earthdistance module provides two different approaches to calculating great circle distances on the surface of the Earth. The one described first depends on the
cube module. The second one is based on the built-in
point data type, using longitude and latitude for the coordinates.
In this module, the Earth is assumed to be perfectly spherical. (If that's too inaccurate for you, you might want to look at the PostGIS project.)
cube module must be installed before
earthdistance can be installed (although you can use the
CASCADE option of
CREATE EXTENSION to install both in one command).
It is strongly recommended that
cube be installed in the same schema, and that that schema be one for which CREATE privilege has not been and will not be granted to any untrusted users. Otherwise there are installation-time security hazards if
earthdistance's schema contains objects defined by a hostile user. Furthermore, when using
earthdistance's functions after installation, the entire search path should contain only trusted schemas.
Data is stored in cubes that are points (both corners are the same) using 3 coordinates representing the x, y, and z distance from the center of the Earth. A domain
cube is provided, which includes constraint checks that the value meets these restrictions and is reasonably close to the actual surface of the Earth.
The radius of the Earth is obtained from the
earth() function. It is given in meters. But by changing this one function you can change the module to use some other units, or to use a different value of the radius that you feel is more appropriate.
This package has applications to astronomical databases as well. Astronomers will probably want to change
earth() to return a radius of
180/pi() so that distances are in degrees.
Functions are provided to support input in latitude and longitude (in degrees), to support output of latitude and longitude, to calculate the great circle distance between two points and to easily specify a bounding box usable for index searches.
The provided functions are shown in Table F.6.
Table F.6. Cube-based Earthdistance Functions
||Returns the assumed radius of the Earth.|
||Converts the normal straight line (secant) distance between two points on the surface of the Earth to the great circle distance between them.|
||Converts the great circle distance between two points on the surface of the Earth to the normal straight line (secant) distance between them.|
||Returns the location of a point on the surface of the Earth given its latitude (argument 1) and longitude (argument 2) in degrees.|
||Returns the latitude in degrees of a point on the surface of the Earth.|
||Returns the longitude in degrees of a point on the surface of the Earth.|
||Returns the great circle distance between two points on the surface of the Earth.|
||Returns a box suitable for an indexed search using the cube
The second part of the module relies on representing Earth locations as values of type
point, in which the first component is taken to represent longitude in degrees, and the second component is taken to represent latitude in degrees. Points are taken as (longitude, latitude) and not vice versa because longitude is closer to the intuitive idea of x-axis and latitude to y-axis.
A single operator is provided, shown in Table F.7.
Table F.7. Point-based Earthdistance Operators
||Gives the distance in statute miles between two points on the Earth's surface.|
Note that unlike the
cube-based part of the module, units are hardwired here: changing the
earth() function will not affect the results of this operator.
One disadvantage of the longitude/latitude representation is that you need to be careful about the edge conditions near the poles and near +/- 180 degrees of longitude. The
cube-based representation avoids these discontinuities.
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