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