What s for today. Introduction to Space-time models. c Mikyoung Jun (Texas A&M) Stat647 Lecture 14 October 16, / 19

Similar documents
What s for today. Random Fields Autocovariance Stationarity, Isotropy. c Mikyoung Jun (Texas A&M) stat647 Lecture 2 August 30, / 13

Simple example of analysis on spatial-temporal data set

Asymptotic standard errors of MLE

What s for today. Continue to discuss about nonstationary models Moving windows Convolution model Weighted stationary model

What s for today. All about Variogram Nugget effect. Mikyoung Jun (Texas A&M) stat647 lecture 4 September 6, / 17

Non-gaussian spatiotemporal modeling

Mean square continuity

Non-stationary Cross-Covariance Models for Multivariate Processes on a Globe

Half-Spectral Space-Time Covariance Models

Introduction to Geostatistics

Introduction to Spatial Data and Models

Statistícal Methods for Spatial Data Analysis

Introduction to Spatial Data and Models

A TEST FOR STATIONARITY OF SPATIO-TEMPORAL RANDOM FIELDS ON PLANAR AND SPHERICAL DOMAINS

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

A test for stationarity of spatio-temporal random fields on planar and spherical domains

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

Paper Review: NONSTATIONARY COVARIANCE MODELS FOR GLOBAL DATA

A General Class of Nonseparable Space-time Covariance

Chapter 4 - Fundamentals of spatial processes Lecture notes

New Classes of Asymmetric Spatial-Temporal Covariance Models. Man Sik Park and Montserrat Fuentes 1

Cross-covariance Functions for Tangent Vector Fields on the Sphere

Nonstationary cross-covariance models for multivariate processes on a globe

An Introduction to Spatial Statistics. Chunfeng Huang Department of Statistics, Indiana University

Spatio-Temporal Geostatistical Models, with an Application in Fish Stock

Bo Li. National Center for Atmospheric Research. Based on joint work with:

A new covariance function for spatio-temporal data analysis with application to atmospheric pollution and sensor networking

Symmetry and Separability In Spatial-Temporal Processes

Point-Referenced Data Models

Space-time analysis using a general product-sum model

Geostatistical Space-Time Models, Stationarity, Separability and Full Symmetry. Technical Report no. 475

Geostatistical Space-Time Models, Stationarity, Separability, and Full Symmetry

Spatial-Temporal Modeling of Active Layer Thickness

The ProbForecastGOP Package

Adaptive Sampling of Clouds with a Fleet of UAVs: Improving Gaussian Process Regression by Including Prior Knowledge

Fluvial Variography: Characterizing Spatial Dependence on Stream Networks. Dale Zimmerman University of Iowa (joint work with Jay Ver Hoef, NOAA)

Predictive spatio-temporal models for spatially sparse environmental data. Umeå University

Spatial analysis is the quantitative study of phenomena that are located in space.

Chapter 4 - Fundamentals of spatial processes Lecture notes

Basics of Point-Referenced Data Models

A Framework for Daily Spatio-Temporal Stochastic Weather Simulation

Nonstationary spatial process modeling Part II Paul D. Sampson --- Catherine Calder Univ of Washington --- Ohio State University

Chapter 1. Summer School GEOSTAT 2014, Spatio-Temporal Geostatistics,

Part 5: Spatial-Temporal Modeling

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

BAYESIAN KRIGING AND BAYESIAN NETWORK DESIGN

Space-time data. Simple space-time analyses. PM10 in space. PM10 in time

Package ProbForecastGOP

CBMS Lecture 1. Alan E. Gelfand Duke University

A kernel indicator variogram and its application to groundwater pollution

Non-Fully Symmetric Space-Time Matérn Covariance Functions

Wrapped Gaussian processes: a short review and some new results

Introduction. Semivariogram Cloud

Positive Definite Functions on Spheres

STATISTICAL INTERPOLATION METHODS RICHARD SMITH AND NOEL CRESSIE Statistical methods of interpolation are all based on assuming that the process

STATISTICAL ESTIMATION OF VARIOGRAM AND COVARIANCE PARAMETERS OF SPATIAL AND SPATIO-TEMPORAL RANDOM PROCESES

Spatial Statistics with Image Analysis. Lecture L02. Computer exercise 0 Daily Temperature. Lecture 2. Johan Lindström.

Spatial Statistics for Energy Challenges

Testing Lack of Symmetry in Spatial-Temporal Processes. Man Sik Park and Montserrat Fuentes 1

A Geostatistical Approach to Predict the Average Annual Rainfall of Bangladesh

Gaussian processes for spatial modelling in environmental health: parameterizing for flexibility vs. computational efficiency

A Frequency Domain Approach for the Estimation of Parameters of Spatio-Temporal Stationary Random Processes

Asymptotic Multivariate Kriging Using Estimated Parameters with Bayesian Prediction Methods for Non-linear Predictands

Multilevel Models in Matrix Form. Lecture 7 July 27, 2011 Advanced Multivariate Statistical Methods ICPSR Summer Session #2

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

Theory and Computation for Gaussian Processes

ON THE USE OF NON-EUCLIDEAN ISOTROPY IN GEOSTATISTICS

Midterm 1 and 2 results

REML Estimation and Linear Mixed Models 4. Geostatistics and linear mixed models for spatial data

PARAMETER ESTIMATION FOR FRACTIONAL BROWNIAN SURFACES

of the 7 stations. In case the number of daily ozone maxima in a month is less than 15, the corresponding monthly mean was not computed, being treated

Statistical Inference and Visualization in Scale-Space for Spatially Dependent Images

Separable approximations of space-time covariance matrices

Groundwater permeability

The Matrix Reloaded: Computations for large spatial data sets

Spatio-temporal analysis and interpolation of PM10 measurements in Europe for 2009

Statistics 203: Introduction to Regression and Analysis of Variance Course review

Practicum : Spatial Regression

Overview of Spatial Statistics with Applications to fmri

Statistical Models for Monitoring and Regulating Ground-level Ozone. Abstract

Assessing the covariance function in geostatistics

Spatial Statistics with Image Analysis. Outline. A Statistical Approach. Johan Lindström 1. Lund October 6, 2016

Lecture 3 Stationary Processes and the Ergodic LLN (Reference Section 2.2, Hayashi)

The Matrix Reloaded: Computations for large spatial data sets

Spatial bias modeling with application to assessing remotely-sensed aerosol as a proxy for particulate matter

Interpolation and 3D Visualization of Geodata

Variance stabilization and simple GARCH models. Erik Lindström

Highly Robust Variogram Estimation 1. Marc G. Genton 2

Spatial Interpolation & Geostatistics

7 Geostatistics. Figure 7.1 Focus of geostatistics

Estimation of non-stationary spatial covariance structure

Interpolation of Spatial Data

Vine Copulas. Spatial Copula Workshop 2014 September 22, Institute for Geoinformatics University of Münster.

Bayesian Transformed Gaussian Random Field: A Review

Data Break 8: Kriging the Meuse RiverBIOS 737 Spring 2004 p.1/27

On building valid space-time covariance models

Comparing Accuracy of Spatial Forecasts

1 Introduction to Generalized Least Squares

Umeå University Sara Sjöstedt-de Luna Time series analysis and spatial statistics

Covariance models on the surface of a sphere: when does it matter?

Transcription:

What s for today Introduction to Space-time models c Mikyoung Jun (Texas A&M) Stat647 Lecture 14 October 16, 2012 1 / 19

Space-time Data So far we looked at the data that vary over space Now we add another dimension: time There are numerous examples and applications for space-time process since things usually change over the space and time at the same time What we did so far is to fix a time point and analyze the spatial component of the data c Mikyoung Jun (Texas A&M) Stat647 Lecture 14 October 16, 2012 2 / 19

Space-time Data When you have space-time data, you can do one of the following things: 1 Separate spatial analyses for each time point 2 Separate temporal analyses for each spatial location 3 Spatio-temporal analysis with methods for random fields in R d R In this class, we mainly take the third approach c Mikyoung Jun (Texas A&M) Stat647 Lecture 14 October 16, 2012 3 / 19

Space-time process Consider a stochastic process in the following way: {Z(s,t) : s D(t) R 2,t T R} Usually T is a space with integers and regularly spaced while D(t) can be either regularly or irregularly spaced In many cases D(t) D Now we may consider Cov{Z(s 1,t 1 ),Z(s 2,t 2 )} c Mikyoung Jun (Texas A&M) Stat647 Lecture 14 October 16, 2012 4 / 19

Isotropy, stationarity... Suppose the mean of Z is constant over space and time Then Z is stationary in time if Cov{Z(s 1,t 1 ),Z(s 2,t 2 )} = K 1 (s 1,s 2,t 1 t 2 ) for all t 1 and t 2 and some valid K 1 We say Z is isotropic in time if Cov{Z(s 1,t 1 ),Z(s 2,t 2 )} = K 2 (s 1,s 2, t 1 t 2 ) for all t 1 and t 2 and some valid K 2 If Z is stationary in both space and time, we have Cov{Z(s 1,t 1 ),Z(s 2,t 2 )} = K 3 (s 1 s 2,t 1 t 2 ) for all s i, t i and for a valid K 3 Isotropy in both space and time is defined in the same way c Mikyoung Jun (Texas A&M) Stat647 Lecture 14 October 16, 2012 5 / 19

Space-time variogram Suppose we assume the process is stationary in space and time and the mean is zero Now we consider γ(h,k) = 1 2Var[Z(s,t) Z(s + h,t + k)] The empirical spatio-temporal semivariogram estimator is given by ˆγ(h,k) = 1 2 N(h, k) N(h,k) {Z(s i,t i ) Z(s j,t j )} 2 Here N(h,k) consists of the points that are about spatial distance h and time lag k Even if we assume spatial isotropy, now the picture of empirical variogram is in 3-dimension or higher dimension c Mikyoung Jun (Texas A&M) Stat647 Lecture 14 October 16, 2012 6 / 19

Space-time variogram Now we can thing of three different kinds of nugget 1 One with respect to space: 1 (h=0) 2 One with respect to time: 1 (k=0) 3 One with respect to space and time: 1 (h=0,k=0) Sometimes having all the three nugget effects improve the model fit substantially, although 1 and 3 may matter more c Mikyoung Jun (Texas A&M) Stat647 Lecture 14 October 16, 2012 7 / 19

Example of space-time variogram c Mikyoung Jun (Texas A&M) Stat647 Lecture 14 October 16, 2012 8 / 19

How to develop space-time variogram (or covariance) model? You may treat you have R d+1 dimension and apply similar ideas as you did for spatial process case But the distance in space and distance in time are different A simple thing to do is to consider a distance in R d+1 such that d((s 1,t 1 ),(s 2,t 2 )) = [d(s 1,s 2 )/β 1 ] 2 + [ t 1 t 2 /β 2 ] 2 Using the above distance, you can use any isotropic model valid for R d+1, for example, a Matérn model Note that you an only have a model isotropic in both space and time in this way c Mikyoung Jun (Texas A&M) Stat647 Lecture 14 October 16, 2012 9 / 19

Separable model Another way you can do is to consider a separable model We say a space-time covariance function is separable if it factors into purely spatial and purely temporal covariance models That is, Cov[Z(s 1,t 1 ),Z(s 2,t 2 )] = K s (s 1,s 2 ) K t (t 1,t 2 ) Here, K s and K t are valid covariance models for space and time, respectively Why is this method creating a valid space-time covariance model? In other words, if we simply multiply a spatial covariance function to a temporal covariance function, do we get a valid space-time covariance function? c Mikyoung Jun (Texas A&M) Stat647 Lecture 14 October 16, 2012 10 / 19

Separable model Simple example for isotropic space-time covariance model that is separable is: Cov[Z(s 1,t 1 ),Z(s 2,t 2 )] = exp ( s 1 s 2 /β 1 ) exp ( t 1 t 2 /β 2 ) In this case, we may call β 1 a spatial range and β 2 a temporal range parameter Note that the process Z has same amount of smoothness both in space and time We may use Matérn model with different smoothness parameters for space and time to overcome this problem c Mikyoung Jun (Texas A&M) Stat647 Lecture 14 October 16, 2012 11 / 19

Separable model Separable models have many nice features One is computational advantage Another is convenient interpretation Another is that enables us to develop space-time covariance models easily However, do you see any problem with separable covariance models? c Mikyoung Jun (Texas A&M) Stat647 Lecture 14 October 16, 2012 12 / 19

Limitation of separable model One of the biggest limitation of separable model is that there is no space-time interaction This is related to what we call space-time asymmetry Suppose you have a wind blowing from one location to the other over time In particular, suppose you have a westerly wind blowing from location A to B (B is east of A) Then, if we think of an air pollutant concentration process (with relatively long life time) Z, and consider two correlations Cor[Z(A, t), Z(B, t + s)] and Cor[Z(B, t), Z(A, t + s)] for s > 0, are they equal or one should be bigger than the other? Can separable covariance models create space-time asymmetry? c Mikyoung Jun (Texas A&M) Stat647 Lecture 14 October 16, 2012 13 / 19

Space-time asymmetry Space-time asymmetry is a very common characteristic of space-time data in geophysical and environmental problems Many people find space-time asymmetry in many real data sets. For example, in Irish wind data including Gneiting (2002), JASA and Stein (2005), JASA Separable model is definitely too limited to model such data sets c Mikyoung Jun (Texas A&M) Stat647 Lecture 14 October 16, 2012 14 / 19

Irish wind data (source: Haslett and Raftery (1989), Applied Statistics) c Mikyoung Jun (Texas A&M) Stat647 Lecture 14 October 16, 2012 15 / 19

Space-time asymmetry (source: Stein (2005), JASA) c Mikyoung Jun (Texas A&M) Stat647 Lecture 14 October 16, 2012 16 / 19

In next class... We will see hypothesis tests on separability and examples of nonseparable space-time covariance models c Mikyoung Jun (Texas A&M) Stat647 Lecture 14 October 16, 2012 17 / 19

Team report 2 (due October 25 12:45 PM) Second team report is on spatial regression modeling with isotropic covariance structure. That is, write your data as Z(s) = m(s)β + e(s), with m term consists of available covariates (you can at least include your x coordinate and y coordinates, and you can add other covariates available) and model e term as a mean zero Gaussian random field with isotropic covariance structure. (continue to next page) c Mikyoung Jun (Texas A&M) Stat647 Lecture 14 October 16, 2012 18 / 19

Team report 2 (due October 25 12:45 PM) I expect to see at least the following (required minimum): Assume Matérn covariance structure and estimate the smoothness parameter ν along with other covariance parameters OLS (or WLS, or both), MLE (or REML, or both) fits of mean and covariance parmameters, with corresponding asymptotic SEs (for MLE) Leave out a few spatial locations (at least one or two) for valiation of your model. That is, perform kriging over the left-out-sites and assess your prediction results Limit 10 pages (with figures and tables). Please do not include large figures (reduce figure file size). c Mikyoung Jun (Texas A&M) Stat647 Lecture 14 October 16, 2012 19 / 19