| Display title | Earth:Atmospheric circulation |
| Default sort key | Atmospheric circulation |
| Page length (in bytes) | 21,653 |
| Namespace ID | 3028 |
| Namespace | Earth |
| Page ID | 886118 |
| 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>WikiG |
| Date of page creation | 11:15, 5 February 2024 |
| Latest editor | imported>WikiG |
| Date of latest edit | 11:15, 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. | Atmospheric circulation is the large-scale movement of air and together with ocean circulation is the means by which thermal energy is redistributed on the surface of the Earth. The Earth's atmospheric circulation varies from year to year, but the large-scale structure of its circulation remains fairly... |
