Thesis

Irreversible multi-scale diffusions: time scales and model reduction

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Abstract

In this work, we consider non-reversible multi-scale stochastic processes, described by stochastic differential equations, for which we review theory on the convergence behaviour to equilibrium and mean first exit times. Relations between these time scales for non-reversible processes are established, and, by resorting to a control theoretic formulation of the large deviations action functional, even the consideration of hypo-elliptic processes is permitted. The convergence behaviour of the processes is studied in a lot of detail, in particular with respect to initial conditions and temperature. Moreover, the behaviour of the conditional and marginal distributions during the relaxation phase is monitored and discussed as we encounter unexpected behaviour. In the end, this results in the proposal of a data-based partitioning into slow and fast degrees of freedom. In addition, recently proposed techniques promising accelerated convergence to equilibrium are examined and a connection to appropriate model reduction approaches is made. For specific examples this leads to either an interesting alternative formulation of the acceleration procedure or structural insight into the acceleration mechanism. For the model order reduction technique of effective dynamics, which uses conditional expectations, error bounds for non-reversible slow-fast stochastic processes are obtained. A comparison with the reduction method of averaging is undertaken, which, for non-reversible processes, possibly yields different reduced equations. For Ornstein-Uhlenbeck processes sufficient conditions are derived for the two methods (effective dynamics and averaging) to agree in the infinite time scale separation regime. Additionally, we provide oblique projections which allow for the sampling of conditional distributions of non-reversible Ornstein-Uhlenbeck processes.

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A method is presented for computing the average solution of problems which are too complicated for adequate resolution, but where information about the statistics of the solution is available. The method involves computing average derivatives by interpolation based on linear regression, and an updating of a measure constrained by the available crude information. Examples are given. 1 Outline of goal and method There are many problems in science whose solution is described by a set of differential equations, but where the solution of these equations is so complicated that it cannot be found in practice, even numerically, because it cannot be properly resolved. An accurate numerical solution requires that the problem be well-resolved, i.e, that enough variables ("degrees of freedom") be retained in the calculation to represent all relevant features of the solution. Well-known examples where good resolution cannot be achieved in practice include turbulence and various problems in st...
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Let π(x)\pi(x) be a given probability density proportional to exp(U(x))\exp(-U(x)) in a high-dimensional Euclidean space Rm\mathbb{R}^m. The diffusion dX(t)=U(X(t))dt+2dW(t)dX(t) = -\nabla U(X(t))dt + \sqrt 2 dW(t) is often used to sample from π\pi. Instead of U(x)-\nabla U(x), we consider diffusions with smooth drift b(x) and having equilibrium π(x)\pi(x). First we study some general properties and then concentrate on the Gaussian case, namely, U(x)=Dx-\nabla U(x) = Dx with a strictly negative-definite real matrix D and b(x)=Bxb(x) = Bx with a stability matrix B; that is, the real parts of the eigenvalues of B are strictly negative. Using the rate of convergence of the covariance of X(t) [or together with EX(t)] as the criterion, we prove that, among all such b(x), the drift Dx is the worst choice and that improvement can be made if and only if the eigenvalues of D are not identical. In fact, the convergence rate of the covariance is exp(2λM(B)t)\exp(2\lambda_M(B)t), where λM(B)\lambda_M(B) is the maximum of the real parts of the eigenvalues of B and the infimum of λM(B)\lambda_M(B) over all such B is 1/mtrD1/m \operatorname{tr} D. If, for example, a "circulant" drift (UxmUx2,Ux1Ux3,,Uxm1Ux1)\bigg(\frac{\partial U}{\partial x_m} - \frac{\partial U}{\partial x_2},\frac{\partial U}{\partial x_1} - \frac{\partial U}{\partial x_3}, \cdots, \frac{\partial U}{\partial x_{m-1}} - \frac{\partial U}{\partial x_1}\bigg) is added to Dx, then for essentially all D, the diffusion with this modified drift has a better convergence rate.
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Three different results are established which turn out to be closely connected so that the first one implies the second one which in turn implies the third one. The first one states the smoothness of an invariant diffusion density with respect to a parameter. The second establishes a similar smoothness of the solution of the Poisson equation in R-d. The third one states a diffusion approximation result, or in other words an averaging of singularly perturbed diffusion for "fully coupled SDE systems" or "SDE systems with complete dependence.".