Variability of the Oceanic Mixed Layer 1960-2004
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Figure 12 Annually averaged climate variability in the equatorial Pacific. MLD, SST, and zonal wind anomaly (a) in the NIÑO3 box (210o-270oE, 5oS-5oN), (b) in a western Pacific box (135o-180oE, 5oS-5oN). (c) Lag correlation among NIÑO3 and western Pacific variables. Positive lags imply that the second variable leads the first. 
Figure 13 Variability in the Indian Ocean sector during the season of the mature phase of ENSO SSTs (DJF). (a) Spatial pattern of leading Empirical Orthogonal Eigenfunction of MLD (explains 9.5% of variance). Time regression of winds onto the EOF time series is overlain. (b) Corresponding principal component time series (solid). The SOI index for DJF is overlain. Correlation of these time series is 0.75. 
Figure 14 Leading Empirical Orthogonal Eigenfunction of MLD variability in the Indian Ocean sector during the season of the Southwest Monsoon (JJA). This EOF explains 8.5% of MLD variance. Time regression of winds onto the EOF time series is overlain. (b) Corresponding principal component time series. Directory: ~senya -> HTML HTML -> Haline hurricane wake in the Amazon/Orinoco plume: aquarius/sacd and smos observations HTML -> Haline hurricane wake in the Amazon/Orinoco plume: aquarius/sacd and smos observations HTML -> Observed subseasonal variability of oceanic barrier and compensated layers HTML -> Seasonal mixed layer heat budget of the tropical Atlantic Ocean HTML -> Near surface westerly wind jet in the Atlantic itcz HTML -> Surface drifter pathways originating in the equatorial Atlantic cold tongue HTML -> P. O. Box 3000 Boulder, co, 80307-3000 HTML -> Tropical Atlantic Oceanic Variability in the ccsm4 Ernesto Muñoz HTML -> Tropical Atlantic Biases in ccsm4 HTML -> Intertropical Convergence Zone in the South Atlantic and the equatorial cold tongue Download 0.7 Mb. Share with your friends:
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