Principal components' features of mid-latitude geomagnetic daily variation

The ionospheric and magnetospheric current systems are responsible of the daily magnetic field changes. Recently, the Natural Orthogonal Components (NOC) technique has been applied to model the physical system responsible of the daily variation of the geomagnetic field, efficiently and accurately...

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Main Authors: P. De Michelis, R. Tozzi, G. Consolini
Format: Article
Language:English
Published: Copernicus Publications 2010-12-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/28/2213/2010/angeo-28-2213-2010.pdf
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spelling doaj-88b2fecaed9e44a58253169c202258442020-11-24T20:40:43ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762010-12-01282213222610.5194/angeo-28-2213-2010Principal components' features of mid-latitude geomagnetic daily variationP. De Michelis0P. De Michelis1R. Tozzi2G. Consolini3Istituto Nazionale di Geofisica e Vulcanologia, 00143 Roma, ItalyDip. Scienze della Terra, Università degli Studi di Siena, 53100 Siena, ItalyIstituto Nazionale di Geofisica e Vulcanologia, 00143 Roma, ItalyINAF-Istituto di Fisica dello Spazio Interplanetario, 00133 Roma, ItalyThe ionospheric and magnetospheric current systems are responsible of the daily magnetic field changes. Recently, the Natural Orthogonal Components (NOC) technique has been applied to model the physical system responsible of the daily variation of the geomagnetic field, efficiently and accurately (Xu and Kamide, 2004). Indeed, this approach guarantees that the number of parameters used to represent the physical process is small as much as possible, and consequently process control for such system becomes apparent. <br><br> We focus our present study on the analysis of the hourly means of the magnetic elements H, D and Z recorded at L'Aquila observatory in Italy from 1993 to 2004. We apply to this dataset the NOC technique to reconstruct the 3-dimensional structures of the different ionospheric and magnetospheric current systems which contribute to the geomagnetic daily variations. To support our interpretation in terms of the different ionospheric and magnetospheric current systems, the spectral and statistical features of the time-dependent amplitudes associated to the set of natural orthogonal components are analyzed and compared to those of a set of descriptors of the magnetospheric dynamics and solar wind changes.https://www.ann-geophys.net/28/2213/2010/angeo-28-2213-2010.pdf
collection DOAJ
language English
format Article
sources DOAJ
author P. De Michelis
P. De Michelis
R. Tozzi
G. Consolini
spellingShingle P. De Michelis
P. De Michelis
R. Tozzi
G. Consolini
Principal components' features of mid-latitude geomagnetic daily variation
Annales Geophysicae
author_facet P. De Michelis
P. De Michelis
R. Tozzi
G. Consolini
author_sort P. De Michelis
title Principal components' features of mid-latitude geomagnetic daily variation
title_short Principal components' features of mid-latitude geomagnetic daily variation
title_full Principal components' features of mid-latitude geomagnetic daily variation
title_fullStr Principal components' features of mid-latitude geomagnetic daily variation
title_full_unstemmed Principal components' features of mid-latitude geomagnetic daily variation
title_sort principal components' features of mid-latitude geomagnetic daily variation
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2010-12-01
description The ionospheric and magnetospheric current systems are responsible of the daily magnetic field changes. Recently, the Natural Orthogonal Components (NOC) technique has been applied to model the physical system responsible of the daily variation of the geomagnetic field, efficiently and accurately (Xu and Kamide, 2004). Indeed, this approach guarantees that the number of parameters used to represent the physical process is small as much as possible, and consequently process control for such system becomes apparent. <br><br> We focus our present study on the analysis of the hourly means of the magnetic elements H, D and Z recorded at L'Aquila observatory in Italy from 1993 to 2004. We apply to this dataset the NOC technique to reconstruct the 3-dimensional structures of the different ionospheric and magnetospheric current systems which contribute to the geomagnetic daily variations. To support our interpretation in terms of the different ionospheric and magnetospheric current systems, the spectral and statistical features of the time-dependent amplitudes associated to the set of natural orthogonal components are analyzed and compared to those of a set of descriptors of the magnetospheric dynamics and solar wind changes.
url https://www.ann-geophys.net/28/2213/2010/angeo-28-2213-2010.pdf
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