It calculates the Lambert's equal area projection.
A two column matrix with the data. The first column is the altitude and the second is the longitude.
The spherical data are first rotated so that their mean direction is the north pole and then are projectedt on the plane tagent to the sphere at the north pole.
A two-column matrix with the projected points.
Kent, John T. (1982). The Fisher-Bingham distribution on the sphere. Journal of the Royal Statistical Society. Series B (Methodological) 44(1):71-80.
1 2 3 4
Add the following code to your website.
For more information on customizing the embed code, read Embedding Snippets.