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...
Sábháilte in:
| Príomhchruthaitheoirí: | , , , , , |
|---|---|
| Formáid: | Статья |
| Teanga: | English |
| Foilsithe / Cruthaithe: |
MDPI AG
2018
|
| Ábhair: | |
| Rochtain ar líne: | https://dspace.ncfu.ru/handle/20.500.12258/3182 |
| Clibeanna: |
Cuir clib leis
Níl clibeanna ann, Bí ar an gcéad duine le clib a chur leis an taifead seo!
|