Causality and Information Transfer Between the Solar Wind and the Magnetosphere–Ionosphere System
An information-theoretic approach for detecting causality and information transfer is used to identify interactions of solar activity and interplanetary medium conditions with the Earth’s magnetosphere–ionosphere systems. A causal information transfer from the solar wind parameters to geomagnetic in...
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doaj-0d0a333b18134189ae18a79ca81721ca2021-03-26T00:03:50ZengMDPI AGEntropy1099-43002021-03-012339039010.3390/e23040390Causality and Information Transfer Between the Solar Wind and the Magnetosphere–Ionosphere SystemPouya Manshour0Georgios Balasis1Giuseppe Consolini2Constantinos Papadimitriou3Milan Paluš4Department of Complex Systems, Institute of Computer Science of the Czech Academy of Sciences, Pod Vodárenskou věží 2, 182 07 Prague 8, Czech RepublicInstitute for Astronomy, Astrophysics, Space Applications and Remote Sensing, National Observatory of Athens, I. Metaxa & Vas. Pavlou Street, 15236 Penteli, GreeceINAF-Istituto di Astrofisica e Planetologia Spaziali, 00133 Rome, ItalyInstitute for Astronomy, Astrophysics, Space Applications and Remote Sensing, National Observatory of Athens, I. Metaxa & Vas. Pavlou Street, 15236 Penteli, GreeceDepartment of Complex Systems, Institute of Computer Science of the Czech Academy of Sciences, Pod Vodárenskou věží 2, 182 07 Prague 8, Czech RepublicAn information-theoretic approach for detecting causality and information transfer is used to identify interactions of solar activity and interplanetary medium conditions with the Earth’s magnetosphere–ionosphere systems. A causal information transfer from the solar wind parameters to geomagnetic indices is detected. The vertical component of the interplanetary magnetic field (<inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><mrow><mi>B</mi><mi>z</mi></mrow></semantics></math></inline-formula>) influences the auroral electrojet (AE) index with an information transfer delay of 10 min and the geomagnetic disturbances at mid-latitudes measured by the symmetric field in the H component (SYM-H) index with a delay of about 30 min. Using a properly conditioned causality measure, no causal link between AE and SYM-H, or between magnetospheric substorms and magnetic storms can be detected. The observed causal relations can be described as linear time-delayed information transfer.https://www.mdpi.com/1099-4300/23/4/390time seriescausalityinformation transfertime reversalsolar wind-magnetosphere–ionosphere systemspace weather |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Pouya Manshour Georgios Balasis Giuseppe Consolini Constantinos Papadimitriou Milan Paluš |
spellingShingle |
Pouya Manshour Georgios Balasis Giuseppe Consolini Constantinos Papadimitriou Milan Paluš Causality and Information Transfer Between the Solar Wind and the Magnetosphere–Ionosphere System Entropy time series causality information transfer time reversal solar wind-magnetosphere–ionosphere system space weather |
author_facet |
Pouya Manshour Georgios Balasis Giuseppe Consolini Constantinos Papadimitriou Milan Paluš |
author_sort |
Pouya Manshour |
title |
Causality and Information Transfer Between the Solar Wind and the Magnetosphere–Ionosphere System |
title_short |
Causality and Information Transfer Between the Solar Wind and the Magnetosphere–Ionosphere System |
title_full |
Causality and Information Transfer Between the Solar Wind and the Magnetosphere–Ionosphere System |
title_fullStr |
Causality and Information Transfer Between the Solar Wind and the Magnetosphere–Ionosphere System |
title_full_unstemmed |
Causality and Information Transfer Between the Solar Wind and the Magnetosphere–Ionosphere System |
title_sort |
causality and information transfer between the solar wind and the magnetosphere–ionosphere system |
publisher |
MDPI AG |
series |
Entropy |
issn |
1099-4300 |
publishDate |
2021-03-01 |
description |
An information-theoretic approach for detecting causality and information transfer is used to identify interactions of solar activity and interplanetary medium conditions with the Earth’s magnetosphere–ionosphere systems. A causal information transfer from the solar wind parameters to geomagnetic indices is detected. The vertical component of the interplanetary magnetic field (<inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><mrow><mi>B</mi><mi>z</mi></mrow></semantics></math></inline-formula>) influences the auroral electrojet (AE) index with an information transfer delay of 10 min and the geomagnetic disturbances at mid-latitudes measured by the symmetric field in the H component (SYM-H) index with a delay of about 30 min. Using a properly conditioned causality measure, no causal link between AE and SYM-H, or between magnetospheric substorms and magnetic storms can be detected. The observed causal relations can be described as linear time-delayed information transfer. |
topic |
time series causality information transfer time reversal solar wind-magnetosphere–ionosphere system space weather |
url |
https://www.mdpi.com/1099-4300/23/4/390 |
work_keys_str_mv |
AT pouyamanshour causalityandinformationtransferbetweenthesolarwindandthemagnetosphereionospheresystem AT georgiosbalasis causalityandinformationtransferbetweenthesolarwindandthemagnetosphereionospheresystem AT giuseppeconsolini causalityandinformationtransferbetweenthesolarwindandthemagnetosphereionospheresystem AT constantinospapadimitriou causalityandinformationtransferbetweenthesolarwindandthemagnetosphereionospheresystem AT milanpalus causalityandinformationtransferbetweenthesolarwindandthemagnetosphereionospheresystem |
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