Порівняння методів
Переглядайте обрані методи поруч; рядки з відмінностями підсвічено.
| Рівняння квазі-геострофічної Омеги× | Модель WRF× | |
|---|---|---|
| Галузь | Метеорологія | Метеорологія |
| Родина | Process / pipeline | Process / pipeline |
| Рік появи≠ | 1970s | 2000 |
| Автор методу≠ | Trenberth, Omaga | Skamarock and Klemp |
| Тип≠ | Diagnostic equation for vertical motion | Atmospheric simulation system |
| Основоположне джерело≠ | 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 ↗ |
| Інші назви≠ | QG omega equation, Quasi-geostrophic dynamics, Vertical motion prediction | Weather Research and Forecasting, WRF, ARW, NMM |
| Пов'язані≠ | 3 | 4 |
| Підсумок≠ | 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. | 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. |
| ScholarGateНабір даних ↗ |
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