MECHANISM OF THE APPEARANCE OF A LARGE-SCALE VORTEX IN THE TROPOSPHERE ABOVE A NONUNIFORMLY HEATED SURFACE

dc.contributor.author	Belotserkovskii O.M.
dc.contributor.author	Oparin A.M.
dc.contributor.author	Mingalev I.V.
dc.contributor.author	Mingalev V.S.
dc.contributor.author	Mingalev O.V.
dc.date.accessioned	2024-11-09T08:38:29Z
dc.date.available	2024-11-09T08:38:29Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13531146
dc.identifier.citation	Doklady Earth Sciences, 2006, 411, 8, 1284-1288
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46472
dc.description.abstract	This paper is dedicated to a numerical modeling study of the formation mechanisms of a large-scale vortex over a warm water band on the ocean surface. For this purpose, we developed a 3D model of the atmospheric circulation in a domain, which is a part of spherical layer over a limited region of the Earth’s surface (altitude 15 km, longitude and latitude 12°). This model takes into account heating/cooling of the air due to absorption/emission of infrared radiation, as well as due to phase transitions of water vapor to microdrops of water and ice particles, which play an important role.
dc.title	MECHANISM OF THE APPEARANCE OF A LARGE-SCALE VORTEX IN THE TROPOSPHERE ABOVE A NONUNIFORMLY HEATED SURFACE
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06080277

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