The Study of Westward Drift in the Main Geomagnetic Field

We have obtained a solution for the velocity of westward drift from the induction equation in which an approach for main geomagnetic field was built. Distribution functions B(r, t) entered into the induction equation have been built by the observatories' data in North America and the Europe fro...

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Main Author: G. Bayanjargal
Format: Article
Language:English
Published: Wiley 2013-01-01
Series:International Journal of Geophysics
Online Access:http://dx.doi.org/10.1155/2013/202763
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author G. Bayanjargal
author_facet G. Bayanjargal
author_sort G. Bayanjargal
collection DOAJ
description We have obtained a solution for the velocity of westward drift from the induction equation in which an approach for main geomagnetic field was built. Distribution functions B(r, t) entered into the induction equation have been built by the observatories' data in North America and the Europe from 1991 to 2006. The longitudinal −0.123 degree/year and latitudinal 0.068 degree/year drifts were defined in North America. And the longitudinal −0.257 degree/year drift was defined in Europe from 1991 to 2006. These drifts are similar to results of other studies.
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institution Kabale University
issn 1687-885X
1687-8868
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publishDate 2013-01-01
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series International Journal of Geophysics
spelling doaj-art-792e4e997c28499baa66983e87d4a5302025-02-03T01:10:37ZengWileyInternational Journal of Geophysics1687-885X1687-88682013-01-01201310.1155/2013/202763202763The Study of Westward Drift in the Main Geomagnetic FieldG. Bayanjargal0Research Center for Astronomy and Geophysics, Mongolian Academy of Sciences (MAS), Ulaanbaatar, MongoliaWe have obtained a solution for the velocity of westward drift from the induction equation in which an approach for main geomagnetic field was built. Distribution functions B(r, t) entered into the induction equation have been built by the observatories' data in North America and the Europe from 1991 to 2006. The longitudinal −0.123 degree/year and latitudinal 0.068 degree/year drifts were defined in North America. And the longitudinal −0.257 degree/year drift was defined in Europe from 1991 to 2006. These drifts are similar to results of other studies.http://dx.doi.org/10.1155/2013/202763
spellingShingle G. Bayanjargal
The Study of Westward Drift in the Main Geomagnetic Field
International Journal of Geophysics
title The Study of Westward Drift in the Main Geomagnetic Field
title_full The Study of Westward Drift in the Main Geomagnetic Field
title_fullStr The Study of Westward Drift in the Main Geomagnetic Field
title_full_unstemmed The Study of Westward Drift in the Main Geomagnetic Field
title_short The Study of Westward Drift in the Main Geomagnetic Field
title_sort study of westward drift in the main geomagnetic field
url http://dx.doi.org/10.1155/2013/202763
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