Сравнение методов
Просматривайте выбранные методы рядом; строки с различиями подсвечены.
| Модель WRF× | Метод вихревых ковариаций× | |
|---|---|---|
| Область | Метеорология | Метеорология |
| Семейство | Process / pipeline | Process / pipeline |
| Год появления≠ | 2000 | 1951 |
| Автор метода≠ | Skamarock and Klemp | Swinbank |
| Тип≠ | Atmospheric simulation system | Micrometeorological flux measurement |
| Основополагающий источник≠ | 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 ↗ | Baldocchi, D. (2003). Assessing the eddy covariance technique for evaluating carbon dioxide fluxes of ecosystems: past, present and future. Global Change Biology, 9(4), 479-492. DOI ↗ |
| Другие названия | Weather Research and Forecasting, WRF, ARW, NMM | Eddy covariance, EC flux, Eddy correlation, Direct flux measurement |
| Связанные≠ | 4 | 3 |
| Сводка≠ | 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. | The eddy covariance method is a direct, micrometeorological technique that measures turbulent fluxes of momentum, heat, water vapor, and CO2 by computing the covariance between high-frequency fluctuations of wind velocity and scalar properties (temperature, humidity, concentration). It is the gold standard for measuring ecosystem-atmosphere exchanges and validating model parameterizations. |
| ScholarGateНабор данных ↗ |
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