Environmental Modeling Spatial Interpolation. 1. Definition ► A procedure of estimating the values of properties at un-sampled sites ► The property must.

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Presentation transcript:

Environmental Modeling Spatial Interpolation

1. Definition ► A procedure of estimating the values of properties at un-sampled sites ► The property must be interval/ratio values ► The rational behind is that points close together in space are more likely to have similar values than points far apart

2. Termonology ► Point/line/areal interpolation point - point, point - line, point - areal

2. Terminology ► Global/local interpolation  Global - apply a single function across the entire region  Local - apply an algorithm to a small portion at a time

2. Terminology ► Exact/approximate interpolation  exact - honor the original points  approximate - when uncertainty is involved in the data ► Gradual/abrupt

3. Interpolation - Linear Assume that changes between two locations are linear

3. Interpolation - Linear ► Linear interpolation Known values Known and predicted values after interpolation

3. Interpolation - Proximal ► Thiesson polygon approach ► Local, exact, abrupt ► Perpendicular bisector of a line connecting two points ► Best for nominal data

Construction of Polygon Polygon of influence for x=180

Construction of Polygon Draw line segments between x and other points

Construction of Polygon Find the midpoint and bisect the lines.

Construction of Polygon Extend the bisecting lines till adjacent ones meet.

Construction of Polygon Continue this process.

3. Interpolation - Proximal

3. Interpolation – Proximal.. ►

3. Interpolation – B-spline ► Local, exact, gradual ► Pieces a series of smooth patches into a smooth surface that has continuous first and second derivatives ► Best for very smooth surfaces e.g. French curves ► enchCurve.html enchCurve.html enchCurve.html

3. Interpolation – Trend Surface ► Trend surface - polynomial approach ► Global, approximate, gradual ► Linear (1st order): z = a 0 + a 1 x + a 2 y ► Quadratic (2nd order): z = a 0 + a 1 x + a 2 y + a 3 x 2 z = a 0 + a 1 x + a 2 y + a 3 x 2 + a 4 xy + a 5 y 2 ► Cubic etc. ► Least square method

Trends of one, two, and three independent variables for polynomial equations of the first, second, and third orders (after Harbaugh, 1964).

3. Interpolation – Inverse Distance ► Local, approximate, gradual  w i z i 1 z = , w i = -----, or w i = e -pd i etc.  w i d i p

3. Interp – Fourier Series ► Sine and cosine approach ► Global, approximate, gradual ► Overlay of a series of sine and cosine curves ► Best for data showing periodicity

3. Interp – Fourier Series ► Fourier series Single harmonic in X 1 direction Two harmonics in X 1 direction Single harmonic in both X 1 and X 2 directions Two harmonics in both directions

3. Interp - Kriging ► Kriging - semivariogram approach, D.G. Krige ► Local, exact, gradual ► Spatial dependence (spatial autocorrelation) ► Regionalized variable theory, by Georges Matheron by Georges Matheron ► A situation between truly random and deterministic ► Stationary vs. non-stationary

3. Kriging ► First rule of geography: ► Everything is related to everything else. Closer things are more related than distant things ► By Waldo Tobler

3. Interp - Kringing ► Semivariogram 1 n  (h) =  (Z i - Z i+h ) 2 2 n i=1 ► Sill, range, nugget Sill Range Lag distance (h) Semivariance

3. Interp - Kringing ► Like inverse distance weighted, kriging considers the distance between a sample and the point of interest ► Kriging also considers the distance between samples, and declusters the crowded samples by the inverse of a covariance matrix ► Kriging also considers the distance between samples, and declusters the crowded samples by the inverse of a covariance matrix

3. Kriging Isotropy vs. anisotropy