Experimenting with Google Earth

Kriging

Today, I will look at some of the assumptions underlying kriging, and important exploratory data analysis summaries, that should be obtained when performing kriging. As you know, Kriging is a geostatistical technique used to interpolate surfaces. It is similar to IDW in that the Z-values are weighted by some parameter. In IDW, Z-values are weighted by the inverse of the distance between the points. In kriging, z-values are weighted by the rate at which variance between sample points changes over space, that is, by the spatial autocorrelation between sample points.


Assumptions
Kriging should only be applied if the following underlying assumptions are met:

1. The data shows existence of second-order stationarity, i.e., at a minimum the mean and variance of the sample data should remain invariant in space. If the mean and variance of the samples are not stationary, then kriging may not be the best interpolation technique to apply.

2. The data represents one single homogenous domain.

3. A sufficient number of sample points should exist. Approximately 40 samples are needed to reasonably define and model a variogram, which can be used to produce an acceptable kriged
estimate.

EDA Output
In ArcGIS, before running kriging interpolation, you should explore the data before modeling the surface. Some things that should be explored include:
1. The number of sample points.
2. The minimum and maximum values in the distribution.
3. The variability of the distribution (variance and standard deviation)
4. The histogram of the distribution with coefficients of skewness and kurtosis,
5. Quantile-quantile (QQ) plots.
6. The semi-variogram cloud and fitted model. An example of a semi-variogram model is shown below:


1. At locations close to the origin, the semi-variances are low values, implying high levels of autocorrelation.
2. As distance (h) increases, variance also increases but levels off with increasing distance from the origin.
3. A constant variogram values imply that the variance between values does not change with distance.

In ArcGIS, the researcher can choose to fit one of several models to the variogram cloud in order to best capture the overall trend in the data (see illustration below). The best fit line can then be used to obtain values for all distance values (h). Alternative models include:

• Linear - a straight line with a positive slope.
• Spherical - rises rapidly then curves to the sill.
• Exponential – rises more gradually and is asymptotic to the sill.
• Gaussian – parabolic near the origin, then rises steeply toward the sill.

ArcGIS.com Viewer

ArcGIS.com viewer helps you to quickly create maps using a basemap from ESRI and additional layers found in ArcGIS.com. When creating these maps, one can set your area of interest, save the maps, and share them with others over the internet. These maps can be embedded in web pages to support themes on your webpage, or they can function as separate web applications. ESRI has created several templates that can be used to create these simple web applications. Visit ArcGIS.com at http://www.arcgis.com/home/webmap/viewer.html and follow the simple tutorial to start creating your own applications.


Here is a map of Guyana's ecumene from ArcGIS.com Viewer


View Larger Map. You can also use a hyperlink to access the map.