| Display title | Physics:Equivalent potential temperature |
| Default sort key | Equivalent potential temperature |
| Page length (in bytes) | 11,883 |
| Namespace ID | 3020 |
| Namespace | Physics |
| Page ID | 630638 |
| 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>Raymond Straus |
| Date of page creation | 03:40, 1 May 2023 |
| Latest editor | imported>Raymond Straus |
| Date of latest edit | 03:40, 1 May 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. | Equivalent potential temperature, commonly referred to as theta-e $ \left(\theta _{e}\right) $, is a quantity that is conserved during changes to an air parcel's pressure (that is, during vertical motions in the atmosphere), even if water vapor condenses during that pressure change. It is therefore more... |
