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Télédéconnexion empirique orthogonale×Modèle WRF×
DomaineMétéorologieMétéorologie
FamilleProcess / pipelineProcess / pipeline
Année d'origine19562000
Auteur d'origineLorenz, WallaceSkamarock and Klemp
TypeData analysis and pattern identificationAtmospheric simulation system
Source fondatriceWallace, 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 ↗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 ↗
AliasEOF analysis, Empirical orthogonal function, Teleconnection patterns, PCA meteorologyWeather Research and Forecasting, WRF, ARW, NMM
Apparentées24
RésuméEmpirical 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.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.
ScholarGateJeu de données
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ScholarGateComparer des méthodes: Empirical Orthogonal Teleconnection · WRF Model. Consulté le 2026-06-19 sur https://scholargate.app/fr/compare