Estimation of the local response to a forcing in a high dimensional system using the fluctuation-dissipation theorem

The fluctuation-dissipation theorem (FDT) has been proposed as a method of calculating the response of the earth's atmosphere to a forcing. For this problem the high dimensionality of the relevant data sets makes truncation necessary. Here we propose a method of truncation based upon the assump...

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Bibliographic Details
Main Authors: F. C. Cooper, J. G. Esler, P. H. Haynes
Format: Article
Language:English
Published: Copernicus Publications 2013-04-01
Series:Nonlinear Processes in Geophysics
Online Access:http://www.nonlin-processes-geophys.net/20/239/2013/npg-20-239-2013.pdf