1 / 31

Geostatistics

Geostatistics. Mike Goodchild. Spatial interpolation. A field variable is interval/ratio z = f ( x , y ) sampled at a set of points How to estimate/guess the value of the field at other points?. Characteristics of interpolated surfaces. Representation raster, isolines, TIN Form

jillian
Télécharger la présentation

Geostatistics

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. Geostatistics Mike Goodchild

  2. Spatial interpolation • A field • variable is interval/ratio • z = f(x,y) • sampled at a set of points • How to estimate/guess the value of the field at other points?

  3. Characteristics of interpolated surfaces • Representation • raster, isolines, TIN • Form • rugged or smooth • exact or approximate • continuity • 0-order • 1-order • 2-order • Uncertainty • variance estimators?

  4. Linear interpolation • Along a line • geocoding with address ranges x2,y2 address2 x,y address x1,y1 address1

  5. In a triangle 30 40 20

  6. (24) 30 20 40 30 (34) In a rectangle • Bilinear interpolation (29)

  7. Characteristics of linear interpolation • Exact • 0-order continuity • Contours are straight • but not parallel in bilinear case

  8. IDW • Advantages • quick, universal, theory-free • Disadvantages • theory-free • directional effects • non-spatial • characteristics of a weighted average • when all weights are non-negative

  9. 4.5 4 3.5 3 2.5 2 1.5 1 0.5 1 4 7 0 10 13 16 19 22 25 28 37 40 43 46 49 52 55 58 61 64 76 79 82 85 88 91 94 97 31 34 67 70 73 100

  10. Characteristics of IDW surfaces • Pass through each data point (exact) • if negative power distance function • 1/0b =  • 0-, 1-, 2-order continuous • except at data points • Underestimate peaks • volcanoes • unless peak is observation point • Extrapolate to the global mean • Noisy extrapolations

  11. Kriging • Geostatistics as theoretical framework • Estimation of parameters from data • Use of estimated model to control interpolation • Many versions • not a simple black box • highlights • demonstration

  12. The variogram • Relationship between variance and distance • Formalization of Tobler's First Law • Estimated from data • how well can a given data set estimate variogram? • distribution of sample points is critical • at peaks and pits • samples the range of possible distances • uniform spacing not desirable • but often out of the user's control

  13. Estimation • Data points zi(xi) • Interpolate at x • stochastic process • multiple realizations • variance obtained from variogram • A set of weights i unique to x • chosen such that the estimate is • unbiased • minimum variance

  14. Kriging prediction

  15. Results of Kriging • A mean surface • A variance surface • minimum at observation points • Mean surface is smoother than any realization • is not a possible realization • a mean map is not a possible map • compare a univariate process • average rainfall versus rainfall from a single storm • conditional simulation

  16. Kriging standard error

  17. Kriging variants • Co-Kriging • interpolation process guided by another variable (field) • hard and soft data • observations of interpolated data are hard • guiding variable is soft

  18. 70 55 83 68 z = f (elevation)

  19. Co-Kriging • Linear relationship f • Point observations are hard • accurate, sparse • Elevation observations are soft • inaccurate (errors in measurement or prediction) • dense

  20. Co-Kriging prediction

  21. Co-Kriging standard error

  22. Indicator Kriging • Binary field • c {0,1} • Obtained by thresholding an interval/ratio field • c=1 if z>t else c=0 • estimate variogram from observations of c • z is hidden • The multivariate case • sequential assignment

  23. Indicator Kriging • Assign Class 1, notClass 1 • Among notClass 1, assign Class 2, notClass 2 • Continue to Class n-1 • notClass n-1 = Class n

  24. Universal Kriging • Simple Kriging is all second order • trend results from random walk • Stochastic process plus trend • trend is first order • remove trend before analysis • restore trend after analysis

  25. Advantages and disadvantages • Theoretically based • Not a black box • Statistical • variance estimates • Sensitivity to sample design

More Related