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Maximale Kovarianzanalyse×Empirische Orthogonale Telekonnektion×
FachgebietMeteorologieMeteorologie
FamilieProcess / pipelineProcess / pipeline
Entstehungsjahr19921956
UrheberBretherton, WallaceLorenz, Wallace
TypCovariance decomposition methodData analysis and pattern identification
Wegweisende QuelleBretherton, 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 ↗
AliasnamenMCA, Singular value decomposition, SVD analysis, Covariance analysisEOF analysis, Empirical orthogonal function, Teleconnection patterns, PCA meteorology
Verwandt22
ZusammenfassungMaximum 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.
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ScholarGateMethoden vergleichen: Maximum Covariance Analysis · Empirical Orthogonal Teleconnection. Abgerufen am 2026-06-19 von https://scholargate.app/de/compare