| Display title | Physics:Convective mixing |
| Default sort key | Convective mixing |
| Page length (in bytes) | 1,899 |
| Namespace ID | 3020 |
| Namespace | Physics |
| Page ID | 428792 |
| 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>John Marlo |
| Date of page creation | 00:46, 8 February 2024 |
| Latest editor | imported>John Marlo |
| Date of latest edit | 00:46, 8 February 2024 |
| 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. | In fluid dynamics, convective mixing is the vertical transport of a fluid and its properties. In many important ocean and atmospheric phenomena, convection is driven by density differences in the fluid, e.g. the sinking of cold, dense water in polar regions of the world's oceans; and the rising of warm... |
