v.kriging - GRASS GIS manual

Note: This document is for an older version of GRASS GIS that has been discontinued. You should upgrade, and read the current manual page.

NAME

v.kriging - Interpolates 2D or 3D raster based on input values located on 2D or 3D point vector layer (method ordinary kriging extended to 3D).

KEYWORDS

raster, 3D raster, ordinary kriging - for 2D and 3D data

SYNOPSIS

v.kriging

v.kriging --help

v.kriging [-2but] input=name [layer=string] phase=string [report=name] [hz_function=string] [output=string] [crossvalid=name] [vert_function=string] [final_function=string] [final_vert_function=string] [atrend=float] [btrend=float] [ctrend=float] [dtrend=float] [fileformat=string] icolumn=name [zcolumn=name] [azimuth=float] [zenith_angle=float] [lmax=float] [vmax=float] [lpieces=integer] [vpieces=integer] [td=float] [hz_nugget=float] [vert_nugget=float] [final_nugget=float] [final_vert_nugget=float] [hz_sill=float] [vert_sill=float] [final_sill=float] [final_vert_sill=float] [hz_range=float] [vert_range=float] [final_range=float] [final_vert_range=float] [--overwrite] [--help] [--verbose] [--quiet] [--ui]

Flags:

-2: Force 2D interpolation even if input is 3D
-b: Compute bivariate variogram (3D interpolation only)
-u: Compute univariate variogram (3D interpolation only)
-t: Eliminate trend if variogram is parabolic
--overwrite: Allow output files to overwrite existing files
--help: Print usage summary
--verbose: Verbose module output
--quiet: Quiet module output
--ui: Force launching GUI dialog

Parameters:

input=name [required]: Name of input vector points map; Or data source for direct OGR access
layer=string: Layer number or name; Vector features can have category values in different layers. This number determines which layer to use. When used with direct OGR access this is the layer name.; Default: 1
phase=string [required]: Phase of interpolation. In the initial phase, there is empirical variogram computed. In the middle phase, function of theoretical variogram is chosen by the user and its coefficients are estimated empirically. In the final phase, unknown values are interpolated using theoretical variogram from previous phase.; Options: initial, middle, final
report=name: File to write the report
hz_function=string: Horizontal variogram function; Options: linear, exponential, spherical, gaussian, bivariate
output=string: Name for output 2D/3D raster map
crossvalid=name: File to write the results of cross validation
vert_function=string: Vertical variogram function; Options: linear, exponential, spherical, gaussian, bivariate
final_function=string: Final variogram function (anisotropic or horizontal component of bivariate variogram); Options: linear, exponential, spherical, gaussian, bivariate
final_vert_function=string: Final variogram function (vertical component of bivariate variogram); Options: linear, exponential, spherical, gaussian, bivariate
atrend=float: Trend: f(x,y,z) = a*x + b*y + c*z + d; Default: 0.0
btrend=float: Trend: f(x,y,z) = a*x + b*y + c*z + d; Default: 0.0
ctrend=float: Trend: f(x,y,z) = a*x + b*y + c*z + d; Default: 0.0
dtrend=float: Trend: f(x,y,z) = a*x + b*y + c*z + d; Default: 0.0
fileformat=string: File format to save variogram plot (empty: preview in Gnuplot terminal); Options: cdr, dxf, eps, tex, pdf, png, svg
icolumn=name [required]: Attribute column containing input values for interpolation
zcolumn=name: Attribute column containing z coordinates (only for 3D interpolation based on 2D point layer)
azimuth=float: Azimuth of variogram computing (isotrophic); Default: 45.0
zenith_angle=float: Zenith angle of variogram computing (isotrophic); Default: 0.0
lmax=float: Maximum distance in horizontal direction
vmax=float: Maximum distance in horizontal direction (only for 3D variogram)
lpieces=integer: Number of horizontal lags
vpieces=integer: Number of vertical lags (only for 3D variogram)
td=float: Angle of variogram processing; Default: 45.0
hz_nugget=float: Nugget effect of horizontal variogram; Default: 0.0
vert_nugget=float: Nugget effect of vertical variogram; Default: 0.0
final_nugget=float: Nugget effect of anisotropic variogram (or horizontal component of bivariate variogram); Default: 0.0
final_vert_nugget=float: For bivariate variogram only: nuget effect of vertical component; Default: 0.0
hz_sill=float: Sill of horizontal variogram
vert_sill=float: Sill of vertical variogram
final_sill=float: Sill of anisotropic variogram (or horizontal component of bivariate variogram)
final_vert_sill=float: For bivariate variogram only: sill of vertical component
hz_range=float: Range of horizontal variogram
vert_range=float: Range of vertical variogram
final_range=float: Range of anisotropic variogram (or horizontal component of bivariate variogram)
final_vert_range=float: Range of final variogram: one value for anisotropic, two values for bivariate (hz and vert component)

DESCRIPTION
EXAMPLES
- 3D kriging
- 2D kriging
TODO
Recommendations
REFERENCES
SEE ALSO
REQUIREMENTS
AUTHOR

DESCRIPTION

v.kriging constructs 2D / 3D raster from the values located on discrete points using interpolation method ordinary kriging. In order to let the user decide on the process and necessary parameters, the module performance is divided into three phases:

initial phase computes experimental variogram.
- Please set up a name of the report file. The file will be created automatically in working directory to enable import of parameters from current to following phases. If the file has been deleted during the module performance, the user is asked to start interpolation again from the initial phase.
- Warning about particular point and "less than 2 neighbours in its closest surrounding. The perimeter of the surrounding will be increased..." indicates that variogram range should be shortened.
- There will appear some temporary files during variogram computation. They will be deleted automatically in following phase. If missing, the user is asked to repeat initial phase.
- It is not necessary to save experimental variogram plots. They just help to estimate parameters of theoretical variogram that will be computed in following step (output contains experimental and theoretical variogram plotted together).
in the middle phase, the user estimates theoretical variogram setting up the range (if necessary, the sill and the nugget effect as well) to fit the experimental variogram from previous phase.
- Default sill is calculated from variogram values, more details in (Stopkova, 2014).
- Save horizontal and vertical variogram plots using file=extension.
- Experimental anisotropic / bivariate variogram is plotted as a base for final theoretical variogram parameters estimation in final phase.
final phase performs interpolation based on parameters of theoretical variogram.
- Save anisotropic or bivariate variogram plot using file=extension.

EXAMPLES

To get optimal results, it is necessary to test various initial settings, anisotropic ratios and variogram functions. Input (2D or 3D point layer) must contain values to be interpolated in the attribute table.

3D kriging

General commands

v.kriging phase=initial in=input_layer icol=name report=report_file.txt file=png

v.kriging in=input_layer phase=middle hz_fun=exponential vert_fun=exponential ic=name file=png  \
hz_range=double vert_range=double [hz_sill=double vert_sill=double hz_nugget=double vert_nugget=double] -u

v.kriging in=input_layer phase=final final_fun=exponential final_range=double \
[final_sill=double final_nugget=double] icol=name file=png out=name crossval=crossval_file.txt

Commands based on the dataset of Slovakia 3D precipitation (Mitasova and Hofierka, 2004). For more detailed information check case studies. Another examples of 3D interpolation are available in (Stopkova, 2014).

v.kriging phase=initial in=precip3d@PERMANENT ic=precip report=precip3d.txt file=png --o

v.kriging in=precip3d@PERMANENT phase=middle hz_fun=exponential vert_fun=gaussian ic=precip file=png hz_range=100000. vert_range=1600 --o -u

v.kriging in=precip3d@PERMANENT phase=middle hz_fun=exponential vert_fun=gaussian ic=precip \
file=png hz_range=100000. vert_range=1600 --o -u

Note: 3D points in this example are concentrated on the Earth's surface. Thus the deeper / higher, the less accurate result of interpolation.

2D kriging

General commands

v.kriging phase=initial in=input_layer icol=name report=report_file.txt file=png -2

v.kriging in=input_layer phase=final final_function=linear icol=name file=png \
  out=name crossval=crossval_file.txt -2

Commands based on 500 random points extracted from input points of Digital Elevation Model (DEM) elev_lid792_randpts from the North Carolina dataset (Neteler and Mitasova, 2004). See the case studies.

v.kriging phase=initial in=elev_lid792_selected ic=value azimuth=45. td=45. \
report=lid792_500_linear.txt -2 --o

v.kriging in=elev_lid792_selected phase=final final_function=linear ic=value \
file=png out=lid792_500_linear crossval=lid792_500_xval_linear.txt -2 --o

TODO

anisotropy in horizontal direction missing
current version is suitable just for metric coordinate systems
enable mask usage
bivariate variogram needs to be rebuilt (theory)
2D interpolation from 3D input layer needs to be rebuilt (especially in case that there are too many points located on identical horizontal coordinates with different elevation)

Recommendations

In case of too much warnings about input points that have "less than 2 neighbours in its closest surrounding. The perimeter of the surrounding will be increased...", please consider shorter variogram range.
Save just figures with theoretical variogram (using file=extension in the middle and final phase). Experimental variograms are included in the theoretical variogram plot and separate "experimental" plots can be just temporal.

REFERENCES

Mitasova, H. and Hofierka, J. (2004). Slovakia Precipitation data. Available at https://grass.osgeo.org/download/data/.

Neteler, M. and Mitasova, H. (2004). Open Source GIS: A GRASS GIS Approach. 2nd Ed. 401 pp, Springer, New York. Online Supplement: https://grassbook.org

Stopkova, E. (2014). Development and application of 3D analytical functions in spatial analyses (Unpublished doctoral dissertation). The Department of Theoretical Geodesy, Faculty of Civil Engineering of Slovak University of Technology in Bratislava, Slovakia.

REQUIREMENTS

Gnuplot graphing utility, more
LAPACK / BLAS (libraries for numerical computing) for GMATH library (GRASS Numerical Library)
https://www.netlib.org/lapack (usually available on Linux distros)

AUTHOR

Eva Stopkova
functions taken from another modules are cited above the function or at the beginning of the file (e.g. quantile.cpp that uses slightly modified functions taken from the module r.quantile (Clements, G.))

SOURCE CODE

Available at: v.kriging source code (history)

Latest change: Monday Nov 11 18:04:48 2024 in commit: 59e289fdb093de6dd98d5827973e41128196887d