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**variogram**is an effective tool for describing the behavior of non-stationary, spatial random processes. It is used primarily in spatial statistics, geostatistics, and statistical design; In geostatistics, it is an “essential step” for analyzing spatial variability (Gómez-Hernández et al., 1999).

## The Variogram Function

The variogram measures dissimilarity in a relatively simple way. Pairs of data points are separated by a specified lag distance. Lags are chosen by the user, and depend on the type of data you’re dealing with. For example, lags might be calculated for data points that are 1 km apart, then 2 km apart, then 3 km apart. Or they might be calculated for points 5, 10, and 15 cm apart. A lag tolerance is set, so that values that aren’t exactly the specified distance fall into a specified lag. This is usually in between lags. For example, a distance of 7 cm rounds down to the 5 cm lag, and a 9 cm lag rounds up to a 10 cm lag (note: if you’re familiar with histogram bins, lag tolerances work in much the same way).

These lags are analyzed for their mean squared differences. The degree of dissimilarity between the Z(x) and Z(x + h) functions are defined with the variogram function γ(h):

Unlike the covariance function, you don’t need to know the mean. Plus, it can handle means that aren’t constant.

## References

Gómez-Hernández et al.(1999). geoENV II — Geostatistics for Environmental Applications. Springer Science & Business Media.

Orshansky, M. et al. (2007). Design for Manufacturability and Statistical Design: A Constructive Approach. Springer Science & Business Media.

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