Remarks on the mean-square values of the geomagnetic field and its components

When considering functions on the Earth's (spherical) surface, mean-square values are often used to indicate their (relative) magnitude. If a function is separated into it, (essentially) spherical harmonic components then, provided these individual harmonic components are orthogonal over the su...

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Main Authors: F. J. Lowes, C. Falcone, A. De Santis
Format: Article
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 1995-06-01
Series:Annals of Geophysics
Subjects:
Online Access:http://www.annalsofgeophysics.eu/index.php/annals/article/view/4117
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author F. J. Lowes
C. Falcone
A. De Santis
author_facet F. J. Lowes
C. Falcone
A. De Santis
author_sort F. J. Lowes
collection DOAJ
description When considering functions on the Earth's (spherical) surface, mean-square values are often used to indicate their (relative) magnitude. If a function is separated into it, (essentially) spherical harmonic components then, provided these individual harmonic components are orthogonal over the surface, the concept of spatial power spectrum can be introduced, with each harmonic contributing separately to the total mean square value; this is true for the geomagnetic field vector B, its horizontal component vector H, and its vertical component z. However, because of the lack of orthogonality this concept is not applicable to the horizontal X and y components individually; problems which arise from this are discussed.
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spelling doaj.art-d8c5af28c28c4a049e51662701ef3cbb2022-12-21T23:59:47ZengIstituto Nazionale di Geofisica e Vulcanologia (INGV)Annals of Geophysics1593-52132037-416X1995-06-0138210.4401/ag-4117Remarks on the mean-square values of the geomagnetic field and its componentsF. J. LowesC. FalconeA. De SantisWhen considering functions on the Earth's (spherical) surface, mean-square values are often used to indicate their (relative) magnitude. If a function is separated into it, (essentially) spherical harmonic components then, provided these individual harmonic components are orthogonal over the surface, the concept of spatial power spectrum can be introduced, with each harmonic contributing separately to the total mean square value; this is true for the geomagnetic field vector B, its horizontal component vector H, and its vertical component z. However, because of the lack of orthogonality this concept is not applicable to the horizontal X and y components individually; problems which arise from this are discussed.http://www.annalsofgeophysics.eu/index.php/annals/article/view/4117spherical harmonicsorthogonalitygeomagnetic spectrum
spellingShingle F. J. Lowes
C. Falcone
A. De Santis
Remarks on the mean-square values of the geomagnetic field and its components
Annals of Geophysics
spherical harmonics
orthogonality
geomagnetic spectrum
title Remarks on the mean-square values of the geomagnetic field and its components
title_full Remarks on the mean-square values of the geomagnetic field and its components
title_fullStr Remarks on the mean-square values of the geomagnetic field and its components
title_full_unstemmed Remarks on the mean-square values of the geomagnetic field and its components
title_short Remarks on the mean-square values of the geomagnetic field and its components
title_sort remarks on the mean square values of the geomagnetic field and its components
topic spherical harmonics
orthogonality
geomagnetic spectrum
url http://www.annalsofgeophysics.eu/index.php/annals/article/view/4117
work_keys_str_mv AT fjlowes remarksonthemeansquarevaluesofthegeomagneticfieldanditscomponents
AT cfalcone remarksonthemeansquarevaluesofthegeomagneticfieldanditscomponents
AT adesantis remarksonthemeansquarevaluesofthegeomagneticfieldanditscomponents