[R-sig-Geo] Problem with gstat variogram estimation
Paul Hiemstra
p.hiemstra at geo.uu.nl
Mon Oct 12 16:41:15 CEST 2009
Edzer Pebesma wrote:
> John, thanks for sharing this with r-sig-geo.
>
> As Thierry mentioned, the default model fitting procedure (fit.variogram
> in package gstat) uses weighted least squares, with weights proportional
> to N_h/(h^2). This explains why the first lag gets so much weight.
>
> For pure nugget models, this of course makes little sense; for other
> models it often does. Argument fit.method gives you somewhat more
> control. Give it value 1 to have N_h weights; give it value 6 to do
> unweighted averaging (I agree that this information should be in the
>
It is listed in the gstat documentation:
http://www.gstat.org/gstat.pdf
on page 42, in the middle.
cheers,
Paul
> fit.variogram documentation). The SSErr values will be uncomparable
> accross different weighting schemes, as you might expect.
> --
> Edzer
>
> Carson, John wrote:
>
>> I have found anomalous behavior in gstat's variogram estimation. I have listed 3 example variograms below for small data sets. In order to better estimate the nugget effect, I slightly perturbed the locations (by 1 foot increments) of duplicate results. The empirical variograms are given below.
>>
>> Before I did this (I averaged duplicate values initially), a Gaussian model with 0 nugget was selected for the second variogram and pure nugget models for the first and third. I am using the candidate model list ('Nug', 'Exp', 'Sph', 'Gau', 'Mat', 'Cir', 'Lin', 'Bes') and selecting the model based on SSErr for preliminary testing purposes. Afterward, the pure nugget models had the lowest SSErr and were selected. Note that the variogram fits are completely controlled by the short range variance, because even the original pure nugget models are substantially different in the estimate of the nugget. The fitted models are listed below. Just by inspection, based on the numbers of pairs in these examples, a pure nugget model should be about halfway between the empirical semivariance of the last lag and the average of the other lags. However, the fitted nuggets are almost identical to the semivariance of the first last (dist = 1.4).
>>
>> It seems to me that this must be due to a bug in the GSTAT code. I pointed this out to Edzer Pebesma, and he asked me to post it here.
>>
>> The variograms are
>>
>> tmp.vgm
>> [[1]]
>> np dist gamma dir.hor dir.ver id
>> 1 4 1.414214 0.14174537 0 0 PC1
>> 2 2 44.742603 6.70989788 0 0 PC1
>> 3 2 57.707880 1.76351594 0 0 PC1
>> 4 4 59.987678 1.52197310 0 0 PC1
>> 5 3 71.512518 1.21348268 0 0 PC1
>> 6 1 84.852877 0.05381849 0 0 PC1
>> 7 1 97.266495 1.21827622 0 0 PC1
>> 8 3 112.237133 5.07947925 0 0 PC1
>> 9 18 121.478856 1.93707676 0 0 PC1
>>
>> [[2]]
>> np dist gamma dir.hor dir.ver id
>> 1 4 1.414214 0.09725079 0 0 PC2
>> 2 2 44.742603 0.33598072 0 0 PC2
>> 3 2 57.707880 0.39088727 0 0 PC2
>> 4 4 59.987678 0.87315735 0 0 PC2
>> 5 3 71.512518 0.14944845 0 0 PC2
>> 6 1 84.852877 0.19809863 0 0 PC2
>> 7 1 97.266495 0.63557814 0 0 PC2
>> 8 3 112.237133 1.92063948 0 0 PC2
>> 9 18 121.478856 0.65468693 0 0 PC2
>>
>> [[3]]
>> np dist gamma dir.hor dir.ver id
>> 1 4 1.414214 0.035250817 0 0 PC3
>> 2 2 44.742603 0.105299796 0 0 PC3
>> 3 2 57.707880 0.020245674 0 0 PC3
>> 4 4 59.987678 0.124159836 0 0 PC3
>> 5 3 71.512518 0.008112554 0 0 PC3
>> 6 1 84.852877 0.034337591 0 0 PC3
>> 7 1 97.266495 0.053879459 0 0 PC3
>> 8 3 112.237133 0.021922987 0 0 PC3
>> 9 18 121.478856 0.085270969 0 0 PC3
>>
>>
>> But the fitted models are:
>>
>> tmp.vgm.fit
>> [[1]]
>> model psill range
>> 1 Nug 0.1483120 0
>>
>> [[2]]
>> model psill range
>> 1 Nug 0.09849419 0
>>
>> [[3]]
>> model psill range
>> 1 Nug 0.03535234 0
>>
>>
>>
>>
>> John H. Carson Jr., PhD
>> Senior Statistician
>> Applied Sciences & Engineering
>> Shaw Environmental & Infrastructure
>> 16406 US Rte 224 East
>> Findlay, OH 45840
>> Phone 419-425-6156
>> Fax 419-425-6085
>> john.carson at shawgrp.com
>>
>> http://www.shawgrp.com/
>> Shaw(tm) a world of Solutions(tm)
>>
>>
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--
Drs. Paul Hiemstra
Department of Physical Geography
Faculty of Geosciences
University of Utrecht
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