مقایسهٔ روشها
روشهای انتخابی خود را کنار هم مرور کنید؛ ردیفهای متفاوت برجسته شدهاند.
| تحلیل کوواریانس بیشینه× | تلاتصال متعامد تجريبي× | |
|---|---|---|
| حوزه | هواشناسی | هواشناسی |
| خانواده | Process / pipeline | Process / pipeline |
| سال پیدایش≠ | 1992 | 1956 |
| پدیدآور≠ | Bretherton, Wallace | Lorenz, Wallace |
| نوع≠ | Covariance decomposition method | Data analysis and pattern identification |
| منبع بنیادین≠ | 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 ↗ | Wallace, J. M., & Gutzler, D. S. (1981). Teleconnections in the geopotential height field during the Northern Hemisphere winter. Monthly Weather Review, 109(4), 784-812. DOI ↗ |
| نامهای دیگر | MCA, Singular value decomposition, SVD analysis, Covariance analysis | EOF analysis, Empirical orthogonal function, Teleconnection patterns, PCA meteorology |
| مرتبط | 2 | 2 |
| خلاصه≠ | 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. | Empirical orthogonal function (EOF) analysis is a statistical technique that identifies dominant spatial patterns and temporal variability in atmospheric or oceanic data. When applied to geographically distant locations, EOF analysis reveals teleconnection patterns—coherent patterns of variability that link weather systems across ocean basins and continents. |
| ScholarGateمجموعهداده ↗ |
|
|