Empirical model of equatorial electrojet based on ground-based magnetometer data during solar minimum in fall
Abstract In this study, we constructed an empirical model of the equatorial electrojet (EEJ), including local time and longitudinal dependence, based on simultaneous data from 12 magnetometer stations located in six longitude sectors. An analysis was carried out using the equatorial electrojet index...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Hamid, Nurul Shazana Abdul [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2015 |
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| Schlagwörter: |
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| Anmerkung: |
© Hamid et al. 2015 |
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| Übergeordnetes Werk: |
Enthalten in: Earth, planets and space - Heidelberg : Springer, 1998, 67(2015), 1 vom: 29. Dez. |
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| Übergeordnetes Werk: |
volume:67 ; year:2015 ; number:1 ; day:29 ; month:12 |
| Links: |
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| DOI / URN: |
10.1186/s40623-015-0373-1 |
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SPR036924369 |
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| 100 | 1 | |a Hamid, Nurul Shazana Abdul |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Empirical model of equatorial electrojet based on ground-based magnetometer data during solar minimum in fall |
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| 520 | |a Abstract In this study, we constructed an empirical model of the equatorial electrojet (EEJ), including local time and longitudinal dependence, based on simultaneous data from 12 magnetometer stations located in six longitude sectors. An analysis was carried out using the equatorial electrojet index, EUEL, calculated from the geomagnetic northward H component. The magnetic EEJ strength is calculated as the difference between the normalized EUEL index of the magnetic dip equator station and the normalized EUEL index of the off-dip equator station located beyond the EEJ band. Analysis showed that this current is always strongest in the South American sector, regardless of local time (LT), and weakest in the Indian sector during 0900 and 1000 LT, but shifted to the African sector during 1100 to 1400 LT. These longitude variations of EEJ roughly follow variations of the inversed main field strength along the dip equator, except for the Indian and Southeast Asian sectors. The result showed that the EEJ component derived from the model exhibits a similar pattern with measured EEJ from ground data during noontime, mainly before 1300 LT. | ||
| 650 | 4 | |a Equatorial electrojet |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Empirical model |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Local time dependence |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Longitudinal dependence |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Liu, Huixin |4 aut | |
| 700 | 1 | |a Uozumi, Teiji |4 aut | |
| 700 | 1 | |a Yoshikawa, Akimasa |4 aut | |
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10.1186/s40623-015-0373-1 doi (DE-627)SPR036924369 (SPR)s40623-015-0373-1-e DE-627 ger DE-627 rakwb eng Hamid, Nurul Shazana Abdul verfasserin aut Empirical model of equatorial electrojet based on ground-based magnetometer data during solar minimum in fall 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Hamid et al. 2015 Abstract In this study, we constructed an empirical model of the equatorial electrojet (EEJ), including local time and longitudinal dependence, based on simultaneous data from 12 magnetometer stations located in six longitude sectors. An analysis was carried out using the equatorial electrojet index, EUEL, calculated from the geomagnetic northward H component. The magnetic EEJ strength is calculated as the difference between the normalized EUEL index of the magnetic dip equator station and the normalized EUEL index of the off-dip equator station located beyond the EEJ band. Analysis showed that this current is always strongest in the South American sector, regardless of local time (LT), and weakest in the Indian sector during 0900 and 1000 LT, but shifted to the African sector during 1100 to 1400 LT. These longitude variations of EEJ roughly follow variations of the inversed main field strength along the dip equator, except for the Indian and Southeast Asian sectors. The result showed that the EEJ component derived from the model exhibits a similar pattern with measured EEJ from ground data during noontime, mainly before 1300 LT. Equatorial electrojet (dpeaa)DE-He213 Empirical model (dpeaa)DE-He213 Local time dependence (dpeaa)DE-He213 Longitudinal dependence (dpeaa)DE-He213 Liu, Huixin aut Uozumi, Teiji aut Yoshikawa, Akimasa aut Enthalten in Earth, planets and space Heidelberg : Springer, 1998 67(2015), 1 vom: 29. Dez. (DE-627)353898597 (DE-600)2087663-4 1880-5981 nnns volume:67 year:2015 number:1 day:29 month:12 https://dx.doi.org/10.1186/s40623-015-0373-1 kostenfrei Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 67 2015 1 29 12 |
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10.1186/s40623-015-0373-1 doi (DE-627)SPR036924369 (SPR)s40623-015-0373-1-e DE-627 ger DE-627 rakwb eng Hamid, Nurul Shazana Abdul verfasserin aut Empirical model of equatorial electrojet based on ground-based magnetometer data during solar minimum in fall 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Hamid et al. 2015 Abstract In this study, we constructed an empirical model of the equatorial electrojet (EEJ), including local time and longitudinal dependence, based on simultaneous data from 12 magnetometer stations located in six longitude sectors. An analysis was carried out using the equatorial electrojet index, EUEL, calculated from the geomagnetic northward H component. The magnetic EEJ strength is calculated as the difference between the normalized EUEL index of the magnetic dip equator station and the normalized EUEL index of the off-dip equator station located beyond the EEJ band. Analysis showed that this current is always strongest in the South American sector, regardless of local time (LT), and weakest in the Indian sector during 0900 and 1000 LT, but shifted to the African sector during 1100 to 1400 LT. These longitude variations of EEJ roughly follow variations of the inversed main field strength along the dip equator, except for the Indian and Southeast Asian sectors. The result showed that the EEJ component derived from the model exhibits a similar pattern with measured EEJ from ground data during noontime, mainly before 1300 LT. Equatorial electrojet (dpeaa)DE-He213 Empirical model (dpeaa)DE-He213 Local time dependence (dpeaa)DE-He213 Longitudinal dependence (dpeaa)DE-He213 Liu, Huixin aut Uozumi, Teiji aut Yoshikawa, Akimasa aut Enthalten in Earth, planets and space Heidelberg : Springer, 1998 67(2015), 1 vom: 29. Dez. (DE-627)353898597 (DE-600)2087663-4 1880-5981 nnns volume:67 year:2015 number:1 day:29 month:12 https://dx.doi.org/10.1186/s40623-015-0373-1 kostenfrei Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 67 2015 1 29 12 |
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10.1186/s40623-015-0373-1 doi (DE-627)SPR036924369 (SPR)s40623-015-0373-1-e DE-627 ger DE-627 rakwb eng Hamid, Nurul Shazana Abdul verfasserin aut Empirical model of equatorial electrojet based on ground-based magnetometer data during solar minimum in fall 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Hamid et al. 2015 Abstract In this study, we constructed an empirical model of the equatorial electrojet (EEJ), including local time and longitudinal dependence, based on simultaneous data from 12 magnetometer stations located in six longitude sectors. An analysis was carried out using the equatorial electrojet index, EUEL, calculated from the geomagnetic northward H component. The magnetic EEJ strength is calculated as the difference between the normalized EUEL index of the magnetic dip equator station and the normalized EUEL index of the off-dip equator station located beyond the EEJ band. Analysis showed that this current is always strongest in the South American sector, regardless of local time (LT), and weakest in the Indian sector during 0900 and 1000 LT, but shifted to the African sector during 1100 to 1400 LT. These longitude variations of EEJ roughly follow variations of the inversed main field strength along the dip equator, except for the Indian and Southeast Asian sectors. The result showed that the EEJ component derived from the model exhibits a similar pattern with measured EEJ from ground data during noontime, mainly before 1300 LT. Equatorial electrojet (dpeaa)DE-He213 Empirical model (dpeaa)DE-He213 Local time dependence (dpeaa)DE-He213 Longitudinal dependence (dpeaa)DE-He213 Liu, Huixin aut Uozumi, Teiji aut Yoshikawa, Akimasa aut Enthalten in Earth, planets and space Heidelberg : Springer, 1998 67(2015), 1 vom: 29. Dez. (DE-627)353898597 (DE-600)2087663-4 1880-5981 nnns volume:67 year:2015 number:1 day:29 month:12 https://dx.doi.org/10.1186/s40623-015-0373-1 kostenfrei Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 67 2015 1 29 12 |
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10.1186/s40623-015-0373-1 doi (DE-627)SPR036924369 (SPR)s40623-015-0373-1-e DE-627 ger DE-627 rakwb eng Hamid, Nurul Shazana Abdul verfasserin aut Empirical model of equatorial electrojet based on ground-based magnetometer data during solar minimum in fall 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Hamid et al. 2015 Abstract In this study, we constructed an empirical model of the equatorial electrojet (EEJ), including local time and longitudinal dependence, based on simultaneous data from 12 magnetometer stations located in six longitude sectors. An analysis was carried out using the equatorial electrojet index, EUEL, calculated from the geomagnetic northward H component. The magnetic EEJ strength is calculated as the difference between the normalized EUEL index of the magnetic dip equator station and the normalized EUEL index of the off-dip equator station located beyond the EEJ band. Analysis showed that this current is always strongest in the South American sector, regardless of local time (LT), and weakest in the Indian sector during 0900 and 1000 LT, but shifted to the African sector during 1100 to 1400 LT. These longitude variations of EEJ roughly follow variations of the inversed main field strength along the dip equator, except for the Indian and Southeast Asian sectors. The result showed that the EEJ component derived from the model exhibits a similar pattern with measured EEJ from ground data during noontime, mainly before 1300 LT. Equatorial electrojet (dpeaa)DE-He213 Empirical model (dpeaa)DE-He213 Local time dependence (dpeaa)DE-He213 Longitudinal dependence (dpeaa)DE-He213 Liu, Huixin aut Uozumi, Teiji aut Yoshikawa, Akimasa aut Enthalten in Earth, planets and space Heidelberg : Springer, 1998 67(2015), 1 vom: 29. Dez. (DE-627)353898597 (DE-600)2087663-4 1880-5981 nnns volume:67 year:2015 number:1 day:29 month:12 https://dx.doi.org/10.1186/s40623-015-0373-1 kostenfrei Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 67 2015 1 29 12 |
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10.1186/s40623-015-0373-1 doi (DE-627)SPR036924369 (SPR)s40623-015-0373-1-e DE-627 ger DE-627 rakwb eng Hamid, Nurul Shazana Abdul verfasserin aut Empirical model of equatorial electrojet based on ground-based magnetometer data during solar minimum in fall 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Hamid et al. 2015 Abstract In this study, we constructed an empirical model of the equatorial electrojet (EEJ), including local time and longitudinal dependence, based on simultaneous data from 12 magnetometer stations located in six longitude sectors. An analysis was carried out using the equatorial electrojet index, EUEL, calculated from the geomagnetic northward H component. The magnetic EEJ strength is calculated as the difference between the normalized EUEL index of the magnetic dip equator station and the normalized EUEL index of the off-dip equator station located beyond the EEJ band. Analysis showed that this current is always strongest in the South American sector, regardless of local time (LT), and weakest in the Indian sector during 0900 and 1000 LT, but shifted to the African sector during 1100 to 1400 LT. These longitude variations of EEJ roughly follow variations of the inversed main field strength along the dip equator, except for the Indian and Southeast Asian sectors. The result showed that the EEJ component derived from the model exhibits a similar pattern with measured EEJ from ground data during noontime, mainly before 1300 LT. Equatorial electrojet (dpeaa)DE-He213 Empirical model (dpeaa)DE-He213 Local time dependence (dpeaa)DE-He213 Longitudinal dependence (dpeaa)DE-He213 Liu, Huixin aut Uozumi, Teiji aut Yoshikawa, Akimasa aut Enthalten in Earth, planets and space Heidelberg : Springer, 1998 67(2015), 1 vom: 29. Dez. (DE-627)353898597 (DE-600)2087663-4 1880-5981 nnns volume:67 year:2015 number:1 day:29 month:12 https://dx.doi.org/10.1186/s40623-015-0373-1 kostenfrei Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 67 2015 1 29 12 |
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Enthalten in Earth, planets and space 67(2015), 1 vom: 29. Dez. volume:67 year:2015 number:1 day:29 month:12 |
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Hamid, Nurul Shazana Abdul @@aut@@ Liu, Huixin @@aut@@ Uozumi, Teiji @@aut@@ Yoshikawa, Akimasa @@aut@@ |
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Hamid, Nurul Shazana Abdul |
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empirical model of equatorial electrojet based on ground-based magnetometer data during solar minimum in fall |
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Empirical model of equatorial electrojet based on ground-based magnetometer data during solar minimum in fall |
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Abstract In this study, we constructed an empirical model of the equatorial electrojet (EEJ), including local time and longitudinal dependence, based on simultaneous data from 12 magnetometer stations located in six longitude sectors. An analysis was carried out using the equatorial electrojet index, EUEL, calculated from the geomagnetic northward H component. The magnetic EEJ strength is calculated as the difference between the normalized EUEL index of the magnetic dip equator station and the normalized EUEL index of the off-dip equator station located beyond the EEJ band. Analysis showed that this current is always strongest in the South American sector, regardless of local time (LT), and weakest in the Indian sector during 0900 and 1000 LT, but shifted to the African sector during 1100 to 1400 LT. These longitude variations of EEJ roughly follow variations of the inversed main field strength along the dip equator, except for the Indian and Southeast Asian sectors. The result showed that the EEJ component derived from the model exhibits a similar pattern with measured EEJ from ground data during noontime, mainly before 1300 LT. © Hamid et al. 2015 |
| abstractGer |
Abstract In this study, we constructed an empirical model of the equatorial electrojet (EEJ), including local time and longitudinal dependence, based on simultaneous data from 12 magnetometer stations located in six longitude sectors. An analysis was carried out using the equatorial electrojet index, EUEL, calculated from the geomagnetic northward H component. The magnetic EEJ strength is calculated as the difference between the normalized EUEL index of the magnetic dip equator station and the normalized EUEL index of the off-dip equator station located beyond the EEJ band. Analysis showed that this current is always strongest in the South American sector, regardless of local time (LT), and weakest in the Indian sector during 0900 and 1000 LT, but shifted to the African sector during 1100 to 1400 LT. These longitude variations of EEJ roughly follow variations of the inversed main field strength along the dip equator, except for the Indian and Southeast Asian sectors. The result showed that the EEJ component derived from the model exhibits a similar pattern with measured EEJ from ground data during noontime, mainly before 1300 LT. © Hamid et al. 2015 |
| abstract_unstemmed |
Abstract In this study, we constructed an empirical model of the equatorial electrojet (EEJ), including local time and longitudinal dependence, based on simultaneous data from 12 magnetometer stations located in six longitude sectors. An analysis was carried out using the equatorial electrojet index, EUEL, calculated from the geomagnetic northward H component. The magnetic EEJ strength is calculated as the difference between the normalized EUEL index of the magnetic dip equator station and the normalized EUEL index of the off-dip equator station located beyond the EEJ band. Analysis showed that this current is always strongest in the South American sector, regardless of local time (LT), and weakest in the Indian sector during 0900 and 1000 LT, but shifted to the African sector during 1100 to 1400 LT. These longitude variations of EEJ roughly follow variations of the inversed main field strength along the dip equator, except for the Indian and Southeast Asian sectors. The result showed that the EEJ component derived from the model exhibits a similar pattern with measured EEJ from ground data during noontime, mainly before 1300 LT. © Hamid et al. 2015 |
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| score |
7.3991175 |