaling factor:

\[k_0 = \cos \phi_{ts}\]

Forward projection

\[x = k_0R \lambda; \qquad y = k_0R \psi\]
\[\begin{split}\psi &= \ln \tan \biggl(\frac{\pi}{4} + \frac{\phi}{2} \biggr)\\ &= \sinh^{-1}\tan\phi\end{split}\]

The quantity \(\psi\) is the isometric latitude.

Inverse projection

\[\lambda = \frac{x}{k_0R}; \qquad \psi = \frac{y}{k_0R}\]
\[\begin{split}\phi &= \frac{\pi}{2} - 2 \tan^{-1} \exp(-\psi)\\ &= \tan^{-1}\sinh\psi\end{split}\]

Ellipsoidal form

For the ellipsoidal form of the projection we introduce the scaling factor:

\[k_0 = m( \phi_{ts} )\]


\[m(\phi) = \frac{\cos\phi}{\sqrt{1 - e^2\sin^2\phi}}\]

\(a\,m(\phi)\) is the radius of the circle of latitude \(\phi\).

Forward projection

\[x = k_0 a \lambda; \qquad y = k_0 a \psi\]
\[\begin{split}\psi &= \ln\tan\biggl(\frac\pi4 + \frac{\phi}2\biggr) -\frac12 e \ln \biggl(\frac{1 + e \sin\phi}{1 - e \sin\phi}\biggr)\\ &= \sinh^{-1}\tan\phi - e \tanh^{-1}(e \sin\phi)\end{split}\]

Inverse projection

\[\lambda = \frac{x}{k_0 a}; \quad \psi = \frac{y}{k_0 a}\]

The latitude \(\phi\) is found by inverting the equation for \(\psi\) iteratively.

Further reading

  1. Wikipedia

  2. Wolfram Mathworld