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| Phân tích hiệp phương sai cực đại× | Mô hình WRF× | |
|---|---|---|
| Lĩnh vực | Khí tượng học | Khí tượng học |
| Họ | Process / pipeline | Process / pipeline |
| Năm ra đời≠ | 1992 | 2000 |
| Người khởi xướng≠ | Bretherton, Wallace | Skamarock and Klemp |
| Loại≠ | Covariance decomposition method | Atmospheric simulation system |
| Công trình gốc≠ | Bretherton, C. S., Widmann, M., Dymnikov, V. P., Wallace, J. M., & Blade, I. (1992). The effective number of spatial degrees of freedom of a time-varying field. Journal of the Atmospheric Sciences, 49(11), 1063-1083. 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 | MCA, Singular value decomposition, SVD analysis, Covariance analysis | Weather Research and Forecasting, WRF, ARW, NMM |
| Liên quan≠ | 2 | 4 |
| Tóm tắt≠ | Maximum covariance analysis (MCA) is a statistical technique that identifies coupled patterns of variability between two spatially distributed fields (e.g., sea surface temperature and precipitation). Unlike EOF analysis which focuses on variance in a single field, MCA identifies spatial patterns that are maximally correlated between two different fields. | 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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