Spatial Interpolation & Trend Surface Analysis Flashcards
Spatial interpolation background
- Data collection and analysis is expensive and infrequently collected
- Unknown values must be estimated from collected data that can be sampled
- Interpolation is procedure of estimating unknown values w/in area covered by existing observations
- x, y, and z are important
What can spatial interpolation be used for in GIS?
- Provide contours to display data graphically
- Calculate some property of the surface at a given point
- Calculate value for how good the model fits data (where it performs well vs. poorly)
Spatial interpolation is often used to aid what?
- Spatial decision making process both in physical and human geography
- ex. Mineral prospecting and hydrocarbon exploration
4 Types of Spatial Interpolation
- Global/Local
- Exact/Approximate
- Stochastic/Deterministic
- Gradual/Abrupt
Global Interpolators
- Determine a single function which is mapped across the whole region
- A change in one input value affects the entire map
Local Interpolators
- Algorithm is applied repeatedly to a small portion of total points
- A change in one input value only affects the result within the window
Exact Interpolators
- Surface passes through all points whose values are known
Approximate Interpolators
- Used when there is some uncertainty about the given surface values
Stochastic Method
- Trend Surface Analysis and Kriging
- Incorporates concept of randomness
- Interpolated surface is conceptualized as one of many that might have been observed, all of which could have produced known data points
- Allow for statistical significance of surface and uncertainty of predictions to be calculated
Gradual Interpolators
- Surface is smooth, no sharp boundaries
- Gradual changes
What can the statistical significance and uncertainty of a surface aid with?
- Use errors to ID places that need more sampling (margins, edge effects)
Abrupt Interpolators
- Quickly changing but continuous values
- Impermeable barriers (eg geological faults)
- High contrast from one variable to the next
Deterministic Methods
- Do no use probability theory
Distance Weighted
- IDW
- Simple
- Assigns values using weighted average
- Local algorithm, decide over what distance to process algorithm
IDW problems
- No assessment of prediction errors
- Can produce ‘bulls eyes’ around data locations
How does IDW work?
- Weights are a decreasing function of distance
- w (d) = 1/d^P, where p is power
- Larger the P, the greatest influence to values closest to the interpolated point
- Weights values higher that are close by to create predicted value
Would additional points improve IDW?
- Probably
- But if variable does not change much over an area then additional points can be redundant
- Possibly costly to collect redundant points
TSA, Fitting Polynomials: Global vs. Local
- Global: Single surface function for entire map
- Local: Estimate surface using only a selection of nearest points
TSA: Multiple functions
- Using a continuous to produce a surface, y = f (x1, x2…xn)
- 1 dependent variable, y
- k independent explanatory variables, x1, x2…xn
TSA: Power Functions
y = f(x^n)
- Linear: y = f (x) = a plus bx, no bend
- Quadratic: y = f (x^2), one bend
- Cubic: y = f (x^3), 2 bends
TSA: Fitting Polynomials
- Decomposes each observation on a spatially distributed variable into a component associated with global trends and a component associated with purely local effects
- Looks at residuals to see difference from global data
- De-trends data