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Applications of a Multiple Linear Regression Model to the Analysis of Relationships between Eastward- and Westward-Moving Intraseasonal Modes.

Authors :
Roundy, Paul E.
Frank, William M.
Source :
Journal of the Atmospheric Sciences. 12/15/2004, Vol. 61 Issue 24, p3041-3048. 8p.
Publication Year :
2004

Abstract

Multiple linear regression models with nonlinear power terms may be applied to find relationships between interacting wave modes that may be characterized by different frequencies. Such regression techniques have been explored in other disciplines, but they have not been used in the analysis of atmospheric circulations. In this study, such a model is developed to predict anomalies of westward-moving intraseasonal precipitable water by utilizing the first through fourth powers of a time series of outgoing longwave radiation that is filtered for eastward propagation and for the temporal and spatial scales of the tropical intraseasonal oscillations. An independent and simpler compositing method is applied to show that the results of this multiple linear regression model provide a better description of the actual relationships between eastward- and westward-moving intraseasonal modes than a regression model that includes only the linear predictor. A statistical significance test is applied to the coefficients of the multiple linear regression model, and they are found to be significant over broad regions of the Tropics. Correlations between the predictors are shown to not significantly influence results for this case. Results show that this regression model reveals physical relationships between eastward- and westward-moving intraseasonal modes. The physical interpretation of these regression relationships is given in a companion paper. [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
00224928
Volume :
61
Issue :
24
Database :
Academic Search Index
Journal :
Journal of the Atmospheric Sciences
Publication Type :
Academic Journal
Accession number :
15456218
Full Text :
https://doi.org/10.1175/JAS-3349.1