Determination of fractal dimensions of solar radio bursts

Citation
A. Veronig et al., Determination of fractal dimensions of solar radio bursts, ASTRON ASTR, 357(1), 2000, pp. 337-350
Citations number
39
Categorie Soggetti
Space Sciences
Journal title
ASTRONOMY AND ASTROPHYSICS
ISSN journal
00046361 → ACNP
Volume
357
Issue
1
Year of publication
2000
Pages
337 - 350
Database
ISI
SICI code
0004-6361(200005)357:1<337:DOFDOS>2.0.ZU;2-W
Abstract
We present a dimension analysis of a set of solar type I storms and type IV events with different kind of fine structures, recorded at the Trieste Ast ronomical Observatory. The signature of such types of solar radio events is highly structured in time. However, periodicities are rather seldom, and l inear mode theory can provide only limited interpretation of the data. Ther efore, we performed an analysis based on methods of the nonlinear dynamics theory. Additionally to the commonly used correlation dimension, we also calculated local pointwise dimensions. This alternative approach is motivated by the fact that astrophysical time series represent real-world systems, which can not be kept in a controlled state and which are highly interconnected with their surroundings. In such systems pure determinism is rather unlikely to be realized, and therefore a characterization by invariants of the dynamics might probably be inadequate. In fact, the outcome of the dimension analysis does not give hints for low- dimensional determinism in the data, but we show that, contrary to the corr elation dimension method, local dimension estimations can give physical ins ight into the events even in cases in which pure determinism cannot be esta blished. In particular, in most of the analyzed radio events nonlinearity i n the data is detected, and the local dimension analysis provides a basis f or a quantitative description of the time series, which can be used to char acterize the complexity of the related physical system in a comparative and non-invariant manner. In this frame, the degree of complexity we inferred for type I storms is on the average lower than that relevant to type IV events. For the type TV ev ents significant differences occur with regard to the various subtypes, whe re pulsations and sudden reductions can be described by distinctly lower va lues than spikes and fast pulsations.