Effect of Non‐Dipole Field on VGP Estimation
Abstract The virtual geomagnetic pole (VGP) calculated under the assumption of a central dipole field is generally different from the real geomagnetic pole (RGP) since effect of the non‐dipole field. In order to quantitatively examine effects of the non‐dipole field on VGP determination, the VGP and...
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Online Access: | http://dx.doi.org/10.1002/cjg2.1130 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fcjg2.1130 https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/cjg2.1130 |
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crwiley:10.1002/cjg2.1130 2024-06-02T07:57:21+00:00 Effect of Non‐Dipole Field on VGP Estimation 2007 http://dx.doi.org/10.1002/cjg2.1130 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fcjg2.1130 https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/cjg2.1130 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Chinese Journal of Geophysics volume 50, issue 5, page 1117-1122 ISSN 0898-9591 2326-0440 journal-article 2007 crwiley https://doi.org/10.1002/cjg2.1130 2024-05-03T12:02:46Z Abstract The virtual geomagnetic pole (VGP) calculated under the assumption of a central dipole field is generally different from the real geomagnetic pole (RGP) since effect of the non‐dipole field. In order to quantitatively examine effects of the non‐dipole field on VGP determination, the VGP and RGP are calculated at 5° × 5° virtual sites by using the IGRF1900~2000 models. The results show significant departures of VGP from RGP in some major magnetic anomaly regions. The latitude departures of VGP from the RGP are as large as 25° in these anomaly regions, although they are acceptable in most sites on the earth's surface (less than 10°), mainly confined in the regions with a weak intensity of the non‐dipole field, such as Pacific Ocean. The longitude departures of VGP from RGP are much more remarkable, scattering in a wide range from –180° to 180° in Eurasian continent. The angle distance between VGP and the RGP are generally within a range of 15°, except the Antarctica, South Atlantic Ocean and Eurasia regions. Article in Journal/Newspaper Antarc* Antarctica Geomagnetic Pole South Atlantic Ocean Wiley Online Library Pacific Chinese Journal of Geophysics 50 5 1117 1122 |
institution |
Open Polar |
collection |
Wiley Online Library |
op_collection_id |
crwiley |
language |
English |
description |
Abstract The virtual geomagnetic pole (VGP) calculated under the assumption of a central dipole field is generally different from the real geomagnetic pole (RGP) since effect of the non‐dipole field. In order to quantitatively examine effects of the non‐dipole field on VGP determination, the VGP and RGP are calculated at 5° × 5° virtual sites by using the IGRF1900~2000 models. The results show significant departures of VGP from RGP in some major magnetic anomaly regions. The latitude departures of VGP from the RGP are as large as 25° in these anomaly regions, although they are acceptable in most sites on the earth's surface (less than 10°), mainly confined in the regions with a weak intensity of the non‐dipole field, such as Pacific Ocean. The longitude departures of VGP from RGP are much more remarkable, scattering in a wide range from –180° to 180° in Eurasian continent. The angle distance between VGP and the RGP are generally within a range of 15°, except the Antarctica, South Atlantic Ocean and Eurasia regions. |
format |
Article in Journal/Newspaper |
title |
Effect of Non‐Dipole Field on VGP Estimation |
spellingShingle |
Effect of Non‐Dipole Field on VGP Estimation |
title_short |
Effect of Non‐Dipole Field on VGP Estimation |
title_full |
Effect of Non‐Dipole Field on VGP Estimation |
title_fullStr |
Effect of Non‐Dipole Field on VGP Estimation |
title_full_unstemmed |
Effect of Non‐Dipole Field on VGP Estimation |
title_sort |
effect of non‐dipole field on vgp estimation |
publisher |
Wiley |
publishDate |
2007 |
url |
http://dx.doi.org/10.1002/cjg2.1130 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fcjg2.1130 https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/cjg2.1130 |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
Antarc* Antarctica Geomagnetic Pole South Atlantic Ocean |
genre_facet |
Antarc* Antarctica Geomagnetic Pole South Atlantic Ocean |
op_source |
Chinese Journal of Geophysics volume 50, issue 5, page 1117-1122 ISSN 0898-9591 2326-0440 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/cjg2.1130 |
container_title |
Chinese Journal of Geophysics |
container_volume |
50 |
container_issue |
5 |
container_start_page |
1117 |
op_container_end_page |
1122 |
_version_ |
1800740500091699200 |