VARIATIONS IN THE ELECTRIC FIELD AND TURBULENCE IN THE SURFACE ATMOSPHERIC LAYER

dc.contributor.author	Koprov B.M.
dc.contributor.author	Koprov V.M.
dc.contributor.author	Anisimov S.V.
dc.date.accessioned	2024-10-23T07:16:05Z
dc.date.available	2024-10-23T07:16:05Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13512635
dc.identifier.citation	Doklady Earth Sciences, 2006, 407, 2, 312-316
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46175
dc.description.abstract	An experiment was carried out on the synchronous recording, in cloudless summer conditions in the middle region of Russia, of variations in the vertical component of electric field intensity E'; temperature; and the wind velocity components T', U', V', and W' . It was found that the correlation coefficient is positive between W' and E' and negative between U' and E'. If the temperature gradient sign changes to the opposite one, the correlation signs are retained, while the sign of the T' – E' correlation changes to the opposite one.
dc.title	VARIATIONS IN THE ELECTRIC FIELD AND TURBULENCE IN THE SURFACE ATMOSPHERIC LAYER
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X0602036X

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