posted on 2012-10-11, 00:00authored byRafail V. Abramov
Many applications of contemporary science involve multiscale dynamics, which are
typically characterized by the time and space scale separation of patterns of motion, with fewer slowly
evolving variables and a much larger set of faster evolving variables. This time-space scale separation
causes direct numerical simulation of the evolution of the dynamics to be computationally expensive
due to both the large number of variables and the necessity to choose a small discretization time
step in order to resolve the fast components of dynamics. In this work we propose a simple method
of determining the closed model for slow variables alone, which requires only a single computation
of appropriate statistics for the fast dynamics with a certain fixed state of the slow variables. The
method is based on the first-order Taylor expansion of the averaged coupling term with respect to
the slow variables, which can be computed using the linear fluctuation-dissipation theorem. We
show that, with simple linear coupling in both slow and fast variables, this method produces quite
comparable statistics to what is exhibited by a complete two-scale model. The main advantage of the
method is that it applies even when the statistics of the full multiscale model cannot be simulated
due to computational complexity, which makes it practical for real-world large scale applications.