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| Vento Termico× | Equazione Omega Quasi-Geostrofica× | |
|---|---|---|
| Campo | Meteorologia | Meteorologia |
| Famiglia | Process / pipeline | Process / pipeline |
| Anno di origine≠ | 1920s | 1970s |
| Ideatore≠ | Jacobbian insights from geostrophic flow | Trenberth, Omaga |
| Tipo≠ | Wind-temperature relationship | Diagnostic equation for vertical motion |
| Fonte seminale | Holton, J. R. (2004). An Introduction to Dynamic Meteorology (4th ed.). Academic Press. link ↗ | Holton, J. R. (2004). An Introduction to Dynamic Meteorology (4th ed.). Academic Press. link ↗ |
| Alias | Thermal wind, Vertical wind shear, Barotropic | QG omega equation, Quasi-geostrophic dynamics, Vertical motion prediction |
| Correlati | 3 | 3 |
| Sintesi≠ | The thermal wind relationship is a fundamental meteorological principle that links vertical wind shear to horizontal temperature gradients. It states that wind speed increases with height in the direction of warming—a direct consequence of hydrostatic and geostrophic balance combined with the ideal gas law. | The quasi-geostrophic (QG) omega equation is a fundamental diagnostic equation in synoptic meteorology that relates vertical motion (omega = dP/dt) to horizontal temperature and vorticity fields. It predicts where air rises and sinks based on the geostrophic flow structure without explicitly solving for vertical velocity. |
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