vgram {gear} | R Documentation |
Empirical variogram
Description
vgram
calculates an empirical variogram. Note that, by convention,
the empirical variogram actually estimates the semivariogram, not the
theoretical variogram (which is twice the semivariogram).
Usage
vgram(
formula,
data,
coordnames = NULL,
nbins = 10,
maxd = NULL,
angle = 0,
ndir = 1,
type = "standard",
npmin = 2,
longlat = FALSE,
verbose = TRUE,
coords = NULL
)
Arguments
formula |
A formula describing the relationship between the response and any covariates of interest, e.g., response ~ 1. The variogram is computed for the residuals of the linear model |
data |
A |
coordnames |
The columns of |
nbins |
The number of bins (tolerance regions) to use when estimating the sample semivariogram. |
maxd |
The maximum distance used when calculating the semivariogram. Default is NULL, in which case half the maximum distance between coordinates is used. |
angle |
A single value (in degrees) indicating the starting direction for a directional variogram. The default is 0. |
ndir |
The number of directions for which to calculate a sample semivariogram. The default is 1, meaning calculate an omnidirection semivariogram. |
type |
The name of the estimator to use in the estimation process. The default is "standard", the typical method-of-moments estimator. Other options include "cressie" for the robust Cressie-Hawkins estimator, and "cloud" for a semivariogram cloud based on the standard estimator. If "cloud" is specified, the |
npmin |
The minimum number of pairs of points to use in the semivariogram estimator. For any bins with fewer points, the estimate for that bin is dropped. |
longlat |
A logical indicating whether Euclidean ( |
verbose |
Print computation information. Default is |
coords |
A deprecated argument. |
Details
Note that the directions may be different from other packages
(e.g., gstat
or geoR
packages) because those
packages calculate angles clockwise from the y-axis, which is
a convention frequently seen in geostatistics
(e.g., the GSLIB software library).
Additionally, note that calculating the empirical variogram for the residuals of lm(response ~ 1) will produce identical results to simply computing the sample semivariogram from the original response. However, if a trend is specified (the righthand side of ~ has non-trival covariates), then the empirical variogram of the residuals will differ from that of the original response. A trend should be specified when the mean is non-stationary over the spatial domain.
Value
Returns an evgram
object with components:
Author(s)
Joshua French
Examples
data(co)
v = vgram(Al ~ 1, co, ~ easting + northing)
plot(v)
v2 = vgram(Al ~ 1, co, c("easting", "northing"), angle = 22.5, ndir = 4)
plot(v2)