Hi Bob
Thank you for the useful references

I forgot to mention the fact that sometime when you detrend hydraulic head data using topography it could happen that the remaining residuals show a pure nugget effect (i.e. all the spatial continuity is described by the trend).

Then, (do you agree?) if you use depth to water (i.e. calculate the residuals subtracting the elevation) you could still have a trend. Sometime, in mountain you have that the water depth decreases with elevation: this is because the "water table" surface is not parallel with topography but converges to topographic surface going downhill.

Bye
Sebastiano

At 01.04 22/08/2006, Bob Harrington wrote:

M.J. Abedini wrote:

Another issue regarding detrending concerns with variogram modeling when trend coefficients are not given (i.e., unknown). I found literature on this issue very disparate. Any comments regarding unified approach on variogram modeling will be greatly appreciated.

This is not a unified approach, but considering Sebastiano Trevisani's suggestion of using topography as an external drift variable for kriging hydraulic head, the residual is simply depth to water from the land surface. Depth to water is typically available (or easily derivable from the DEM and head data) and the residual variogram could be modeled directly from depth to water.

--
Bob Harrington, Hydrologist
Inyo County Water Department
163 May St.
Bishop, CA 93514
(760) 872-1168
[EMAIL PROTECTED]


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