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| Gió địa chuyển× | Mô hình WRF× | |
|---|---|---|
| Lĩnh vực | Khí tượng học | Khí tượng học |
| Họ | Process / pipeline | Process / pipeline |
| Năm ra đời≠ | 1857 | 2000 |
| Người khởi xướng≠ | Buys Ballot, Coriolis | Skamarock and Klemp |
| Loại≠ | Wind balance principle | Atmospheric simulation system |
| Công trình gốc≠ | 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 ↗ |
| Tên gọi khác≠ | Geostrophic wind, Geostrophic balance, Geostrophic approximation | Weather Research and Forecasting, WRF, ARW, NMM |
| Liên quan≠ | 3 | 4 |
| Tóm tắt≠ | 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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