Phases of the isobaric surface shapes in the geostrophic state of the atmosphere and connection to the polar vortices
This paper presents a theoretical study of the disturbed isobaric surface shape in the geostrophic state of the atmosphere. It has been shown that, depending on the overheat sign at the equator, the isobaric surface has the shape of an oblate or prolate geoid. If the geostrophic wind velocity is non...
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| Autors principals: | , , , , , |
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| Format: | Статья |
| Idioma: | English |
| Publicat: |
MDPI AG
2018
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| Matèries: | |
| Accés en línia: | https://dspace.ncfu.ru/handle/20.500.12258/3182 |
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