Linganisha mbinu
Pitia mbinu ulizochagua bega kwa bega; safu zinazotofautiana zinaangaziwa.
| Uchanganuzi wa Kina wa Kawaida× | Muundo wa WRF× | |
|---|---|---|
| Nyanja | Meteorolojia | Meteorolojia |
| Familia | Process / pipeline | Process / pipeline |
| Mwaka wa asili≠ | 1992 | 2000 |
| Mwanzilishi≠ | Bretherton, Wallace | Skamarock and Klemp |
| Aina≠ | Covariance decomposition method | Atmospheric simulation system |
| Chanzo asilia≠ | 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 ↗ |
| Majina mbadala | MCA, Singular value decomposition, SVD analysis, Covariance analysis | Weather Research and Forecasting, WRF, ARW, NMM |
| Zinazohusiana≠ | 2 | 4 |
| Muhtasari≠ | 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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