Fig. 3: Comparisons between Ekman layer depth and depth of the 26 °C isotherm (D26). | Nature Communications

Fig. 3: Comparisons between Ekman layer depth and depth of the 26 °C isotherm (D26).

From: Crucial role of subsurface ocean variability in tropical cyclone genesis

Fig. 3

a, Coloured thick lines are the Ekman layer depths estimated with various empirical formulas (see Methods). Each black dot represents the D26 under a pre-genesis tropical cyclone (TC) case. The black line is the mean D26 of all pre-genesis TCs. b Ratios of the estimated Ekman layer depth to the D26 under pre-genesis TCs. The shaded areas represent the 95% confidence intervals.

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