On polar daily geomagnetic variation

<p style="-qt-block-indent: 0; text-indent: 0px; margin: 0px;">The aim of this work is to investigate the nature of the daily magnetic field perturbations produced by ionospheric and magnetospheric currents at high latitudes. We analyse the hourly means of the X and Y geomagnetic fie...

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Main Authors: Paola De Michelis, Giuseppe Consolini
Format: Article
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 2015-11-01
Series:Annals of Geophysics
Subjects:
Online Access:http://www.annalsofgeophysics.eu/index.php/annals/article/view/6801
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spelling doaj-1e17375153ca4190add52632531f22ee2020-11-24T22:35:52ZengIstituto Nazionale di Geofisica e Vulcanologia (INGV)Annals of Geophysics1593-52132037-416X2015-11-0158510.4401/ag-68016056On polar daily geomagnetic variationPaola De Michelis0Giuseppe Consolini1Istituto Nazionale di Geofisica e Vulcanologia, Rome,INAF - Istituto di Astrofisica e Planetologia Spaziali, Rome,<p style="-qt-block-indent: 0; text-indent: 0px; margin: 0px;">The aim of this work is to investigate the nature of the daily magnetic field perturbations produced by ionospheric and magnetospheric currents at high latitudes. We analyse the hourly means of the X and Y geomagnetic field components recorded by a meridian chain of permanent geomagnetic observatories in the polar region of the Northern Hemisphere during a period of four years (1995-1998) around the solar minimum. We apply a mathematical method, known as natural orthogonal component (NOC), which is capable of characterizing the dominant modes of the geomagnetic field daily variability through a set of empirical orthogonal functions (EOFs). Using the first two modes we reconstruct a two-dimensional equivalent current representation of the ionospheric electric currents, which contribute substantially to the geomagnetic daily variations. The obtained current structures resemble the equivalent current patterns of DP2 and DP1. We characterize these currents by studying their evolution with the geomagnetic activity level and by analysing their dependence on the interplanetary magnetic field. The obtained results support the idea of a coexistence of two main processes during all analysed period although one of them, the directly driven process, represents the dominant component of the geomagnetic daily variation.</p>http://www.annalsofgeophysics.eu/index.php/annals/article/view/6801Daily geomagnetic variationSun-Earth interactionNatural orthogonal component analysis
collection DOAJ
language English
format Article
sources DOAJ
author Paola De Michelis
Giuseppe Consolini
spellingShingle Paola De Michelis
Giuseppe Consolini
On polar daily geomagnetic variation
Annals of Geophysics
Daily geomagnetic variation
Sun-Earth interaction
Natural orthogonal component analysis
author_facet Paola De Michelis
Giuseppe Consolini
author_sort Paola De Michelis
title On polar daily geomagnetic variation
title_short On polar daily geomagnetic variation
title_full On polar daily geomagnetic variation
title_fullStr On polar daily geomagnetic variation
title_full_unstemmed On polar daily geomagnetic variation
title_sort on polar daily geomagnetic variation
publisher Istituto Nazionale di Geofisica e Vulcanologia (INGV)
series Annals of Geophysics
issn 1593-5213
2037-416X
publishDate 2015-11-01
description <p style="-qt-block-indent: 0; text-indent: 0px; margin: 0px;">The aim of this work is to investigate the nature of the daily magnetic field perturbations produced by ionospheric and magnetospheric currents at high latitudes. We analyse the hourly means of the X and Y geomagnetic field components recorded by a meridian chain of permanent geomagnetic observatories in the polar region of the Northern Hemisphere during a period of four years (1995-1998) around the solar minimum. We apply a mathematical method, known as natural orthogonal component (NOC), which is capable of characterizing the dominant modes of the geomagnetic field daily variability through a set of empirical orthogonal functions (EOFs). Using the first two modes we reconstruct a two-dimensional equivalent current representation of the ionospheric electric currents, which contribute substantially to the geomagnetic daily variations. The obtained current structures resemble the equivalent current patterns of DP2 and DP1. We characterize these currents by studying their evolution with the geomagnetic activity level and by analysing their dependence on the interplanetary magnetic field. The obtained results support the idea of a coexistence of two main processes during all analysed period although one of them, the directly driven process, represents the dominant component of the geomagnetic daily variation.</p>
topic Daily geomagnetic variation
Sun-Earth interaction
Natural orthogonal component analysis
url http://www.annalsofgeophysics.eu/index.php/annals/article/view/6801
work_keys_str_mv AT paolademichelis onpolardailygeomagneticvariation
AT giuseppeconsolini onpolardailygeomagneticvariation
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