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Kriging for Weak or Second Order stationary RF

An RF is said to be second order stationary if:

  1. Constant mean:

    $\displaystyle E[Z(\vec{x},\xi)] = m$ (2.1)

  2. the autocovariance (another name for the covariance) is a function of the distance between the reference points $ \vec{x}_1$ and $ \vec{x}_2$:

    cov$\displaystyle [\vec{x}_1,\vec{x}_2] = E[(Z(\vec{x}_1,\xi) - m)(Z(\vec{x}_2,\xi) - m)] = C(\vec{h})$ (2.2)

In practice second order stationarity implies that the first two statistical moments (expected value and covariance) be translation invariant. Note that by saying that $ E[Z(\vec{x},\xi)] = m$ we imply that effectively the expected value taken on all the possible realizations $ \xi$ does not vary with space. However, for a given realization $ Z(\vec{x},\xi_1)$ is a function of $ \vec{x}$.

Because of (2.1), the covariance (2.2) can be written as:

cov$\displaystyle [\vec{x}_1,\vec{x}_2]$ $\displaystyle =$ $\displaystyle E[(Z(\vec{x}_1,\xi) - m)(Z(\vec{x}_2,\xi) - m)]$  
  $\displaystyle =$ $\displaystyle E[Z(\vec{x}_1,\xi)Z(\vec{x}_2,\xi)] -mE[Z(\vec{x}_2,\xi)]
- E[Z(\vec{x}_1,\xi)]m + m^2$  
  $\displaystyle =$ $\displaystyle E[Z(\vec{x}_1,\xi)Z(\vec{x}_2,\xi)] - m^2$ (2.3)

Obviously if $ \vec{h}=0$ we have the definition of variance, also called the ``dispersion'' variance:

$\displaystyle C(0) =$   var$\displaystyle [Z] = \sigma^2_Z
$

For simplicity of notation, from now on, we will denote $ x=\vec{x}$, $ h=\vec{h}$ and we will drop the variable $ \xi$ in the RF.



Subsections
next up previous contents
Next: Case with and known Up: Geostatistics in Hydrology: Kriging Previous: Statistical assumptions   Contents
Mario Putti 2003-10-06