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Sullivan - Introduction to Uncertainty Quantification

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Sullivan Introduction to Uncertainty Quantification
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Springer International Publishing Switzerland 2015
T.J. Sullivan Introduction to Uncertainty Quantification Texts in Applied Mathematics 10.1007/978-3-319-23395-6_1
1. Introduction
T. J. Sullivan 1
(1)
Mathematics Institute, University of Warwick, Coventry, UK
We must think differently about our ideas and how we test them. We must become more comfortable with probability and uncertainty. We must think more carefully about the assumptions and beliefs that we bring to a problem.
The Signal and the Noise: The Art of Science and Prediction
Nate Silver
1.1 What is Uncertainty Quantification?
This book is an introduction to the mathematics of Uncertainty Quantification (UQ), but what is UQ? It is, roughly put, the coming together of probability theory and statistical practice with the real world. These two anecdotes illustrate something of what is meant by this statement:
  • Until the early-to-mid 1990s, risk modelling for catastrophe insurance and re-insurance (i.e. insurance for property owners against risks arising from earthquakes, hurricanes, terrorism, etc., and then insurance for the providers of such insurance) was done on a purely statistical basis. Since that time, catastrophe modellers have tried to incorporate models for the underlying physics or human behaviour, hoping to gain a more accurate predictive understanding of risks by blending the statistics and the physics, e.g. by focussing on what is both statistically and physically reasonable. This approach also allows risk modellers to study interesting hypothetical scenarios in a meaningful way, e.g. using a physics-based model of water drainage to assess potential damage from rainfall 10% in excess of the historical maximum.
  • Over roughly the same period of time, deterministic engineering models of complex physical processes began to incorporate some element of uncertainty to account for lack of knowledge about important physical parameters, random variability in operating circumstances, or outright ignorance about what the form of a correct model would be. Again the aim is to provide more accurate predictions about systems behaviour.
Thus, a typical UQ problem involves one or more mathematical models for a process of interest, subject to some uncertainty about the correct form of, or parameter values for, those models. Often, though not always, these uncertainties are treated probabilistically.
Perhaps as a result of its history, there are many perspectives on what UQ is, including at the extremes assertions like UQ is just a buzzword for statistics or UQ is just error analysis. These points of view are somewhat extremist, but they do contain a kernel of truth: very often, the probabilistic theory underlying UQ methods is actually quite simple, but is obscured by the details of the application. However, the complications that practical applications present are also part of the essence of UQ: it is all very well giving an accurate prediction for some insurance risk in terms of an elementary mathematical object such as an expected value, but how will you actually go about evaluating that expected value when it is an integral over a million-dimensional parameter space? Thus, it is important to appreciate both the underlying mathematics and the practicalities of implementation, and the presentation here leans towards the former while keeping the latter in mind.
Typical UQ problems of interest include certification, prediction, model and software verification and validation, parameter estimation, data assimilation, and inverse problems. At its very broadest,
UQ studies all sources of error and uncertainty, including the following: systematic and stochastic measurement error; ignorance; limitations of theoretical models; limitations of numerical representations of those models; limitations of the accuracy and reliability of computations, approximations, and algorithms; and human error. A more precise definition is UQ is the end-to-end study of the reliability of scientific inferences. (U.S. Department of Energy, , p. 135)
It is especially important to appreciate the end-to-end nature of UQ studies: one is interested in relationships between pieces of information , not the truth of those pieces of information/assumptions, bearing in mind that they are only approximations of reality. There is always going to be a risk of Garbage In, Garbage Out. UQ cannot tell you that your model is right or true, but only that, if you accept the validity of the model (to some quantified degree), then you must logically accept the validity of certain conclusions (to some quantified degree). In the authors view, this is the proper interpretation of philosophically sound but somewhat unhelpful assertions like Verification and validation of numerical models of natural systems is impossible and The primary value of models is heuristic (Oreskes et al., ). UQ can, however, tell you that two or more of your modelling assumptions are mutually contradictory, and hence that your model is wrong, and a complete UQ analysis will include a meta-analysis examining the sensitivity of the original analysis to perturbations of the governing assumptions.
A prototypical, if rather over-used, example for UQ is an elliptic PDE with uncertainty coefficients:
Example 1.1.
Consider the following elliptic boundary value problem on a connected Lipschitz domain typically n 2 or 3 11 Problem is a simple but not overly nave - photo 1 (typically n =2 or 3):
11 Problem is a simple but not overly nave model for the pressure field u - photo 2
(1.1)
Problem () is a simple but not overly nave model for the pressure field u of some fluid occupying a domain Introduction to Uncertainty Quantification - image 3 . The domain Introduction to Uncertainty Quantification - image 4 consists of a material, and the tensor field Introduction to Uncertainty Quantification - image 5 describes the permeability of this material to the fluid. There is a source term Introduction to Uncertainty Quantification - image 6 , and the boundary condition specifies the values Introduction to Uncertainty Quantification - image 7 that the pressure takes on the boundary of Picture 8 . This model is of interest in the earth sciences because Darcys law asserts that the velocity field v of the fluid flow in this medium is related to the gradient of the pressure field by
Picture 9
If the fluid contains some kind of contaminant, then it may be important to understand where fluid following the velocity field v will end up, and when.
In a course on PDE theory, you will learn that, for each given positive-definite and essentially bounded permeability field , problem () has a unique weak solution u in the Sobolev space Picture 10 for each forcing term f in the dual Sobolev space Picture 11
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