Lintner, Benjamin Richard - Department of Atmospheric and Oceanic Sciences, University of California at Los Angeles

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Lintner, Benjamin Richard - Department of Atmospheric and Oceanic Sciences, University of California at Los Angeles

Reorganization of Tropical Climate during El Nio: A Weak Temperature Gradient Approach
SUPPLEMENTARY INFORMATION1 Transport mechanisms for synoptic, seasonal and interannual SF63
Note that we have assumed all parameters are spatial constants (with H set to 0) and used the notation Mqc = Mqpqc and Mc = Ms -Mqc. The convective margin is defined as the location for which q(xc,yc) = qc. Two points worth mentioning are: (i) in the abse
Mechanisms of Remote Tropical Surface Warming during El Nio JOHN C. H. CHIANG AND BENJAMIN R. LINTNER
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Eastern margin variability of the South Pacific Convergence Zone Benjamin R. Lintner1
Adjustment of the Remote Tropical Climate to El Nio Conditions BENJAMIN R. LINTNER* AND JOHN C. H. CHIANG