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contributor authorFraedrich, Klaus
date accessioned2017-06-09T14:26:16Z
date available2017-06-09T14:26:16Z
date copyright1986/03/01
date issued1986
identifier issn0022-4928
identifier otherams-19241.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4155336
description abstractThe dimensions of attractors are estimated from phase space trajectories of observed weather and climate variables (local surface pressure and relative sunshine duration, zonal wave amplitude; a δ18O-record). They provide primary information for descriptions of properties of the attractors of dynamical systems and give a lower limit to the number of the essential variables necessary to model the dynamics. These estimates are based on distance distributions of pairs of points on the single variable trajectory evolving in phase spaces which embed the attractor. One observes a low fractal dimensionality between three and four for the weather attractor, if interannual variability and seasonal changes are eliminated. The physical interpretation is based on the three dominating scales of cyclones, cyclone families and index-cycle; the irregularity of the flow and strong dependence on initial conditions amount for the fractal value. The climate variable also reveals a low dimensionality (between four and five) of the climate attractor. This is supported by an independent estimate based on eigenfunction expansion of the embedded phase space trajectory. These types of analyses suggest how to extend the standard data evaluation and model verification techniques to an analysis of the phase space behavior of observed and simulated dynamical systems.
publisherAmerican Meteorological Society
titleEstimating the Dimensions of Weather and Climate Attractors
typeJournal Paper
journal volume43
journal issue5
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1986)043<0419:ETDOWA>2.0.CO;2
journal fristpage419
journal lastpage432
treeJournal of the Atmospheric Sciences:;1986:;Volume( 043 ):;issue: 005
contenttypeFulltext


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