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Validation of the interpolation model

The chosen model (in practice the variogram) can be validated by interpolating observed values. If $ n$ observations $ Y(x_i), i=1,\ldots,n$ are available, the validation process proceeds as follows:



For each $ j$, $ j=1,\ldots,n$:



The chosen model can be considered theoretically valid if the error distribution is approximately gaussian with zero mean and unit variance ($ N(0,1)$, i.e. satisfies the following:

  1. there is no bias:

    $\displaystyle \frac{1}{n}\sum_{i=1}^n \epsilon _i \approx 0
$

  2. the estimation variance $ \sigma_i$ is coherent with the error standard deviation:

    $\displaystyle \frac{1}{n}\sum_{i=1}^n \left( \frac{Y^*_i-Y_i}{\sigma_i} \right)^2 =1
$

One can also look at the behavior of the interpolation error at each point looking at the mean square error of the vector $ \epsilon$:

$\displaystyle Q = \sqrt{\frac{1}{n} \sum_{i=1}^n \epsilon_i^2}
$

The uncertainties connected to the choice of the theoritcal variogram from the experimental data can be minimized by anaylizing the validation test. In fact, among all the possible variograms $ \gamma(h)$, that close to the origin display a slope compatible with the obesrvations and gives rise to a theoretically coherent model, one can choose the variogram with the smallest value of $ Q$.


next up previous contents
Next: Computational aspects Up: Geostatistics in Hydrology: Kriging Previous: Kriging with uncertainties   Contents
Mario Putti 2003-10-06