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Continuity and covariance Recall that for stationary processes so if C is continuous then Z is mean square continuous. To get results about sample paths need stronger conditions. Isotropic case: if then fractal dimension is 3- /2 2m times differentiable at origin yields paths having m derivatives
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Nugget and smoothness Matérn covariance, =3/2, =1. Nugget 2 = 0 (left); small (right) Simulated using RandomFields in R.
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Nonstationary covariance structure I: Deformations
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Evidence of anisotropy 15 o red 60 o green 105 o blue 150 o brown
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Another view of anisotropy
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General setup Z(x,t) = (x,t) + (x) 1/2 E(x,t) + (x,t) trend + smooth + error We shall assume that is known or constant t = 1,...,T indexes temporal replications E is L 2 -continuous, mean 0, variance 1, independent of the error C(x,y) = Cor(E(x,t),E(y,t)) D(x,y) = Var(E(x,t)-E(y,t)) (dispersion)
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Geometric anisotropy Recall that if we have an isotropic covariance (circular isocorrelation curves). If for a linear transformation A, we have geometric anisotropy (elliptical isocorrelation curves). General nonstationary correlation structures are typically locally geometrically anisotropic.
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The deformation idea In the geometric anisotropic case, write where f(x) = Ax. This suggests using a general nonlinear transformation. Usually d=2 or 3. G-plane D-space We do not want f to fold.
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Implementation Consider observations at sites x 1,...,x n. Let be the empirical covariance between sites x i and x j. Minimize where P(f) is a penalty for non-smooth transformations, such as the bending energy Solution: pair of thin-plate splines
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SARMAP An ozone monitoring exercise in California, summer of 1990, collected data on some 130 sites.
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Transformation This is for hr. 16 in the afternoon
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Identifiability Perrin and Meiring (1999): Let If (1) f and f -1 are differentiable in R n (2) (u) is differentiable for u>0 then (f, ) is unique up to a scaling for and a homothetic transformation for f (scaling, rotation, reflection)
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Richness Perrin & Senoussi (2000): Let f and f -1 be differentiable, and let C(x,y) be continuously differentiable. Then (stationarity) iff Let f(0)=0,c i i th column of. Then (isotropy) iff and
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Levy’s spatial Brownian motion
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Deformation of Brownian process Let and Then So this Gaussian process can be thought of as a stationary deformation. It is however not an istropic deformation.
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Estimating variability Resample time slices with replacement from the original data (to maintain spatial structure). Re-estimate deformation based on each bootstrap sample. Kriging estimates can be made based on each of the bootstrap estimates, to get a better sense of the variability.
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French rainfall data Altitude-adjusted 10-day aggregated rainfall data Nov-Dec 1975-1992 for 39 sites from Languedoc-Rousillon region of France.
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Estimated deformation
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G-plane equicorrelation contours
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D-plane Equicorrelation Contours
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Uncertainty in deformation Model refitted using 24 of the 36 sites.
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The smoothing parameter Cross-validation: Leave out sampling station i, estimate(θ,f) from remaining n-1 stations. Minimize the prediction error for site i, summed over i. Together with bootstrap estimate of variability, very computer intensive.
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Thin-plate splines
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A Bayesian implementation Likelihood: (Integrated) likelihood:
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Prior on deformation Linear part: fix two points in the G-D mapping put a (proper) prior on the remaining two parameters smoothing parameter
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Computation Metropolis-Hastings algorithm for sampling from highly multidimensional posterior. Given estimates of D-plane locations, f(x i ), the transformation is extrapolated to the whole domain using thin plate splines. Predictive distributions for (a) temporal variance at unobserved sites, (b) the spatial covariance for pairs of observed and/or unobserved sites, (c) the observation process at unobserved sites.
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California ozone
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Posterior samples
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Application to US presidential elections NY Times election map 2004
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Other applications Point process deformation (Jensen & Nielsen, Bernoulli, 2000) Deformation of brain images (Worseley et al., 1999)
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