A Covariance Conversion Approach of Gamma Random Field Simulation

Similar documents
Gamma random field simulation by a covariance matrix transformation method

Acceptable Ergodic Fluctuations and Simulation of Skewed Distributions

Water shortage risk assessment using spatiotemporal flow simulation

Handbook of Spatial Statistics Chapter 2: Continuous Parameter Stochastic Process Theory by Gneiting and Guttorp

Entropy of Gaussian Random Functions and Consequences in Geostatistics

PRODUCING PROBABILITY MAPS TO ASSESS RISK OF EXCEEDING CRITICAL THRESHOLD VALUE OF SOIL EC USING GEOSTATISTICAL APPROACH

MA/ST 810 Mathematical-Statistical Modeling and Analysis of Complex Systems

Statistícal Methods for Spatial Data Analysis

A MultiGaussian Approach to Assess Block Grade Uncertainty

Estimating Design Rainfalls Using Dynamical Downscaling Data

Geostatistics for Gaussian processes

Preliminary statistics

Multivariate Distributions

Spatial Interpolation & Geostatistics

The Proportional Effect of Spatial Variables

PGA Semi-Empirical Correlation Models Based on European Data

COMPARISON OF DIGITAL ELEVATION MODELLING METHODS FOR URBAN ENVIRONMENT

Lecture 2: Repetition of probability theory and statistics

Spatial Backfitting of Roller Measurement Values from a Florida Test Bed

Latin Hypercube Sampling with Multidimensional Uniformity

x. Figure 1: Examples of univariate Gaussian pdfs N (x; µ, σ 2 ).

Optimization Problems with Probabilistic Constraints

Non-Ergodic Probabilistic Seismic Hazard Analyses

Modeling of Atmospheric Effects on InSAR Measurements With the Method of Stochastic Simulation

7 Geostatistics. Figure 7.1 Focus of geostatistics

11/8/2018. Spatial Interpolation & Geostatistics. Kriging Step 1

Monte Carlo Simulation. CWR 6536 Stochastic Subsurface Hydrology

Simulating Spatial Distributions, Variability and Uncertainty of Soil Arsenic by Geostatistical Simulations in Geographic Information Systems

Climate Change: the Uncertainty of Certainty

Multiple Random Variables

Lecture Note 1: Probability Theory and Statistics

Stepwise Conditional Transformation for Simulation of Multiple Variables 1

Basics of Point-Referenced Data Models

Algorithms for Uncertainty Quantification

A Program for Data Transformations and Kernel Density Estimation

A STUDY OF MEAN AREAL PRECIPITATION AND SPATIAL STRUCTURE OF RAINFALL DISTRIBUTION IN THE TSEN-WEN RIVER BASIN

Correcting Variogram Reproduction of P-Field Simulation

Generating Spatial Correlated Binary Data Through a Copulas Method

Investigation of Monthly Pan Evaporation in Turkey with Geostatistical Technique

Finding the Nearest Positive Definite Matrix for Input to Semiautomatic Variogram Fitting (varfit_lmc)

Kriging for processes solving partial differential equations

Dale L. Zimmerman Department of Statistics and Actuarial Science, University of Iowa, USA

Geostatistics: Kriging

Application of Copulas as a New Geostatistical Tool

Review of Probability Theory

Conditional Simulation of Random Fields by Successive Residuals 1

1: PROBABILITY REVIEW

Advanced analysis and modelling tools for spatial environmental data. Case study: indoor radon data in Switzerland

The Wishart distribution Scaled Wishart. Wishart Priors. Patrick Breheny. March 28. Patrick Breheny BST 701: Bayesian Modeling in Biostatistics 1/11

Advances in Locally Varying Anisotropy With MDS

Joint Gaussian Graphical Model Review Series I

Appendix of the paper: Are interest rate options important for the assessment of interest rate risk?

Probabilistic evaluation of liquefaction-induced settlement mapping through multiscale random field models

Index. Geostatistics for Environmental Scientists, 2nd Edition R. Webster and M. A. Oliver 2007 John Wiley & Sons, Ltd. ISBN:

3/10/03 Gregory Carey Cholesky Problems - 1. Cholesky Problems

Multivariate Random Variable

Coregionalization by Linear Combination of Nonorthogonal Components 1

On dealing with spatially correlated residuals in remote sensing and GIS

Statistical Inference with Monotone Incomplete Multivariate Normal Data

Spatial Cross-correlation Models for Vector Intensity Measures (PGA, Ia, PGV and Sa s) Considering Regional Site Conditions

Beta-Binomial Kriging: An Improved Model for Spatial Rates

Next is material on matrix rank. Please see the handout

Simulating Uniform- and Triangular- Based Double Power Method Distributions

A Probability Review

Dependence. Practitioner Course: Portfolio Optimization. John Dodson. September 10, Dependence. John Dodson. Outline.

Assessing the uncertainty associated with intermittent rainfall fields

Geostatistical Modeling for Large Data Sets: Low-rank methods

BAYESIAN MODEL FOR SPATIAL DEPENDANCE AND PREDICTION OF TUBERCULOSIS

LIST OF FORMULAS FOR STK1100 AND STK1110

On prediction and density estimation Peter McCullagh University of Chicago December 2004

Derivatives of Spatial Variances of Growing Windows and the Variogram 1

ESTIMATING THE MEAN LEVEL OF FINE PARTICULATE MATTER: AN APPLICATION OF SPATIAL STATISTICS

VALUES FOR THE CUMULATIVE DISTRIBUTION FUNCTION OF THE STANDARD MULTIVARIATE NORMAL DISTRIBUTION. Carol Lindee

Soil Moisture Modeling using Geostatistical Techniques at the O Neal Ecological Reserve, Idaho

3D geostatistical porosity modelling: A case study at the Saint-Flavien CO 2 storage project

Semiparametric Gaussian Copula Models: Progress and Problems

Applications of Randomized Methods for Decomposing and Simulating from Large Covariance Matrices

Random Matrix Eigenvalue Problems in Probabilistic Structural Mechanics

A Few Special Distributions and Their Properties

L2: Review of probability and statistics

Using linear and non-linear kriging interpolators to produce probability maps

Models for spatial data (cont d) Types of spatial data. Types of spatial data (cont d) Hierarchical models for spatial data

Advanced Experimental Design

Human-Oriented Robotics. Probability Refresher. Kai Arras Social Robotics Lab, University of Freiburg Winter term 2014/2015

BME STUDIES OF STOCHASTIC DIFFERENTIAL EQUATIONS REPRESENTING PHYSICAL LAW

Chapter 5 continued. Chapter 5 sections

Comparing Non-informative Priors for Estimation and Prediction in Spatial Models

MAXIMUM ENTROPY-BASED UNCERTAINTY MODELING AT THE FINITE ELEMENT LEVEL. Pengchao Song and Marc P. Mignolet

Structural Reliability

Probability and Stochastic Processes

SPATIAL VARIABILITY MAPPING OF N-VALUE OF SOILS OF MUMBAI CITY USING ARCGIS

COLLOCATED CO-SIMULATION USING PROBABILITY AGGREGATION

Financial Econometrics and Quantitative Risk Managenent Return Properties

Anomaly Density Estimation from Strip Transect Data: Pueblo of Isleta Example

STAT Chapter 5 Continuous Distributions

Accounting for Population Uncertainty in Covariance Structure Analysis

Geostatistics in Hydrology: Kriging interpolation

4th HR-HU and 15th HU geomathematical congress Geomathematics as Geoscience Reliability enhancement of groundwater estimations

Building Blocks for Direct Sequential Simulation on Unstructured Grids

1 Data Arrays and Decompositions

Transcription:

Proceedings of the 8th International Symposium on Spatial Accuracy Assessment in Natural Resources and Environmental Sciences Shanghai, P. R. China, June 5-7, 008, pp. 4-45 A Covariance Conversion Approach of Gamma Random Field Simulation Jun-Jih Liou, Yuan-Fong Su, Jie-Lun Chiang and Ke-Sheng Cheng + Department of Bioenvironmental Systems Engineering, National Taiwan University, Taiwan Dept. of Soil and ater Conservation, National Pingtung University of Science and Technology, Taiwan Abstract. In studies involving environmental risk assessment, random field generators such as the sequential Gaussian simulation are often used to yield realizations of a Gaussian random field, and then realizations of the non-gaussian target random field are obtained by an inverse-normal transformation. Such simulation requires a set of observed data for estimation of the empirical cumulative distribution function and covariance function of the random field under investigation. However, such observed-data-based simulation will not work if no observed data are available and realizations of a non-gaussian random field with specific probability density and covariance function are needed. In this paper we present details of a gamma random field simulation approach which does not require a set of observed data. A key element of the approach lies on the theoretical relationship between the covariance functions of a gamma random field and its corresponding standard normal random field. The proposed gamma random field simulation technique is composed of three sequential components: ( covariance function conversion between a gamma random field and a corresponding Gaussian random field, ( generating realizations of a Gaussian random field with standard normal density and the desired covariance function, and ( transforming Gaussian realizations to corresponding gamma realizations. Through a set of devised simulation scenarios, the proposed technique is shown to be capable of generating realizations of the given gamma random fields. The approximation function of the gamma-gaussian covariance conversion works well for coefficient of skewness of the gamma density not exceeding.0. Keywords: stochastic simulation, gamma distribution, geostatistics, random field simulation. Introduction Random field simulation has been widely applied to studies involving environmental risk assessment such as soil contamination, flood inundation, solutes transport in a porous medium, etc. Many of these applications use random field generators to generate large sets of realizations which can be characterized by the desired Gaussian distribution and spatial variation structure (or semi-variogram. However, many environmental variables are non-gaussian and asymmetric. For practical applications involving uncertainty or risk mapping of these variables, observed data are transformed to normal scores in the beginning, and sequential Gaussian simulation (SGS is then performed in normal space. Finally, data generated by SGS are back-transformed to realizations of the target variables. In such practices, normal transformation of the observed data and inversenormal transformation of the simulated data are generally based on the empirical cumulative distribution function (ECDF of the observed data. From a theoretical point of view, if no observed data are available and we want to generate realizations of a non-gaussian random field with specific probability density and covariance function, the above observed-data-based SGS process will not work since the covariance function of the Gaussian random field cannot be estimated without a set of normal scores transformed from observed data. In this paper a gamma random field simulation approach which does not require observed data is presented. + Corresponding author. Tel.: +886--66465; fax: +886--65854. E-mail address: rslab@ntu.edu.tw ISBN: -8466-70-8, ISBN: 978--8466-70-

. Conceptual description of the proposed approach Based on the bivariate gamma simulation approach proposed by Cheng et al. (008, simulation of a gamma random field can be achieved in a similar, yet more complicated, manner. Through a theoretical conversion between ρ UV and ρ XY, random samples of a pair of bivariate gamma random variates (X,Y with desired marginal densities and correlation coefficient ρ XY can be obtained by first generating random samples of a corresponding pair of bivariate variates (U,V with standard normal density and correlation coefficient ρ UV, followed by a Gaussian-to-gamma transformation. In contrast to stochastic simulation of bivariate random variables, stochastic simulation of a random field Z(x involves correlations among a set of random variables which are expressed in terms of a multivariate covariance (or correlation matrix. For random field simulation, the whole process is composed of three sequential components: Converting the covariance function C Z of a gamma random field Z(x to the covariance function C of a corresponding Gaussian random field (x. In a sequential random field simulation process, the covariance function appears as a covariance matrix which involves a point for random number generation and its neighboring points. Thus, conversion between the covariance function C Z and C is equivalent to conversion between the covariance matrices Z and. Generating realizations of the Gaussian random field with covariance function C, and Transforming realizations of (x to corresponding realizations of the gamma random field Z(x.. Methodology and detailed procedures.. Sequential Gaussian simulation Given a homogeneous and isotropic random field { Z ( x, x Ω} with known probability density function f Z (z and covariance function C Z (or semi-variogram γ Z, we want to generate as many random samples (realizations of the random field. For a set of (p+q normally distributed random variables, say = (, L, p + q, the multivariate joint density is given by (Morrison, 990 ( w μ ' ( w μ f ( w = e ( p+ q / / ( (π where is the covariance matrix with ( p + q ( p + q dimension and μ is the ( p + q dimensional mean vector. Let be divided into two subsets = (, L, p and = ( p +, L, p + q, the mean vector and the covariance matrix can thus be respectively expressed as and 4 μ = μ μ ( = ( where μ and μ are respectively the mean vectors of and, and ij is the covariance matrix of i and j ( i, j = or. Suppose that values of are known, i.e. w = ( w p +, L, w p + q, the conditional multivariate density of given = w can then be expressed by (Morrison, 990 f ( w w = e p/ * / ( π * μ = μ * = ( * * * ( w μ ( w μ (4 w = μ + μ = ( w (5 w (6

Equation (4 lays the foundation for stochastic simulation of a Gaussian random field... Covariance matrices conversion In the previous section we have implicitly assumed the covariance function C is given or known. This unfortunately raises a question of how can we be sure that our stochastic simulation process using the assumed C will eventually yield realizations of Z(x which are associated with the desired covariance function C Z. Apparently, the covariance function C cannot be arbitrarily chosen and a conversion between C and C Z (or between Z and is necessitated. Let X be a gamma random variable, i,e, X~ G (, λ, with the following density f λ Γ( λx X ( x = x e,, λ > 0 and 0 x < +. (7 e proved that the covariance of two gamma random variables X and X can be related to covariance of two corresponding standard normal random variables and, i.e. ρ, by the following equation: COV ( X, X ( ( A + Bρ ρ ρ ( + C + D λ λ λ λ (8 where ξ = ξ = 9 9,, A = ( ξ ( ξ + ( ξ ξ ( ξ B = 9( ξ.5.5 ξ 0.5 ξ C = 8( ξ ξ ( ξ ξ ( ξ ξ 0.5 + 9ξ.5 + ( ξ ( ξ ξ + 9( ξ ξ ( ξ ξ ( ξ ξ 0.5 + 9( ξ 0.5.5 ξ ξ + 9ξ.5.5 ξ D = 6ξ Approximation by Equation (8 works well for, 0. 5, or equivalently, coefficients of skewness of X and X being less than.0. Equation (8 can be used to convert entry values in Z to their corresponding values in. It should be emphasized that the covariance matrices conversion is unique since the conversional relationship in Equation (8 is also a single-value function... Transforming Gaussian realizations to gamma realizations It can be shown that if X is a gamma random variable with density function of Eq.(7, then a new random variable Y = g( X = λx is chi-square distributed with degree of freedom k =. An approximation of the chi-squared distribution by the standard normal distribution, known as the ilson-hilferty approximation, is given as follows (Patel and Read, 996 y + w (9 9 9 where w represents the standard normal deviate and y is the corresponding chi-squared variate. Thus, the transformation of the standard normal deviate w to gamma variate x can be derived as y x = + w λ λ 9 9 (0 e end this section with the following summary of the simulation procedures: Generate a standard Gaussian random number at the initial node, Determine neighboring nodes to be involved in the subsequent simulation by considering range of the random field Z(x, and use the covariance function C Z to establish the covariance matrix Z, Transform Z to using Equation (8, Generate a standard Gaussian number at the target node using the conditional Gaussian density of Equation (4, Repeat the above procedures until a realization of the standard Gaussian random field is established, 4

Perform point-to-point Gaussian-to-gamma transformation using Equation (0, and it yields a realization of the gamma random field with desired properties. 4. Simulation and verification In order to demonstrate the implementation and verification of the proposed gamma random field simulation approach, several simulation scenarios (see Table using the spherical semi-variogram model with range a and sill ω were adopted for generation of realizations. Table. Parameters of the gamma density and spherical semi-variogram model designated for random field stochastic simulation. Gamma density parameters λ Variogram parameters ω = σ a Size of simulation 4,,, 6 80 80 Size of simulation represents the spatial domain of the random field Z(x. Table. Sample mean of the parameter estimators of the density function and the semi-variogram model.[size of simulation 80 80, = 4, λ =, ω = ] ParameterEs timator a (range of the semi-variogram 6 One hundred simulation runs were conducted for a specific simulation scenario, and density and variogram parameters were estimated from each of the 00 realizations. Parameters (sill ω and range a of the spherical semi-variogram model were estimated by the ordinary least squares fitting method. The method of ordinary least squares assumes that different data pairs involved in semi-variogram fitting are uncorrelated. Except for realizations with very short range as compared to the size of simulation, such assumption is a clear violation of the simulated realizations which are associated with certain spatial covariance matrix. Thus, it inevitably introduces higher degree of uncertainty in the process of parameter estimation. Other semivariogram fitting methods such as the weighted least squares (Cressie, 985; Gotway, 99; Pardo-Iguzqúiza, 999 and the generalized least squares (Pardo-Iguzqúiza and Dowd, 00 have also been proposed, and the uncertainty of semi-variogram parameter estimation using these methods has also been addressed (Pardo- Iguzqúiza and Dowd, 00. These estimates vary among realizations. Therefore, the sample mean of these realization-specific parameter estimates were calculated and tabulated in Table. Generally speaking, the estimated values are in very good agreement with the true parameter values. It is worthy to note that since a random field with onepixel range is technically pure random, no attempt was made to fit the spherical semi-variogram model to the corresponding experimental semi-variograms. Finally, images of several simulated realizations are shown in Figure. As can be expected, when the range a increases, higher degree of spatial correlation can be clearly observed. 5. Conclusions ˆ.9698.870.8765 4.065 λˆ.986.947.99.990 ωˆ 0.9976.004.0098.07 â NA.05.06 6.075 In this study we present a technique for gamma random field simulation. The proposed gamma random field simulation technique is composed of three sequential components: ( covariance function conversion between a gamma random field and a corresponding Gaussian random field, ( generating realizations of a Gaussian random field with standard normal density and the desired covariance function, and ( transforming Gaussian realizations to corresponding gamma realizations. Through a set of devised 44

simulation scenarios, the proposed technique is shown to be capable of generating realizations of given gamma random fields. The proposed gamma random field simulation technique may be very useful for risk assessment and spatial modeling of non-negative and asymmetric environmental variables. a = a = a = a = 6 Fig. : Images of simulated realizations of a gamma random field ( = 4, λ =, ω =, size of simulation 80 80. Grey levels represent simulated values of the random field. 6. Acknowledgements This research was originally initiated from a project funded by the Council of Agriculture, Taiwan, R.O.C. e also thank the National Science Council for subsequent funding support. 7. References [] K.S. Cheng, J.C. Hou, and J.J. Liou, Stochastic simulation of bivariate gamma distribution a frequency-factor based approach, submitted to environmetrics, 008, in review. [] N. Cressie, Fitting variogram models by weighted least squares, Mathematical Geology, 985, 7: 56-586. [] C.A., Gotway, Fitting semi-variogram models by weighted least squares, Computers and Geosciences, 99, 7: 7-7. [4] D.F. Morrison, Multivariate Statistical Methods, McGraw-Hill, 990. [5] E. Pardo-Iguzqúiza, VARFIT: a Fortran-77 program for fitting variogram models by weighted least squares, Computers and Geosciences, 999, 5: 5-6. [6] E. Pardo-Iguzqúiza, and P.A. Dowd, VARIOGD: a computer program for estimating the semi-variogram and its uncertainty, Computers and Geosciences, 00, 7: 549-56. [7] J.K. Patel and C.B. Read, Handbook of the Normal Distribution. Marcel Dekker, 996. 45