| Display title | Physics:Quasi-geostrophic equations |
| Default sort key | Quasi-geostrophic equations |
| Page length (in bytes) | 11,828 |
| Namespace ID | 3020 |
| Namespace | Physics |
| Page ID | 422273 |
| Page content language | en - English |
| Page content model | wikitext |
| Indexing by robots | Allowed |
| Number of redirects to this page | 0 |
| Counted as a content page | Yes |
| HandWiki item ID | None |
| Edit | Allow all users (infinite) |
| Move | Allow all users (infinite) |
| Page creator | imported>S.Timg |
| Date of page creation | 19:46, 25 June 2023 |
| Latest editor | imported>S.Timg |
| Date of latest edit | 19:46, 25 June 2023 |
| Total number of edits | 1 |
| Recent number of edits (within past 90 days) | 0 |
| Recent number of distinct authors | 0 |
Description | Content |
Article description: (description)
This attribute controls the content of the description and og:description elements. | While geostrophic motion refers to the wind that would result from an exact balance between the Coriolis force and horizontal pressure-gradient forces, quasi-geostrophic (QG) motion refers to flows where the Coriolis force and pressure gradient forces are almost in balance, but with inertia also having... |
