HR: 10:25h
AN: NG22A-01 INVITED [Abstracts]
TI: Nonlinear Dynamics, Poor Data, and What to Make of Them?
AU: * Ghil, M
EM: ghil@atmos.ucla.edu
AF: AOS Dept. and IGPP, UCLA, 405 Hilgard Ave., Los Angeles, CA 90095-1565
United States
AU: Zaliapin, I V
EM: zal@ess.ucla.edu
AF: ESS Dept. and IGPP, UCLA, 405 Hilgard Ave., Los Angeles, CA 90095-1567
United States
AB:
The analysis of univariate or multivariate time series provides crucial information to describe, understand, and predict
variability in the geosciences. The discovery and implementation of a number of novel methods for extracting useful
information from time series has recently revitalized this classical field of study. Considerable progress has also been made
in interpreting the information so obtained in terms of dynamical systems theory.
In this talk we will describe the connections between time series analysis and nonlinear dynamics, discuss signal-to-noise
enhancement, and present some of the novel methods for spectral analysis. These fall into two broad categories: (i) methods
that try to ferret out regularities of the time series; and (ii) methods aimed at describing the characteristics of irregular
processes. The former include singular-spectrum analysis (SSA), the multi-taper method (MTM), and the maximum-entropy method
(MEM). The various steps, as well as the advantages and disadvantages of these methods, will be illustrated by their
application to several important climatic time series, such as the Southern Oscillation Index (SOI), paleoclimatic time
series, and instrumental temperature time series. The SOI index captures major features of interannual climate variability
and is used extensively in its prediction. The other time series cover interdecadal and millennial time scales.
The second category includes the calculation of fractional dimension, leading Lyapunov exponents, and Hurst exponents. More
recently, multi-trend analysis (MTA), binary-decomposition analysis (BDA), and related methods have attempted to describe the
structure of time series that include both regular and irregular components. Within the time available, I will try to give a
feeling for how these methods work, and how well.
UR: http://www.atmos.ucla.edu/tcd/ssa/
DE: 9820 Techniques applicable in three or more fields
SC: Nonlinear Geophysics [NG]
MN: Fall Meeting 2005