On the ionic and electrostatic nature of the activation of linear cloud anomalies over seismically active zones
One-dimensional model of medium self-coordinated electrostatic field (SF) of lower atmosphere (0-30 km) has been obtained. The model has been presented by Poisson equation for self-coordinated field of electrons within dense gas. Exact solution has been found in approximation of constant coefficient...
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| Дата: | 2012 |
|---|---|
| Автори: | , |
| Формат: | Стаття |
| Мова: | Російська |
| Опубліковано: |
S. Subbotin Institute of Geophysics of the NAS of Ukraine
2012
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| Онлайн доступ: | https://journals.uran.ua/geofizicheskiy/article/view/116652 |
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| Назва журналу: | Geofizicheskiy Zhurnal |
Репозитарії
Geofizicheskiy Zhurnal| _version_ | 1856543270117572608 |
|---|---|
| author | Belyi, T. A. Zelenin, Yu. A. |
| author_facet | Belyi, T. A. Zelenin, Yu. A. |
| author_sort | Belyi, T. A. |
| baseUrl_str | |
| collection | OJS |
| datestamp_date | 2020-10-07T12:21:30Z |
| description | One-dimensional model of medium self-coordinated electrostatic field (SF) of lower atmosphere (0-30 km) has been obtained. The model has been presented by Poisson equation for self-coordinated field of electrons within dense gas. Exact solution has been found in approximation of constant coefficients corresponding to integrability of classical Morse oscillator. The solution is parametrized by the values of field energy in the unit of volume. Basic functions of linear approximation, in contrast to homogenous approximation of Debye - Huckel, are Eyre functions (Ai, Bi) which show oscillation hyperpolarizing ability of electrons distribution in the gravity field. Within the limits of this model injection-polarization mechanism has been proposed of stabilization of linear cloudy anomalies (LCA) by the waves of charge density in heterogeneous (overabundant) electronic-ionic subsystem of the atmosphere in vertical stratified field. Calculations demonstrated that disturbance of surface electrostatic field from seismically active faults or edges of earthquakes sources is enough for polarization of charged subsystem of water steam of LCA. |
| first_indexed | 2025-07-17T11:07:20Z |
| format | Article |
| id | journalsuranua-geofizicheskiy-article-116652 |
| institution | Geofizicheskiy Zhurnal |
| language | Russian |
| last_indexed | 2025-07-17T11:07:20Z |
| publishDate | 2012 |
| publisher | S. Subbotin Institute of Geophysics of the NAS of Ukraine |
| record_format | ojs |
| spelling | journalsuranua-geofizicheskiy-article-1166522020-10-07T12:21:30Z On the ionic and electrostatic nature of the activation of linear cloud anomalies over seismically active zones Belyi, T. A. Zelenin, Yu. A. One-dimensional model of medium self-coordinated electrostatic field (SF) of lower atmosphere (0-30 km) has been obtained. The model has been presented by Poisson equation for self-coordinated field of electrons within dense gas. Exact solution has been found in approximation of constant coefficients corresponding to integrability of classical Morse oscillator. The solution is parametrized by the values of field energy in the unit of volume. Basic functions of linear approximation, in contrast to homogenous approximation of Debye - Huckel, are Eyre functions (Ai, Bi) which show oscillation hyperpolarizing ability of electrons distribution in the gravity field. Within the limits of this model injection-polarization mechanism has been proposed of stabilization of linear cloudy anomalies (LCA) by the waves of charge density in heterogeneous (overabundant) electronic-ionic subsystem of the atmosphere in vertical stratified field. Calculations demonstrated that disturbance of surface electrostatic field from seismically active faults or edges of earthquakes sources is enough for polarization of charged subsystem of water steam of LCA. S. Subbotin Institute of Geophysics of the NAS of Ukraine 2012-06-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/116652 10.24028/gzh.0203-3100.v34i3.2012.116652 Geofizicheskiy Zhurnal; Vol. 34 No. 3 (2012); 145-154 Геофизический журнал; Том 34 № 3 (2012); 145-154 Геофізичний журнал; Том 34 № 3 (2012); 145-154 2524-1052 0203-3100 ru https://journals.uran.ua/geofizicheskiy/article/view/116652/110689 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0 |
| spellingShingle | Belyi, T. A. Zelenin, Yu. A. On the ionic and electrostatic nature of the activation of linear cloud anomalies over seismically active zones |
| title | On the ionic and electrostatic nature of the activation of linear cloud anomalies over seismically active zones |
| title_full | On the ionic and electrostatic nature of the activation of linear cloud anomalies over seismically active zones |
| title_fullStr | On the ionic and electrostatic nature of the activation of linear cloud anomalies over seismically active zones |
| title_full_unstemmed | On the ionic and electrostatic nature of the activation of linear cloud anomalies over seismically active zones |
| title_short | On the ionic and electrostatic nature of the activation of linear cloud anomalies over seismically active zones |
| title_sort | on the ionic and electrostatic nature of the activation of linear cloud anomalies over seismically active zones |
| url | https://journals.uran.ua/geofizicheskiy/article/view/116652 |
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