Parameters:
input input raster map from source location
output output raster map for current location
mapset mapset of input map
location source location of input map
dbase database of input map
method interpolation method to use
options: nearest,bilinear,cubic
default: nearest
resolution resolution of output map
Introduction
Map projections
Map projections are a method of representing information from a curved surface (usually a spheroid) in two dimensions, typically to allow indexing through cartesian coordinates. There are a wide variety of projections, with common ones divided into a number of classes, including cylindrical and pseudo-cylindrical, conic and pseudo-conic, and azimuthal methods, each of which may be conformal, equal-area, or neither.
The particular projection chosen depends on the purpose of the project, and the size, shape and location of the area of interest. For example, normal cylindrical projections are good for maps which are of greater extent east-west than north-south and in equatorial regions, while conic projections are better in mid-latitudes; transverse cylindrical projections are used for maps which are of greater extent north-south than east-west; azimuthal projections are used for polar regions. Oblique versions of any of these may also be used. Conformal projections preserve angular relationships, and better preserve arc-length, while equal-area projections are more appropriate for statistical studies and work in which the amount of material is important.
Projections are defined by precise mathematical relations, so the method of projecting coordinates from a geographic reference frame (latitude-longitude) into a projected cartesian reference frame (eg metres) is governed by these equations. Inverse projections can also be achieved. The public-domain Unix software package proj [1] has been designed to perform these transformations, and the user's manual contains a detailed description of over 100 useful projections. This also includes a programmers library of the projection methods to support other software development.
Thus, converting a "vector" map - in which objects are located with arbitrary spatial precision - from one projection into another is usually accomplished by a simple two-step process: first the location of all the points in the map are converted from the source through an inverse projection into latitude-longitude, and then through a forward projection into the target. (Of course the procedure will be one-step if either the source or target is in geographic coordinates.)
Converting a "raster map", or image, between different projections, however, involves additional considerations. A raster may be considered to represent a sampling of a process at a regular, ordered set of locations. The set of locations that lie at the intersections of a cartesian grid in one projection will not, in general, coincide with the sample points in another projection. Thus, the conversion of raster maps involves an interpolation step in which the values of points at intermediate locations relative to the source grid are estimated.
Projecting maps within the GRASS GIS
GIS data capture, import and transfer often requires a projection step, since the source or client will frequently be in a different projection to the working projection.
In some cases it is convenient to do the conversion outside the package, prior to import or after export, using software such as proj [1]. This is certainly the easiest method for site-lists, since there is no topology to be preserved, and proj can be used to process simple lists with a one-line command.
The format of files describing maps containing lines and arcs is generally more complex, as even in ascii parts of the files will describe topology, and not just locations. In the GRASS GIS package a program v.proj is provided to convert "vector" maps, transferring topology and attributes as well as node locations. This program uses the projection definition and parameters which are stored in the PROJ_INFO and PROJ_UNITS files in the PERMANENT mapset directory for every GRASS location.
However, although it is oriented mainly towards operations on raster maps, the standard GRASS distribution includes this r.proj module to convert raster maps. That is the purpose of the program described here.
Design of r.proj
As discussed briefly above, the fundamental step in re-projecting a
raster is resampling the source grid at locations corresponding to the
intersections of a grid in the target projection. The basic procedure for
accomplishing this, therefore, is as follows:
r.proj converts a map to a new geographic projection. It reads a
map from a different location, projects it and write it out
to the current location. The projected data is resampled with
one of three different methods: nearest neighbor, bilinear and
cubic convolution.
Note that, following normal GRASS conventions, the coverage and resolution of the resulting grid is set by the current region settings, which may be adjusted using g.region. The target raster will be relatively unbiased for all cases if its grid has a similar resolution to the source, so that the resampling/interpolation step is only a local operation. If the resolution is changed significantly, then the behaviour of the generalisation or refinement will depend on the model of the process being represented. This will be very different for categorical versus numerical data. Note that three methods for the local interpolation step are provided.
References:
[1]Evenden, G.I. (1990) Cartographic projection procedures for the UNIX environment - a user's manual. USGS Open-File Report 90-284 (Also see Interim Report and 2nd Interim Report on Release 4, Evenden 1994).
Man page text from S.J.D. Cox, AGCRC, CSIRO Exploration & Mining, Nedlands, WA