| GeoModels-3D | R Documentation |
Conventions and current limitations for purely spatial models whose locations have three Cartesian coordinates.
For an irregular three-dimensional spatial data set, supply either an
N \times 3 numeric matrix in coordx, or three equal-length
vectors through coordx, coordy, and coordz. Use
grid = FALSE and distance = "Eucl".
Euclidean lags use all three coordinates. The principal fitting, covariance, variogram, Cholesky simulation, neighborhood, and global/local kriging paths support this representation.
Regular three-dimensional grids specified by three coordinate axes and
grid = TRUE are not implemented. Supply their Cartesian product as an
explicit N \times 3 matrix and use grid = FALSE.
For purely spatial univariate fields, spectral turning-bands simulation accepts
explicit irregular three-dimensional Euclidean coordinates through
GeoSimapprox(..., method = "TB", grid = FALSE). The same TB simulator
can be used by GeoVarest() and GeoVarestbootstrap() for such
fits. Three-dimensional TB does not support bivariate or spatio-temporal
models, and does not accept anisopars; transform coordinates explicitly
when needed. CE remains restricted to regular two-dimensional grids. Use
method = "cholesky" for unsupported three-dimensional cases.
Distances "Geod" and "Chor" require exactly two columns
(longitude and latitude) and cannot be combined with a third coordinate.
For GeoVariogramDir(), three-dimensional lag lengths use all three
coordinates, while direction classes are horizontal azimuths computed from
the x- and y-coordinate differences. This is not a full
three-dimensional directional analysis with azimuth and elevation.
GeoFit, GeoCovmatrix,
GeoVariogram, GeoVariogramDir,
GeoSim, GeoSimapprox,
GeoKrig, GeoKrigloc
Add the following code to your website.
For more information on customizing the embed code, read Embedding Snippets.