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Interpolation Content Point data Interpolation Review Simple Interpolation Geostatistical Analyst in ArcGIS IDW in Geostatistical Analyst Semivariograms Auto-correlation Exploration Kriging

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Interpolation Content. Point data Interpolation Review Simple Interpolation Geostatistical Analyst in ArcGIS IDW in Geostatistical Analyst Semivariograms Auto-correlation Exploration Kriging. US Temperature Range. US Weather Stations. ~450 km. http://www.raws.dri.edu/. Interpolation. - PowerPoint PPT Presentation

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Page 1: Interpolation Content

Interpolation Content

• Point data• Interpolation Review• Simple Interpolation• Geostatistical Analyst in ArcGIS• IDW in Geostatistical Analyst • Semivariograms • Auto-correlation Exploration• Kriging

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US Temperature Range

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US Weather Stations

http://www.raws.dri.edu/~450 km

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Interpolation

• Interpolation is a method of constructing new data points within the range of a discrete set of known data points.

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John Snow• Soho, England, 1854• Cholera via polluted water

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Simple Interpolation

Mea

sure

d V

alue

s

Spatial Cross-section

50

3540

20

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Linear Interpolation

Mea

sure

d V

alue

s

Spatial Cross-section

50

3540

20

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Linear Interpolation

• Trend surface with order of 1M

easu

red

Val

ues

Spatial Cross-section

50

3540

20

55 4247 36 36 37 38 40 34 28 21

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Process• Obtain points with measurements• Evaluate data (autocorrelation)• Interpolate between the points using:

– Nearest (Natural) Neighbor– Trend (fitted polynomial)– Inverse Distance Weighting– Kriging– Splines– Density

• Convert the raster to vector using contours

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Inverse Distance Weighting

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Geostatistical Analyst

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Inverse Distance Weighting

• Points closer to the pixel have more “weight”

ArcGIS Help

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Inverse Distance Weighting

• Fk=new value• wi=weight• fi=data value

pki

n

j

pki

id

d

w

1

2

1

2

ki

n

jkj

i d

d

w

i

n

iik fwF

1

• Square root of distance to point over sum of square root of all distances

• General case• “Shepard's Method”

More information: http://en.wikipedia.org/wiki/Inverse_distance_weighting

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Geostatistical Analyst

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Geostatistical Analyst - IDW

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IDW – Cross Validation

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Issue with values 9 and 22

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IDW – Posterized Result

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IDW – Continuous Result

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Inverse Distance Weighting

• No value is outside the available range of values

• Assumes 0 uncertainty in the data• Smooth's the data

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Kriging

• Semivariograms– Analysis of the nature of autocorrelation– Determine the parameters for Kriging

• Kriging– Interpolation to raster– Assumes stochastic data– Can provide error surface

• Does not include field data error (spatial or measured)

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Semivariance

• Variance = (zi - zj)2

• Semivariance = Variance / 2

DistancePoint i Point j

zi

zj

zi - zj

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Semivariance

• For 2 points separated by 10 units with values of 0 and 2:

Sem

ivar

ianc

e

Distance Between Points

2 ( 0 – 2 )2 / 2 = 2

10

(zi - zj)2 / 2

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Binned and Averaged

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Variogram - Formal Definition

• For each pair of points separated by distance h:– Take the different between the attribute

values– Square it– Add to sum

• Divide the result by the number of pairs

 

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Range, Sill, Nugget

www.unc.edu

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Semivariogram

Andraski, B. J. Plant-Based Plume-Scale Mapping of Tritium Contamination in Desert Soils, vadzone, 2005 4: 819–827

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Synthetic Data Exploration

• To evaluate a new tool:– Create simple datasets in Excel or with a

Python• Ask your self:

– How does the tool work?– What are it’s capabilities?– What are it’s limitations?

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Linear Autocorrelationx y z

0 0 010 0 1020 0 2030 0 3040 0 4050 0 5060 0 6070 0 7080 0 8090 0 90100 0 100

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Linear Autocorrelation

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Randomx y z

0 0 0.76529110 0 0.3984520 0 0.50514530 0 0.89742140 0 0.81194950 0 0.97124160 0 0.48923470 0 0.26485480 0 0.08845590 0 0.668775100 0 0.741699

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Identical Valuesx y z

0 0 010 0 020 0 030 0 040 0 050 0 060 0 070 0 080 0 090 0 0100 0 0

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Ozone Semivariogram

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Ozone Semivariogram

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Ordinary Kriging - Example

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Ordinary Kriging - Example

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Ordinary Kriging - Example

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Ordinary Kriging - Example

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Categorical to Continuous

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Kriged Surface - Continuous

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Max Neighbors = 50

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Anisotropic Kriging

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Anisotropic Kriging

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IDW – Continuous Result

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Constant Kernel Smoothing

en.wikipedia.org

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Interpolation Software• ArcGIS with Geostatistical Analyst • R• Surfer (Golden Software) • Surface II package (Kansas Geological

Survey) • GEOEAS (EPA) • Spherekit (NCGIA, UCSB)• Matlab

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Cross-Validation

• Cross-Validation:– Comparing a model to a “different” set of

date to see if the model is “valid”• Approaches:

– Leave-one-out– Repeated random: test and training

datasets– K-fold: k equal size subsamples, one for

validation– 2-fold (holdout): two datasets of data, one

for testing, one for training, then switch

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More Resources• Geostatistical Analyst -> Tutorial• Wikipedia:

– http://en.wikipedia.org/wiki/Kriging• USDA geostatistical workshop

– http://www.ars.usda.gov/News/docs.htm?docid=12555

• EPA workshop with presentations on geostatistical applications for stream networks:– http://oregonstate.edu/dept/statistics/

epa_program/sac2005js.htm

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Literature• Lam, N.S.-N., Spatial interpolation methods: A

review, Am. Cartogr., 10 (2), 129-149, 1983.• Gold, C.M., Surface interpolation, spatial

adjacency, and GIS, in Three Dimensional Applications in Geographic Information Systems, edited by J. Raper, pp. 21-35, Taylor and Francis, Ltd., London, 1989.

• Robeson, S.M., Spherical methods for spatial interpolation: Review and evaluation, Cartog. Geog. Inf. Sys., 24 (1), 3-20, 1997.

• Mulugeta, G., The elusive nature of expertise in spatial interpolation, Cart. Geog. Inf. Sys., 25 (1), 33-41, 1999.

• Wang, F., Towards a natural language user interface: An approach of fuzzy query, Int. J. Geog. Inf. Sys., 8 (2), 143-162, 1994.

• Davies, C., and D. Medyckyj-Scott, GIS usability: Recommendations based on the user's view, Int. J. Geographical Info. Sys., 8 (2), 175-189, 1994.

• Blaser, A.D., M. Sester, and M.J. Egenhofer, Visualization in an early stage of the problem-solving process in GIS, Comp. Geosci, 26, 57-66, 2000.