方法对比
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| 地转风× | WRF模型× | |
|---|---|---|
| 领域 | 气象学 | 气象学 |
| 方法族 | Process / pipeline | Process / pipeline |
| 起源年份≠ | 1857 | 2000 |
| 提出者≠ | Buys Ballot, Coriolis | Skamarock and Klemp |
| 类型≠ | Wind balance principle | Atmospheric simulation system |
| 开创性文献≠ | 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 ↗ |
| 别名≠ | Geostrophic wind, Geostrophic balance, Geostrophic approximation | Weather Research and Forecasting, WRF, ARW, NMM |
| 相关≠ | 3 | 4 |
| 摘要≠ | Geostrophic wind balance is a fundamental concept in meteorology that describes the balance between the pressure gradient force and the Coriolis force in large-scale atmospheric flow. When this balance is achieved, wind blows parallel to isobars without acceleration—a condition observed in the free atmosphere away from the equator and surface boundary layer. | 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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