Secular variations of the geomagnetic field at the African plate
Geomagnetic secular variations at the African plate consist of shortperiod and longperiod components. Shortperiod SV depends on solar activity. To separate longperiod SV for the Athens magnetic observatories with confidence is impossible so, as rows of mean year values at most observatories are shor...
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| Date: | 2017 |
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| Main Authors: | , |
| Format: | Article |
| Language: | Ukrainian |
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S. Subbotin Institute of Geophysics of the NAS of Ukraine
2017
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| Online Access: | https://journals.uran.ua/geofizicheskiy/article/view/97375 |
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| Journal Title: | Geofizicheskiy Zhurnal |
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Geofizicheskiy Zhurnal| _version_ | 1856543121991532544 |
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| author | Sumaruk, Yu. P. Sumaruk, T. P. |
| author_facet | Sumaruk, Yu. P. Sumaruk, T. P. |
| author_sort | Sumaruk, Yu. P. |
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| collection | OJS |
| datestamp_date | 2020-10-07T11:14:31Z |
| description | Geomagnetic secular variations at the African plate consist of shortperiod and longperiod components. Shortperiod SV depends on solar activity. To separate longperiod SV for the Athens magnetic observatories with confidence is impossible so, as rows of mean year values at most observatories are short. We used the data of fifteen observatories, but only MLT, TAN and PLS made observations from the twentieth century beginning.On the data of these observatories and fragment data another ones, the 80-year period of SV may be discovered. These variations have quasisinusoidal form and their extremums coinside to the solar activity maximuma.SV are generated by internal and external sources. The internal sources manifest itself at vertical component and external ones in horizontal component of the geomagnetic field. SV (observed variation) may be devided on the quasiconstant (SV1) and variable quantities. We have chosen as SV1 variations at 1979 year. At this year the sign of SV changes at all observatories. There was supposed that SV1 reflects the sources connected to the changes of region tectonic. The differences between SV and SV1 reflects the external sources component, and it is confirmed by its connection to solar activity change.On the coast and islands observatories the values of shortperiod and longperiod variations were increased.On the tectonic most active east part of African plate SV were more active. Distinctive peculiarity of the SV on the African plate is decreasing of the SV absolute values. It begins at the end of 70-th year of twentieth century. It means the sources of the geomagnetic field relaxe. |
| first_indexed | 2025-07-17T11:04:52Z |
| format | Article |
| id | journalsuranua-geofizicheskiy-article-97375 |
| institution | Geofizicheskiy Zhurnal |
| language | Ukrainian |
| last_indexed | 2025-07-17T11:04:52Z |
| publishDate | 2017 |
| publisher | S. Subbotin Institute of Geophysics of the NAS of Ukraine |
| record_format | ojs |
| spelling | journalsuranua-geofizicheskiy-article-973752020-10-07T11:14:31Z Secular variations of the geomagnetic field at the African plate Sumaruk, Yu. P. Sumaruk, T. P. secular variations external and internal sources African plate Geomagnetic secular variations at the African plate consist of shortperiod and longperiod components. Shortperiod SV depends on solar activity. To separate longperiod SV for the Athens magnetic observatories with confidence is impossible so, as rows of mean year values at most observatories are short. We used the data of fifteen observatories, but only MLT, TAN and PLS made observations from the twentieth century beginning.On the data of these observatories and fragment data another ones, the 80-year period of SV may be discovered. These variations have quasisinusoidal form and their extremums coinside to the solar activity maximuma.SV are generated by internal and external sources. The internal sources manifest itself at vertical component and external ones in horizontal component of the geomagnetic field. SV (observed variation) may be devided on the quasiconstant (SV1) and variable quantities. We have chosen as SV1 variations at 1979 year. At this year the sign of SV changes at all observatories. There was supposed that SV1 reflects the sources connected to the changes of region tectonic. The differences between SV and SV1 reflects the external sources component, and it is confirmed by its connection to solar activity change.On the coast and islands observatories the values of shortperiod and longperiod variations were increased.On the tectonic most active east part of African plate SV were more active. Distinctive peculiarity of the SV on the African plate is decreasing of the SV absolute values. It begins at the end of 70-th year of twentieth century. It means the sources of the geomagnetic field relaxe. S. Subbotin Institute of Geophysics of the NAS of Ukraine 2017-06-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/97375 10.24028/gzh.0203-3100.v39i2.2017.97375 Geofizicheskiy Zhurnal; Vol. 39 No. 2 (2017); 96-108 Геофизический журнал; Том 39 № 2 (2017); 96-108 Геофізичний журнал; Том 39 № 2 (2017); 96-108 2524-1052 0203-3100 uk https://journals.uran.ua/geofizicheskiy/article/view/97375/95024 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0 |
| spellingShingle | secular variations external and internal sources African plate Sumaruk, Yu. P. Sumaruk, T. P. Secular variations of the geomagnetic field at the African plate |
| title | Secular variations of the geomagnetic field at the African plate |
| title_full | Secular variations of the geomagnetic field at the African plate |
| title_fullStr | Secular variations of the geomagnetic field at the African plate |
| title_full_unstemmed | Secular variations of the geomagnetic field at the African plate |
| title_short | Secular variations of the geomagnetic field at the African plate |
| title_sort | secular variations of the geomagnetic field at the african plate |
| topic | secular variations external and internal sources African plate |
| topic_facet | secular variations external and internal sources African plate |
| url | https://journals.uran.ua/geofizicheskiy/article/view/97375 |
| work_keys_str_mv | AT sumarukyup secularvariationsofthegeomagneticfieldattheafricanplate AT sumaruktp secularvariationsofthegeomagneticfieldattheafricanplate |