ANALYSIS OF STEEPENED MAGNETOSONIC WAVES USING WAVELET TRANSFORMS ANDNEURAL NETWORKS

Authors
Citation
P. Muret et N. Omidi, ANALYSIS OF STEEPENED MAGNETOSONIC WAVES USING WAVELET TRANSFORMS ANDNEURAL NETWORKS, J GEO R-S P, 100(A12), 1995, pp. 23465-23479
Citations number
23
Categorie Soggetti
Geosciences, Interdisciplinary","Astronomy & Astrophysics","Metereology & Atmospheric Sciences
Journal title
JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS
ISSN journal
21699380 → ACNP
Volume
100
Issue
A12
Year of publication
1995
Pages
23465 - 23479
Database
ISI
SICI code
2169-9380(1995)100:A12<23465:AOSMWU>2.0.ZU;2-S
Abstract
In this study, wavelet transforms and neural networks are used to anal yze the formation and evolution of steepened magnetosonic waves (shock lets) generated in hybrid (fluid electrons, particle ions) simulations , These waves model the shocklets observed upstream of planetary bow s hocks and at comets, Specifically, the usefulness of wavelet transform s and neural networks for understanding the nature of the steepening p rocess, and the further evolution of shocklets into less coherent stru ctures is investigated, Previous studies had suggested that the nonlin ear steepening process is associated with the excitation of higher fre quency waves within the original wave, This hypothesis, however, could not be directly substantiated using Fourier transforms, In order to c ontinue with the analysis of shocklets, it has become necessary to imp lement new techniques using wavelet transforms and neural networks, Wa velet transforms are tailored to the analysis of localized structures such as shocklets, while neural networks have the ability to model non linear dynamical systems, Application of wavelet transforms has verifi ed the presence of higher frequency waves within the steepening shockl et and has identified them as the forward propagating and the backward propagating magnetosonic waves as well as the backward propagating Al fven ion-cyclotron mode, The wavelet transform has also located the so urce of the whistler wave packet attached to the shocklet to be the re gion of steep magnetic field gradient, In order to understand the furt her evolution of shocklets, neural networks have been applied in the a nalysis, Used in conjunction with a translation invariant transform, n eural networks have been successfully trained to identify shocklets, T his allows for the scanning of large datasets as well as the developme nt of a classification system for shocklets, A multinetwork classifica tion system using various techniques, including wavelet preprocessing, has been developed to analyze the further evolution of shocklets and their components, Identification and classification of neural networks have increased our understanding of shocklet evolution, The technique s involving wavelet transforms and neural networks that have been empl oyed in this study show considerable potential for the study of not on ly shocklets, but also other wave phenomena in space plasmas.