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In atmospheric science, geostrophic flow (/ˌdʒiːəˈstrɒfɪk, ˌdʒiːoʊ-, -ˈstroʊ-/) 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…
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geostrophic wind pressure flow air balance force gradient friction approximation atmospheric coriolis height would result actual isobars also used called
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| friction from the ground | instance of | The true wind almost always differs from the geostrophic wind due to other forces | 0.80 | text |
| Geostrophic wind | related to External links | Geostrophic | 0.60 | section |
| Geostrophic wind | related to Geostrophic currents | Flow | 0.60 | section |
| Geostrophic wind | related to Geostrophic currents | Just | 0.60 | section |
| Geostrophic wind | related to Geostrophic currents | Satellite | 0.60 | section |
| Geostrophic wind | related to Limitations of the geostrophic approximation | The | 0.60 | section |
| Geostrophic wind | related to Limitations of the geostrophic approximation | Friction | 0.60 | section |
| Geostrophic wind | related to Limitations of the geostrophic approximation | Coriolis | 0.60 | section |
| Geostrophic wind | related to Limitations of the geostrophic approximation | As | 0.60 | section |
| Geostrophic wind | related to Limitations of the geostrophic approximation | This | 0.60 | section |
| Geostrophic wind | related to Limitations of the geostrophic approximation | Although | 0.60 | section |
| Geostrophic wind | related to Limitations of the geostrophic approximation | Quasigeostrophic | 0.60 | section |
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