Penetration of an electrostatic field from the lithosphere into the ionosphere and its effect on the D-region before earthquakes
The penetration of an electrostatic field, from a source located in the lithosphere into the ionosphere is investigated. The electrostatic problem is solved numerically for a medium with an inhomogeneous anisotropic conductivity coupled to an “effective upper boundary condition”. The results show th...
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| Veröffentlicht in: | Journal of atmospheric and solar-terrestrial physics 2003-03, Vol.65 (4), p.391-407 |
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| container_end_page | 407 |
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| container_issue | 4 |
| container_start_page | 391 |
| container_title | Journal of atmospheric and solar-terrestrial physics |
| container_volume | 65 |
| creator | Grimalsky, V.V. Hayakawa, M. Ivchenko, V.N. Rapoport, Yu.G. Zadorozhnii, V.I. |
| description | The penetration of an electrostatic field, from a source located in the lithosphere into the ionosphere is investigated. The electrostatic problem is solved numerically for a medium with an inhomogeneous anisotropic conductivity coupled to an “effective upper boundary condition”. The results show that the electric field in the ionosphere D-layer can effectively change the parameters of the lower ionosphere. The kinetics in the D-region are considered along with calculations of the atmospheric conductivity at an altitude of
60
km
. It is concluded that (i) the atmospheric conductivity at
60
km
can change by 30–70% as a result of electrostatic perturbations, created before the onset of earthquakes, and (ii) the penetration of an electrostatic field from the lithosphere into the ionosphere above
60
km
is much better at night-time than during the day. |
| doi_str_mv | 10.1016/S1364-6826(02)00341-3 |
| format | Article |
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60
km
. It is concluded that (i) the atmospheric conductivity at
60
km
can change by 30–70% as a result of electrostatic perturbations, created before the onset of earthquakes, and (ii) the penetration of an electrostatic field from the lithosphere into the ionosphere above
60
km
is much better at night-time than during the day.</description><identifier>ISSN: 1364-6826</identifier><identifier>EISSN: 1879-1824</identifier><identifier>DOI: 10.1016/S1364-6826(02)00341-3</identifier><language>eng</language><publisher>Elsevier Ltd</publisher><subject>Atmosphere ; Earth-ionosphere waveguide ; Earthquake ; Electromagnetic waves ; Electrostatic field ; Photochemistry dynamics ; Upper boundary condition</subject><ispartof>Journal of atmospheric and solar-terrestrial physics, 2003-03, Vol.65 (4), p.391-407</ispartof><rights>2003 Elsevier Science Ltd</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a473t-18d5f09d1ab806773d9fd71f87b9dea30ee1526d60615d87216a9aa0e346c43a3</citedby><cites>FETCH-LOGICAL-a473t-18d5f09d1ab806773d9fd71f87b9dea30ee1526d60615d87216a9aa0e346c43a3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.sciencedirect.com/science/article/pii/S1364682602003413$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,776,780,3537,27901,27902,65306</link.rule.ids></links><search><creatorcontrib>Grimalsky, V.V.</creatorcontrib><creatorcontrib>Hayakawa, M.</creatorcontrib><creatorcontrib>Ivchenko, V.N.</creatorcontrib><creatorcontrib>Rapoport, Yu.G.</creatorcontrib><creatorcontrib>Zadorozhnii, V.I.</creatorcontrib><title>Penetration of an electrostatic field from the lithosphere into the ionosphere and its effect on the D-region before earthquakes</title><title>Journal of atmospheric and solar-terrestrial physics</title><description>The penetration of an electrostatic field, from a source located in the lithosphere into the ionosphere is investigated. The electrostatic problem is solved numerically for a medium with an inhomogeneous anisotropic conductivity coupled to an “effective upper boundary condition”. The results show that the electric field in the ionosphere D-layer can effectively change the parameters of the lower ionosphere. The kinetics in the D-region are considered along with calculations of the atmospheric conductivity at an altitude of
60
km
. It is concluded that (i) the atmospheric conductivity at
60
km
can change by 30–70% as a result of electrostatic perturbations, created before the onset of earthquakes, and (ii) the penetration of an electrostatic field from the lithosphere into the ionosphere above
60
km
is much better at night-time than during the day.</description><subject>Atmosphere</subject><subject>Earth-ionosphere waveguide</subject><subject>Earthquake</subject><subject>Electromagnetic waves</subject><subject>Electrostatic field</subject><subject>Photochemistry dynamics</subject><subject>Upper boundary condition</subject><issn>1364-6826</issn><issn>1879-1824</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2003</creationdate><recordtype>article</recordtype><recordid>eNqFkUtLAzEUhQdRsFZ_gpCV6GI0r0kyKxHfUFBQ1yGd3NjodFKTVHDnTzdtde0ql8N3TrjnVtUhwacEE3H2RJjgtVBUHGN6gjHjpGZb1Ygo2dZEUb5d5j9kt9pL6Q1jLKkSo-r7EQbI0WQfBhQcMgOCHrocQ8pF7JDz0FvkYpijPAPU-zwLaTGDCMgPOazF4v3TzGCRzwmBcyUFldAVcFVHeF39MAUXCgUm5tnH0rxD2q92nOkTHPy-4-rl5vr58q6ePNzeX15MasMly2UN2zjcWmKmCgspmW2dlcQpOW0tGIYBSEOFFViQxipJiTCtMRgYFx1nho2ro03uIoaPJaSs5z510PdmgLBMmsqWU4abf0GiVMMazgvYbMCulJUiOL2Ifm7ilyZYrw6j14fRq9Y1pnp9GM2K73zjg7Lup4eoU-dh6MD6WDrTNvh_En4ArWqW-w</recordid><startdate>20030301</startdate><enddate>20030301</enddate><creator>Grimalsky, V.V.</creator><creator>Hayakawa, M.</creator><creator>Ivchenko, V.N.</creator><creator>Rapoport, Yu.G.</creator><creator>Zadorozhnii, V.I.</creator><general>Elsevier Ltd</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>KL.</scope><scope>8FD</scope><scope>H8D</scope><scope>L7M</scope></search><sort><creationdate>20030301</creationdate><title>Penetration of an electrostatic field from the lithosphere into the ionosphere and its effect on the D-region before earthquakes</title><author>Grimalsky, V.V. ; Hayakawa, M. ; Ivchenko, V.N. ; Rapoport, Yu.G. ; Zadorozhnii, V.I.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a473t-18d5f09d1ab806773d9fd71f87b9dea30ee1526d60615d87216a9aa0e346c43a3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2003</creationdate><topic>Atmosphere</topic><topic>Earth-ionosphere waveguide</topic><topic>Earthquake</topic><topic>Electromagnetic waves</topic><topic>Electrostatic field</topic><topic>Photochemistry dynamics</topic><topic>Upper boundary condition</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Grimalsky, V.V.</creatorcontrib><creatorcontrib>Hayakawa, M.</creatorcontrib><creatorcontrib>Ivchenko, V.N.</creatorcontrib><creatorcontrib>Rapoport, Yu.G.</creatorcontrib><creatorcontrib>Zadorozhnii, V.I.</creatorcontrib><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Technology Research Database</collection><collection>Aerospace Database</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Journal of atmospheric and solar-terrestrial physics</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Grimalsky, V.V.</au><au>Hayakawa, M.</au><au>Ivchenko, V.N.</au><au>Rapoport, Yu.G.</au><au>Zadorozhnii, V.I.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Penetration of an electrostatic field from the lithosphere into the ionosphere and its effect on the D-region before earthquakes</atitle><jtitle>Journal of atmospheric and solar-terrestrial physics</jtitle><date>2003-03-01</date><risdate>2003</risdate><volume>65</volume><issue>4</issue><spage>391</spage><epage>407</epage><pages>391-407</pages><issn>1364-6826</issn><eissn>1879-1824</eissn><abstract>The penetration of an electrostatic field, from a source located in the lithosphere into the ionosphere is investigated. The electrostatic problem is solved numerically for a medium with an inhomogeneous anisotropic conductivity coupled to an “effective upper boundary condition”. The results show that the electric field in the ionosphere D-layer can effectively change the parameters of the lower ionosphere. The kinetics in the D-region are considered along with calculations of the atmospheric conductivity at an altitude of
60
km
. It is concluded that (i) the atmospheric conductivity at
60
km
can change by 30–70% as a result of electrostatic perturbations, created before the onset of earthquakes, and (ii) the penetration of an electrostatic field from the lithosphere into the ionosphere above
60
km
is much better at night-time than during the day.</abstract><pub>Elsevier Ltd</pub><doi>10.1016/S1364-6826(02)00341-3</doi><tpages>17</tpages></addata></record> |
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| identifier | ISSN: 1364-6826 |
| ispartof | Journal of atmospheric and solar-terrestrial physics, 2003-03, Vol.65 (4), p.391-407 |
| issn | 1364-6826 1879-1824 |
| language | eng |
| recordid | cdi_proquest_miscellaneous_27942305 |
| source | Elsevier ScienceDirect Journals |
| subjects | Atmosphere Earth-ionosphere waveguide Earthquake Electromagnetic waves Electrostatic field Photochemistry dynamics Upper boundary condition |
| title | Penetration of an electrostatic field from the lithosphere into the ionosphere and its effect on the D-region before earthquakes |
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