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Empirical Orthogonal Functions: The Medium is the Message

Monahan, A. H., Fyfe, J. C., Ambaum, M. H. P. ORCID:, Stephenson, D. B. and North, G. R. (2009) Empirical Orthogonal Functions: The Medium is the Message. Journal of Climate, 22 (24). pp. 6501-6514. ISSN 1520-0442

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To link to this item DOI: 10.1175/2009jcli3062.1


Empirical orthogonal function (EOF) analysis is a powerful tool for data compression and dimensionality reduction used broadly in meteorology and oceanography. Often in the literature, EOF modes are interpreted individually, independent of other modes. In fact, it can be shown that no such attribution can generally be made. This review demonstrates that in general individual EOF modes (i) will not correspond to individual dynamical modes, (ii) will not correspond to individual kinematic degrees of freedom, (iii) will not be statistically independent of other EOF modes, and (iv) will be strongly influenced by the nonlocal requirement that modes maximize variance over the entire domain. The goal of this review is not to argue against the use of EOF analysis in meteorology and oceanography; rather, it is to demonstrate the care that must be taken in the interpretation of individual modes in order to distinguish the medium from the message.

Item Type:Article
Divisions:Science > School of Mathematical, Physical and Computational Sciences > Department of Meteorology
ID Code:4432
Uncontrolled Keywords:singular-value decomposition; sea-surface temperature; annular modes; southern-hemisphere; arctic oscillation; jet eofs; variability; reduction; patterns; anomalies
Publisher:American Meteorological Society

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