Traduction et analyse de mots par intelligence artificielle ChatGPT
Sur cette page, vous pouvez obtenir une analyse détaillée d'un mot ou d'une phrase, réalisée à l'aide de la meilleure technologie d'intelligence artificielle à ce jour:
- comment le mot est utilisé
- fréquence d'utilisation
- il est utilisé plus souvent dans le discours oral ou écrit
- options de traduction de mots
- exemples d'utilisation (plusieurs phrases avec traduction)
- étymologie
quasi-geostrophic - traduction vers russe
общая лексика
квазигеострофический
общая лексика
геострофический ветер
![less dense]] than dark water, but more dense than air; the outwards pressure gradient is balanced by the 90 degrees-right-of-flow [[coriolis force]]. The structure will eventually dissipate due to friction and mixing of water properties.](https://commons.wikimedia.org/wiki/Special:FilePath/Geostrophic current 1 NT.PNG?width=200 "less dense]] than dark water, but more dense than air; the outwards pressure gradient is balanced by the 90 degrees-right-of-flow [[coriolis force]]. The structure will eventually dissipate due to friction and mixing of water properties.")
общая лексика
геострофический
Définition
Wikipédia
In atmospheric science, geostrophic flow () is the theoretical wind that would result from an exact balance between the Coriolis force and the pressure gradient force. This condition is called geostrophic equilibrium or geostrophic balance (also known as geostrophy). The geostrophic wind is directed parallel to isobars (lines of constant pressure at a given height). This balance seldom holds exactly in nature. The true wind almost always differs from the geostrophic wind due to other forces such as friction from the ground. Thus, the actual wind would equal the geostrophic wind only if there were no friction (e.g. above the atmospheric boundary layer) and the isobars were perfectly straight. Despite this, much of the atmosphere outside the tropics is close to geostrophic flow much of the time and it is a valuable first approximation. Geostrophic flow in air or water is a zero-frequency inertial wave.
