| Display title | Earth:Brewer–Dobson circulation |
| Default sort key | Brewer-Dobson circulation |
| Page length (in bytes) | 5,608 |
| Namespace ID | 3028 |
| Namespace | Earth |
| Page ID | 425795 |
| 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 |
| Page image |  |
| HandWiki item ID | None |
| Edit | Allow all users (infinite) |
| Move | Allow all users (infinite) |
| Page creator | imported>Unex |
| Date of page creation | 12:40, 5 February 2024 |
| Latest editor | imported>Unex |
| Date of latest edit | 12:40, 5 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. | Brewer–Dobson circulation refers to the global atmospheric circulation pattern of tropical tropospheric air rising into the stratosphere and then moving poleward as it descends. The basics of the circulation were first proposed by Gordon Dobson and Alan Brewer. The term "Brewer–Dobson circulation" was... |
