Description Details Author(s) References See Also

This is a summary of the features and functionality of
georob, a package in **R** for robust geostatistical analyses.

georob is a package for robust analyses of geostatistical data.
Such data, say *y(s_i)*, are
recorded at a set of locations,
*s_i*, *i=1,2, …, n*, in a
domain *G in R^d*, *d in (1,2,3)*, along
with covariate information
*x_j(s_i)*, *j=1,2,
…, p*.

We use the following model for the data
*y_i=y(s_i)*:

*
Y(s_i) = Z(s_i) + ε = x(s_i)^T β + B(s_i) + ε_i,*

where
*Z(s_i) = x(s_i)^T β + B(s_i)* is the so-called signal,
*x(s_i)^Tβ*
is the external drift,
*{B(s)}* is an unobserved stationary or
intrinsic spatial Gaussian random field with zero mean, and
*ε_i* is an
*i.i.d* error from a possibly long-tailed distribution with scale parameter
*τ* (*τ^2* is usually called nugget effect).
In vector form the model is written as

*
Y = X β + B + ε,*

where *X* is the model matrix with the
rows
*
x^T(s_i)*.

The (generalized) covariance matrix of the vector of
spatial Gaussian random effects
*B*
is denoted by

*
E[B B^T] = Γ_θ = σ_n^2 I+σ^2 V_α =
σ_B^2 V_{α,ξ} = σ_B^2 ((1-ξ) I - ξ V_α)
,*

where
*σ_n^2*
is the variance of seemingly uncorrelated micro-scale variation in
*B(s)*
that cannot be resolved with the chosen sampling design,
*σ^2* is the variance of the captured auto-correlated variation in
*B(s)*,
*σ_B^2=σ_n^2+σ^2*
is the signal variance, and
*ξ=σ^2/σ_B^2*.
To estimate both
*σ_n^2* and *τ^2* (and not only their sum), one needs
replicated measurements for some of the
*s_i*.

We define
*V_{α}*
to be the matrix with elements

*
(V_{α})_ij = γ_0 - γ(|A (s_i - s_j )|),*

where the constant *γ_0* is chosen large enough so that
*V_{α}*
is positive definite,
*v()* is a valid stationary or intrinsic variogram, and
*
A = A(α, f_1, f_2; ω, φ, ζ)*
is a matrix that is used to model geometrically anisotropic auto-correlation.
In more detail,
*A*
maps an arbitrary point on an ellipsoidal surface with constant semi-variance in
*R^3*,
centred on the origin, and having lengths of semi-principal axes,
*p_1*,
*p_2*,
*p_3*,
equal to
*|p_1|=α*,
*|p_2|=f_1 α* and
*|p_3|=f_2 α*,
*0 < f_2 <= f_1 <= 1*,
respectively, onto the surface of the unit ball centred on the origin.

The orientation of the ellipsoid is defined by the three angles
*ω*, *φ* and *ζ*:

*ω*is the azimuth of

*p_1*(= angle between north and the projection of*p_1*onto the*x*-*y*-plane, measured from north to south positive clockwise in degrees),*φ*is 90 degrees minus the altitude of

*p_1*(= angle between the zenith and*p_1*, measured from zenith to nadir positive clockwise in degrees), and*ζ*is the angle between

*p_2*and the direction of the line, say*y'*, defined by the intersection between the*x*-*y*-plane and the plane orthogonal to*p_1*running through the origin (*ζ*is measured from*y'*positive counter-clockwise in degrees).

The transformation matrix is given by

*A=diag(1/α, 1/(f_1\,α),1/(f_2\,α)) (C_1, C_2, C_3)*

where

*C_1^T=( sinω sinφ, -cosω cosζ - sinω cosφ sinζ, cosω sinζ - sinω cosφ cosζ )
*

*C_2^T=( cosω sinφ, sinω cosζ - cosω cosφ sinζ, -sinω sinζ - cosω cosφcosζ )
*

*C_3^T=(cosφ, sinφ sinζ, sinφ cosζ )
*

To model geometrically anisotropic variograms in
*R^2*
one has to set *φ=90* and *f_2 = 1*,
and for *f_1 = f_2 = 1*
one obtains the model for isotropic auto-correlation
with range parameter *α*.
Note that for isotropic auto-correlation the software processes data for
which *d* may exceed 3.

Two remarks are in order:

Clearly, the (generalized) covariance matrix of the observations

*Y*is given by*Cov[Y, Y^T] = τ^2 I + Γ_θ.*Depending on the context, the term “variogram parameters” denotes sometimes all parameters of a geometrically anisotropic variogram model, but in places only the parameters of an isotropic variogram model, i.e.

*σ^2, …, α, …*and*f_1, …, ζ*are denoted by the term “anisotropy parameters”. In the sequel*θ*is used to denote all variogram and anisotropy parameters except the nugget effect*τ^2*.

The unobserved spatial random effects
*B* at the data locations
*s_i*
and the model parameters
*β*, *τ^2* and
*θ^T =
(σ^2, σ^2_n, τ^2, α, f_1, f_2,
ω, φ, ζ, …)
*
are unknown and are estimated in georob either by Gaussian or
robust restricted maximum likelihood (REML) or
Gaussian maximum likelihood (ML). Here `...`
denote further parameters of the variogram such as the smoothness parameter
of the Whittle-Mat¬érn model.

In brief, the robust REML method is based on the insight that for
given *θ* and *τ^2* the
Kriging predictions (= BLUP) of
*B* and the generalized least
squares (GLS = ML) estimates of
*β* can be obtained
simultaneously by maximizing

*
- ∑_i ( y_i - x^T(s_i)β - B(s_i) )^2 / τ^2
- B^T Γ_θ^-1 B
*

with respect to
*B* and
*β* e.g.
Harville (1977).
Hence, the BLUP of *B*,
ML estimates of *β*,
*θ* and *τ^2*
are obtained by maximizing

*
- log(det( τ^2 I + Γ_θ) )
- ∑_i ( y_i - x^T(s_i)β - B(s_i) )^2 / τ^2
- B^T Γ_θ^-1 B
*

jointly with respect to
*B*,
*β*,
*θ* and *τ^2*
or by solving the respective estimating equations.

The estimating equations can then by robustified by

replacing the standardized residuals, say

*ε_i/τ*, by a bounded or re-descending*ψ*-function,*ψ_c(ε_i/τ)*, of them (e.g. Marona et al, 2006, chap. 2) and byintroducing suitable bias correction terms for Fisher consistency at the Gaussian model,

see K¬ünsch et al. (2011) for details.
The robustified estimating equations
are solved numerically by a combination of iterated re-weighted least squares
(IRWLS) to estimate *B* and
*β* for given
*θ* and *τ^2*
and nonlinear root finding by the function
`nleqslv`

of the **R** package nleqslv
to get *θ* and *τ^2*.
The robustness of the procedure is controlled by the tuning parameter *c*
of the *ψ_c*-function. For *c>=1000* the algorithm computes
Gaussian (RE)ML estimates and customary plug-in Kriging predictions.
Instead of solving the Gaussian (RE)ML estimating equations, our software then
maximizes the Gaussian (restricted) log-likelihood using `nlminb`

or
`optim`

.

georob uses variogram models implemented in the **R** package
RandomFields (see `RMmodel`

).
Currently, estimation of the parameters of the following models is
implemented:

`"RMaskey"`

, `"RMbessel"`

, `"RMcauchy"`

,
`"RMcircular"`

, `"RMcubic"`

, `"RMdagum"`

,

`"RMdampedcos"`

, `"RMdewijsian"`

, `"RMexp"`

(default),
`"RMfbm"`

, `"RMgauss"`

,

`"RMgencauchy"`

,
`"RMgenfbm"`

, `"RMgengneiting"`

, `"RMgneiting"`

,
`"RMlgd"`

,

`"RMmatern"`

, `"RMpenta"`

, `"RMqexp"`

,
`"RMspheric"`

, `"RMstable"`

, `"RMwave"`

,

`"RMwhittle"`

.

For most variogram parameters, closed-form
expressions of *dγ/dθ_i* are used in the computations. However,
for the parameter *ν* of the models `"RMbessel"`

,
`"RMmatern"`

and `"RMwhittle"`

*dγ/dν* is evaluated numerically by the function
`numericDeriv`

, and this results in an increase in
computing time when *ν* is estimated.

Robust plug-in external drift point Kriging predictions
can be computed for an non-sampled location
*s_0*
from the covariates
*
x(s_0)*,
the estimated parameters
*hatβ*,
*hatθ*
and the predicted random effects
*hatB*
by

*
hatY(s_0) = hatZ(s_0) = x^T(s_0) hatβ + γ^T_hatθ(s_0) Γ_hatθ^-1 hatB,
*

where
*Γ_hatθ*
is the estimated (generalized) covariance matrix of
*B* and
*
γ^T_hatθ(s_0)*
is the vector with the estimated (generalized) covariances between
*B* and
*B(s_0)*.
Kriging variances can be computed as well, based on approximated covariances of
*hatB* and
*hatβ*
(see K¬ünsch et al., 2011, and appendices of
Nussbaum et al., 2012, for details).

The package georob provides in addition software for computing
robust external drift *block* Kriging predictions. The required
integrals of the generalized covariance function are computed by
functions of the **R** package constrainedKriging.

For the time being, the functionality of georob is limited
to robust geostatistical analyses of *single* response variables.
No software is currently available for robust multivariate geostatistical
analyses.
georob offers functions for:

Robustly fitting a spatial linear model to data that are possibly contaminated by independent errors from a long-tailed distribution by robust REML (see functions

`georob`

— which also fits such models efficiently by Gaussian (RE)ML —`profilelogLik`

and`control.georob`

).Extracting estimated model components (see

`residuals.georob`

,`rstandard.georob`

,

`ranef.georob`

).Robustly estimating sample variograms and for fitting variogram model functions to them (see

`sample.variogram`

and`fit.variogram.model`

).Model building by forward and backward selection of covariates for the external drift (see

`waldtest.georob`

,`step.georob`

,`add1.georob`

,`drop1.georob`

,`extractAIC.georob`

,

`logLik.georob`

,`deviance.georob`

). For a robust fit, the log-likelihood is not defined. The function then computes the (restricted) log-likelihood of an equivalent Gaussian model with heteroscedastic nugget (see`deviance.georob`

for details).Assessing the goodness-of-fit and predictive power of the model by

`K`-fold cross-validation (see`cv.georob`

and`validate.predictions`

).Computing robust external drift point and block Kriging predictions (see

`predict.georob`

,`control.predict.georob`

).Unbiased back-transformation of both point and block Kriging predictions of log-transformed data to the original scale of the measurements (see

`lgnpp`

).

Andreas Papritz [email protected]

http://www.step.ethz.ch/people/scientific-staff/andreas-papritz.html

Nussbaum, M., Papritz, A., Baltensweiler, A. and Walthert, L. (2012)
*Organic Carbon Stocks of Swiss Forest Soils*,
Institute of Terrestrial Ecosystems, ETH Zurich and
Swiss Federal Institute for Forest, Snow and Landscape Research
(WSL), pp. 51.
http://dx.doi.org/10.3929/ethz-a-007555133

K¬ünsch, H. R., Papritz, A., Schwierz, C. and Stahel, W. A. (in preparation) Robust Geostatistics.

K¬ünsch, H. R., Papritz, A., Schwierz, C. and Stahel, W. A. (2011) Robust estimation of the external drift and the variogram of spatial data. Proceedings of the ISI 58th World Statistics Congress of the International Statistical Institute. http://e-collection.library.ethz.ch/eserv/eth:7080/eth-7080-01.pdf

Maronna, R. A., Martin, R. D. and Yohai, V. J. (2006) Robust Statistics Theory and Methods, John Wiley \& Sons.

`georob`

for (robust) fitting of spatial linear models;
`georobObject`

for a description of the class `georob`

;
`plot.georob`

for display of RE(ML) variogram estimates;
`control.georob`

for controlling the behaviour of `georob`

;
`cv.georob`

for assessing the goodness of a fit by `georob`

;
`predict.georob`

for computing robust Kriging predictions; and finally
`georobModelBuilding`

for stepwise building models of class `georob`

;
`georobMethods`

for further methods for the class `georob`

,
`sample.variogram`

and `fit.variogram.model`

for robust estimation and modelling of sample variograms.

georob documentation built on Nov. 17, 2017, 5:53 a.m.

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