Articles | Volume 25, issue 1
https://doi.org/10.5194/npg-25-207-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/npg-25-207-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Evolution of fractality in space plasmas of interest to geomagnetic activity
Víctor Muñoz
CORRESPONDING AUTHOR
Departamento de Física, Facultad de Ciencias, Universidad de Chile, Santiago, Chile
Macarena Domínguez
Departamento de Física, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile, Santiago, Chile
Juan Alejandro Valdivia
Departamento de Física, Facultad de Ciencias, Universidad de Chile, Santiago, Chile
Centro para la Nanociencia y la Nanotecnología, CEDENNA, Santiago, Chile
Simon Good
Department of Physics, University of Helsinki, Helsinki, Finland
The Blackett Laboratory, Imperial College London, London, UK
Giuseppina Nigro
Dipartimento di Fisica, Università della Calabria, Rende, Italy
Vincenzo Carbone
Dipartimento di Fisica, Università della Calabria, Rende, Italy
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Subject: Time series, machine learning, networks, stochastic processes, extreme events | Topic: Ionosphere, magnetosphere, planetary science, solar science
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Miroslava Vukcevic and Luka Č. Popović
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Gurbax S. Lakhina and Bruce T. Tsurutani
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Odim Mendes, Margarete Oliveira Domingues, Ezequiel Echer, Rajkumar Hajra, and Varlei Everton Menconi
Nonlin. Processes Geophys., 24, 407–417, https://doi.org/10.5194/npg-24-407-2017, https://doi.org/10.5194/npg-24-407-2017, 2017
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The effects of the Sun upon the Earth's atmosphere occur in several ways. Significant electrodynamic coupling processes transfer particles and energy from the solar wind into the Earth's environment. Applied to the dynamical characteristics of high-intensity, long-duration, continuous auroral activity (HILDCAA) and non-HILDCAA events, nonlinear analysis tools like RQA aid to unravel peculiarities related to two concurrent space mechanisms known as magnetic reconnection and viscous interaction.
Chris M. Hall
Nonlin. Processes Geophys., 23, 215–222, https://doi.org/10.5194/npg-23-215-2016, https://doi.org/10.5194/npg-23-215-2016, 2016
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The relative ionospheric opacity meter ("riometer") is a traditional instrument for measuring the degree to which cosmic noise is absorbed by the ionosphere and therefore how energetic the particles – electrons, protons etc. – are that cause the ionisation. We identify the same signatures in the "hour-to-days" timescale variability as reported in solar and geomagnetic disturbances. The result demonstrates the relationship between riometer data and the underlying physics for different timescales.
Y. Zou, R. V. Donner, N. Marwan, M. Small, and J. Kurths
Nonlin. Processes Geophys., 21, 1113–1126, https://doi.org/10.5194/npg-21-1113-2014, https://doi.org/10.5194/npg-21-1113-2014, 2014
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We use visibility graphs to characterize asymmetries in the dynamics of sunspot areas in both solar hemispheres. Our analysis provides deep insights into the potential and limitations of this method, revealing a complex interplay between effects due to statistical versus dynamical properties of the observed data. Temporal changes in the hemispheric predominance of the graph connectivity are found to lag those directly associated with the total hemispheric sunspot areas themselves.
A. Ojeda González, W. D. Gonzalez, O. Mendes, M. O. Domingues, and R. R. Rosa
Nonlin. Processes Geophys., 21, 1059–1073, https://doi.org/10.5194/npg-21-1059-2014, https://doi.org/10.5194/npg-21-1059-2014, 2014
C. M. Hall
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A. Shapoval, J. L. Le Mouël, M. Shnirman, and V. Courtillot
Nonlin. Processes Geophys., 21, 797–813, https://doi.org/10.5194/npg-21-797-2014, https://doi.org/10.5194/npg-21-797-2014, 2014
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Short summary
Fractals are self-similar objects (which look the same at all scales), whose dimensions can be noninteger. They are mathematical concepts, useful to describe various physical systems, as the fractal dimension is a measure of their complexity. In this paper we study how these concepts can be applied to some problems in space plasmas, such as the activity of the Earth's magnetosphere, simulations of plasma turbulence, or identification of magnetic structures ejected from the Sun.
Fractals are self-similar objects (which look the same at all scales), whose dimensions can be...
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