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| Termisk vind× | WRF-modellen× | |
|---|---|---|
| Ämnesområde | Meteorologi | Meteorologi |
| Familj | Process / pipeline | Process / pipeline |
| Ursprungsår≠ | 1920s | 2000 |
| Upphovsperson≠ | Jacobbian insights from geostrophic flow | Skamarock and Klemp |
| Typ≠ | Wind-temperature relationship | Atmospheric simulation system |
| Ursprungskälla≠ | Holton, J. R. (2004). An Introduction to Dynamic Meteorology (4th ed.). Academic Press. link ↗ | Skamarock, W. C., Klemp, J. B., Dudhia, J., et al. (2008). A Description of the Advanced Research WRF Version 3. NCAR Technical Note NCAR/TN-475+STR. link ↗ |
| Alias≠ | Thermal wind, Vertical wind shear, Barotropic | Weather Research and Forecasting, WRF, ARW, NMM |
| Närliggande≠ | 3 | 4 |
| Sammanfattning≠ | 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 Weather Research and Forecasting (WRF) model is a mesoscale atmospheric simulation system used for weather forecasting, research, and climate applications. Developed cooperatively by NCAR, NOAA, and academic institutions, WRF became operational in 2004 and has become one of the most widely used atmospheric models worldwide. |
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