DC ELECTRIC FIELD AMPLIFICATION IN THE MID-LATITUDE IONOSPHERE OVER SEISMICALLY ACTIVE FAULTS

dc.contributor.author	Sorokin V.M.
dc.contributor.author	Yaschenko A.K.
dc.contributor.author	Chmyrev V.M.
dc.contributor.author	Hayakawa M.
dc.date.accessioned	2025-05-19T06:46:16Z
dc.date.available	2025-05-19T06:46:16Z
dc.date.issued	2006
dc.identifier	https://elibrary.ru/item.asp?id=13523715
dc.identifier.citation	Physics and Chemistry of the Earth, Parts A/B/C, 2006, 31, 4-9, 447-453
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/49312
dc.description.abstract	DC electric field in the ionosphere above seismically active regions can be formed in a process of external current insertion into the atmosphere–ionosphere electric circuit. This current arises as a result of convective upward transport of charged aerosols and their gravitational sedimentation. Aerosols are injected into the atmosphere by soil gases intensified in the zones of active faults. In general the horizontal distribution of injected aerosols in such zones is asymmetric. In this report we propose a method for computation of DC electric field generated in the ionosphere and the atmosphere by external electric current with arbitrary spatial distribution. Oblique magnetic field and the conjugate ionosphere effects are taken into consideration.
dc.title	DC ELECTRIC FIELD AMPLIFICATION IN THE MID-LATITUDE IONOSPHERE OVER SEISMICALLY ACTIVE FAULTS
dc.type	Статья

Files in this item

Name: Soro_06.pdf

Size: 580.4Kb

Format: PDF