The Superposition of Auroral Currents in the Region of the Harang Discontinuity
Abstract Cases of superposition of auroral electric jets in the auroral zone at the instances of development of the Harang discontinuity have been found and described using the data from ground-based magnetometers. It is shown that special conditions for the development of elements of current system...
Ausführliche Beschreibung
Autor*in: |
Zaitsev, A. N. [verfasserIn] |
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E-Artikel |
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Sprache: |
Englisch |
Erschienen: |
2022 |
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Anmerkung: |
© Pleiades Publishing, Ltd. 2022. ISSN 0016-7932, Geomagnetism and Aeronomy, 2022, Vol. 62, No. 5, pp. 563–572. © Pleiades Publishing, Ltd., 2022, corrected publication 2022. Russian Text © The Author(s), 2022, published in Geomagnetizm i Aeronomiya, 2022, Vol. 62, No. 5, pp. 607–616. |
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Übergeordnetes Werk: |
Enthalten in: Geomagnetism and aeronomy - Moscow : MAIK Nauka/Interperiodica Publ., 1996, 62(2022), 5 vom: 28. Sept., Seite 563-572 |
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Übergeordnetes Werk: |
volume:62 ; year:2022 ; number:5 ; day:28 ; month:09 ; pages:563-572 |
Links: |
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DOI / URN: |
10.1134/S0016793222050176 |
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Katalog-ID: |
SPR051021048 |
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520 | |a Abstract Cases of superposition of auroral electric jets in the auroral zone at the instances of development of the Harang discontinuity have been found and described using the data from ground-based magnetometers. It is shown that special conditions for the development of elements of current systems form in the region of the Harang discontinuity, and those can be taken into account only with a special method of separating the types of variations according to morphological features. With an accuracy of determining the position of electric jets from ground data within tens of kilometers, the convergence of electric jets at the altitude of the ionospheric E-layer of 115 km is 20–30 km. The discovered properties of currents during the formation of the Harang discontinuity should be taken into account in the construction of an equivalent ionospheric current system that determines the dynamics of substorm development. | ||
700 | 1 | |a Kanonidi, K. Kh. |4 aut | |
700 | 1 | |a Petrov, V. G. |4 aut | |
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10.1134/S0016793222050176 doi (DE-627)SPR051021048 (SPR)S0016793222050176-e DE-627 ger DE-627 rakwb eng Zaitsev, A. N. verfasserin aut The Superposition of Auroral Currents in the Region of the Harang Discontinuity 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2022. ISSN 0016-7932, Geomagnetism and Aeronomy, 2022, Vol. 62, No. 5, pp. 563–572. © Pleiades Publishing, Ltd., 2022, corrected publication 2022. Russian Text © The Author(s), 2022, published in Geomagnetizm i Aeronomiya, 2022, Vol. 62, No. 5, pp. 607–616. Abstract Cases of superposition of auroral electric jets in the auroral zone at the instances of development of the Harang discontinuity have been found and described using the data from ground-based magnetometers. It is shown that special conditions for the development of elements of current systems form in the region of the Harang discontinuity, and those can be taken into account only with a special method of separating the types of variations according to morphological features. With an accuracy of determining the position of electric jets from ground data within tens of kilometers, the convergence of electric jets at the altitude of the ionospheric E-layer of 115 km is 20–30 km. The discovered properties of currents during the formation of the Harang discontinuity should be taken into account in the construction of an equivalent ionospheric current system that determines the dynamics of substorm development. Kanonidi, K. Kh. aut Petrov, V. G. aut Enthalten in Geomagnetism and aeronomy Moscow : MAIK Nauka/Interperiodica Publ., 1996 62(2022), 5 vom: 28. Sept., Seite 563-572 (DE-627)342320920 (DE-600)2071667-9 1555-645X nnns volume:62 year:2022 number:5 day:28 month:09 pages:563-572 https://dx.doi.org/10.1134/S0016793222050176 lizenzpflichtig 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_32 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_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 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_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 62 2022 5 28 09 563-572 |
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10.1134/S0016793222050176 doi (DE-627)SPR051021048 (SPR)S0016793222050176-e DE-627 ger DE-627 rakwb eng Zaitsev, A. N. verfasserin aut The Superposition of Auroral Currents in the Region of the Harang Discontinuity 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2022. ISSN 0016-7932, Geomagnetism and Aeronomy, 2022, Vol. 62, No. 5, pp. 563–572. © Pleiades Publishing, Ltd., 2022, corrected publication 2022. Russian Text © The Author(s), 2022, published in Geomagnetizm i Aeronomiya, 2022, Vol. 62, No. 5, pp. 607–616. Abstract Cases of superposition of auroral electric jets in the auroral zone at the instances of development of the Harang discontinuity have been found and described using the data from ground-based magnetometers. It is shown that special conditions for the development of elements of current systems form in the region of the Harang discontinuity, and those can be taken into account only with a special method of separating the types of variations according to morphological features. With an accuracy of determining the position of electric jets from ground data within tens of kilometers, the convergence of electric jets at the altitude of the ionospheric E-layer of 115 km is 20–30 km. The discovered properties of currents during the formation of the Harang discontinuity should be taken into account in the construction of an equivalent ionospheric current system that determines the dynamics of substorm development. Kanonidi, K. Kh. aut Petrov, V. G. aut Enthalten in Geomagnetism and aeronomy Moscow : MAIK Nauka/Interperiodica Publ., 1996 62(2022), 5 vom: 28. Sept., Seite 563-572 (DE-627)342320920 (DE-600)2071667-9 1555-645X nnns volume:62 year:2022 number:5 day:28 month:09 pages:563-572 https://dx.doi.org/10.1134/S0016793222050176 lizenzpflichtig 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_32 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_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 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_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 62 2022 5 28 09 563-572 |
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10.1134/S0016793222050176 doi (DE-627)SPR051021048 (SPR)S0016793222050176-e DE-627 ger DE-627 rakwb eng Zaitsev, A. N. verfasserin aut The Superposition of Auroral Currents in the Region of the Harang Discontinuity 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2022. ISSN 0016-7932, Geomagnetism and Aeronomy, 2022, Vol. 62, No. 5, pp. 563–572. © Pleiades Publishing, Ltd., 2022, corrected publication 2022. Russian Text © The Author(s), 2022, published in Geomagnetizm i Aeronomiya, 2022, Vol. 62, No. 5, pp. 607–616. Abstract Cases of superposition of auroral electric jets in the auroral zone at the instances of development of the Harang discontinuity have been found and described using the data from ground-based magnetometers. It is shown that special conditions for the development of elements of current systems form in the region of the Harang discontinuity, and those can be taken into account only with a special method of separating the types of variations according to morphological features. With an accuracy of determining the position of electric jets from ground data within tens of kilometers, the convergence of electric jets at the altitude of the ionospheric E-layer of 115 km is 20–30 km. The discovered properties of currents during the formation of the Harang discontinuity should be taken into account in the construction of an equivalent ionospheric current system that determines the dynamics of substorm development. Kanonidi, K. Kh. aut Petrov, V. G. aut Enthalten in Geomagnetism and aeronomy Moscow : MAIK Nauka/Interperiodica Publ., 1996 62(2022), 5 vom: 28. Sept., Seite 563-572 (DE-627)342320920 (DE-600)2071667-9 1555-645X nnns volume:62 year:2022 number:5 day:28 month:09 pages:563-572 https://dx.doi.org/10.1134/S0016793222050176 lizenzpflichtig 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_32 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_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 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_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 62 2022 5 28 09 563-572 |
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10.1134/S0016793222050176 doi (DE-627)SPR051021048 (SPR)S0016793222050176-e DE-627 ger DE-627 rakwb eng Zaitsev, A. N. verfasserin aut The Superposition of Auroral Currents in the Region of the Harang Discontinuity 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2022. ISSN 0016-7932, Geomagnetism and Aeronomy, 2022, Vol. 62, No. 5, pp. 563–572. © Pleiades Publishing, Ltd., 2022, corrected publication 2022. Russian Text © The Author(s), 2022, published in Geomagnetizm i Aeronomiya, 2022, Vol. 62, No. 5, pp. 607–616. Abstract Cases of superposition of auroral electric jets in the auroral zone at the instances of development of the Harang discontinuity have been found and described using the data from ground-based magnetometers. It is shown that special conditions for the development of elements of current systems form in the region of the Harang discontinuity, and those can be taken into account only with a special method of separating the types of variations according to morphological features. With an accuracy of determining the position of electric jets from ground data within tens of kilometers, the convergence of electric jets at the altitude of the ionospheric E-layer of 115 km is 20–30 km. The discovered properties of currents during the formation of the Harang discontinuity should be taken into account in the construction of an equivalent ionospheric current system that determines the dynamics of substorm development. Kanonidi, K. Kh. aut Petrov, V. G. aut Enthalten in Geomagnetism and aeronomy Moscow : MAIK Nauka/Interperiodica Publ., 1996 62(2022), 5 vom: 28. Sept., Seite 563-572 (DE-627)342320920 (DE-600)2071667-9 1555-645X nnns volume:62 year:2022 number:5 day:28 month:09 pages:563-572 https://dx.doi.org/10.1134/S0016793222050176 lizenzpflichtig 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_32 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_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 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_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 62 2022 5 28 09 563-572 |
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10.1134/S0016793222050176 doi (DE-627)SPR051021048 (SPR)S0016793222050176-e DE-627 ger DE-627 rakwb eng Zaitsev, A. N. verfasserin aut The Superposition of Auroral Currents in the Region of the Harang Discontinuity 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2022. ISSN 0016-7932, Geomagnetism and Aeronomy, 2022, Vol. 62, No. 5, pp. 563–572. © Pleiades Publishing, Ltd., 2022, corrected publication 2022. Russian Text © The Author(s), 2022, published in Geomagnetizm i Aeronomiya, 2022, Vol. 62, No. 5, pp. 607–616. Abstract Cases of superposition of auroral electric jets in the auroral zone at the instances of development of the Harang discontinuity have been found and described using the data from ground-based magnetometers. It is shown that special conditions for the development of elements of current systems form in the region of the Harang discontinuity, and those can be taken into account only with a special method of separating the types of variations according to morphological features. With an accuracy of determining the position of electric jets from ground data within tens of kilometers, the convergence of electric jets at the altitude of the ionospheric E-layer of 115 km is 20–30 km. The discovered properties of currents during the formation of the Harang discontinuity should be taken into account in the construction of an equivalent ionospheric current system that determines the dynamics of substorm development. Kanonidi, K. Kh. aut Petrov, V. G. aut Enthalten in Geomagnetism and aeronomy Moscow : MAIK Nauka/Interperiodica Publ., 1996 62(2022), 5 vom: 28. Sept., Seite 563-572 (DE-627)342320920 (DE-600)2071667-9 1555-645X nnns volume:62 year:2022 number:5 day:28 month:09 pages:563-572 https://dx.doi.org/10.1134/S0016793222050176 lizenzpflichtig 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_32 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_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 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_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 62 2022 5 28 09 563-572 |
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Zaitsev, A. N. The Superposition of Auroral Currents in the Region of the Harang Discontinuity |
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superposition of auroral currents in the region of the harang discontinuity |
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The Superposition of Auroral Currents in the Region of the Harang Discontinuity |
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Abstract Cases of superposition of auroral electric jets in the auroral zone at the instances of development of the Harang discontinuity have been found and described using the data from ground-based magnetometers. It is shown that special conditions for the development of elements of current systems form in the region of the Harang discontinuity, and those can be taken into account only with a special method of separating the types of variations according to morphological features. With an accuracy of determining the position of electric jets from ground data within tens of kilometers, the convergence of electric jets at the altitude of the ionospheric E-layer of 115 km is 20–30 km. The discovered properties of currents during the formation of the Harang discontinuity should be taken into account in the construction of an equivalent ionospheric current system that determines the dynamics of substorm development. © Pleiades Publishing, Ltd. 2022. ISSN 0016-7932, Geomagnetism and Aeronomy, 2022, Vol. 62, No. 5, pp. 563–572. © Pleiades Publishing, Ltd., 2022, corrected publication 2022. Russian Text © The Author(s), 2022, published in Geomagnetizm i Aeronomiya, 2022, Vol. 62, No. 5, pp. 607–616. |
abstractGer |
Abstract Cases of superposition of auroral electric jets in the auroral zone at the instances of development of the Harang discontinuity have been found and described using the data from ground-based magnetometers. It is shown that special conditions for the development of elements of current systems form in the region of the Harang discontinuity, and those can be taken into account only with a special method of separating the types of variations according to morphological features. With an accuracy of determining the position of electric jets from ground data within tens of kilometers, the convergence of electric jets at the altitude of the ionospheric E-layer of 115 km is 20–30 km. The discovered properties of currents during the formation of the Harang discontinuity should be taken into account in the construction of an equivalent ionospheric current system that determines the dynamics of substorm development. © Pleiades Publishing, Ltd. 2022. ISSN 0016-7932, Geomagnetism and Aeronomy, 2022, Vol. 62, No. 5, pp. 563–572. © Pleiades Publishing, Ltd., 2022, corrected publication 2022. Russian Text © The Author(s), 2022, published in Geomagnetizm i Aeronomiya, 2022, Vol. 62, No. 5, pp. 607–616. |
abstract_unstemmed |
Abstract Cases of superposition of auroral electric jets in the auroral zone at the instances of development of the Harang discontinuity have been found and described using the data from ground-based magnetometers. It is shown that special conditions for the development of elements of current systems form in the region of the Harang discontinuity, and those can be taken into account only with a special method of separating the types of variations according to morphological features. With an accuracy of determining the position of electric jets from ground data within tens of kilometers, the convergence of electric jets at the altitude of the ionospheric E-layer of 115 km is 20–30 km. The discovered properties of currents during the formation of the Harang discontinuity should be taken into account in the construction of an equivalent ionospheric current system that determines the dynamics of substorm development. © Pleiades Publishing, Ltd. 2022. ISSN 0016-7932, Geomagnetism and Aeronomy, 2022, Vol. 62, No. 5, pp. 563–572. © Pleiades Publishing, Ltd., 2022, corrected publication 2022. Russian Text © The Author(s), 2022, published in Geomagnetizm i Aeronomiya, 2022, Vol. 62, No. 5, pp. 607–616. |
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The Superposition of Auroral Currents in the Region of the Harang Discontinuity |
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ISSN 0016-7932, Geomagnetism and Aeronomy, 2022, Vol. 62, No. 5, pp. 563–572. © Pleiades Publishing, Ltd., 2022, corrected publication 2022. Russian Text © The Author(s), 2022, published in Geomagnetizm i Aeronomiya, 2022, Vol. 62, No. 5, pp. 607–616.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Cases of superposition of auroral electric jets in the auroral zone at the instances of development of the Harang discontinuity have been found and described using the data from ground-based magnetometers. It is shown that special conditions for the development of elements of current systems form in the region of the Harang discontinuity, and those can be taken into account only with a special method of separating the types of variations according to morphological features. With an accuracy of determining the position of electric jets from ground data within tens of kilometers, the convergence of electric jets at the altitude of the ionospheric E-layer of 115 km is 20–30 km. The discovered properties of currents during the formation of the Harang discontinuity should be taken into account in the construction of an equivalent ionospheric current system that determines the dynamics of substorm development.</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Kanonidi, K. Kh.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Petrov, V. G.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Geomagnetism and aeronomy</subfield><subfield code="d">Moscow : MAIK Nauka/Interperiodica Publ., 1996</subfield><subfield code="g">62(2022), 5 vom: 28. Sept., Seite 563-572</subfield><subfield code="w">(DE-627)342320920</subfield><subfield code="w">(DE-600)2071667-9</subfield><subfield code="x">1555-645X</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:62</subfield><subfield code="g">year:2022</subfield><subfield code="g">number:5</subfield><subfield code="g">day:28</subfield><subfield code="g">month:09</subfield><subfield code="g">pages:563-572</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://dx.doi.org/10.1134/S0016793222050176</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_SPRINGER</subfield></datafield><datafield tag="912" 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