Fig. 3: Each role of IOD model parameters in decadal changes of IOD seasonal synchronization. | Communications Earth & Environment

Fig. 3: Each role of IOD model parameters in decadal changes of IOD seasonal synchronization.

From: Local feedback and ENSO govern decadal changes in variability and seasonal synchronization of the Indian Ocean Dipole

Fig. 3

Timeseries of DMI peak month obtained from the control experiment (black line), the constant φl experiment (red line), and the non-ENSO-forcing experiment (βmE(t); blue line). DMI peak month is determined over 30-year moving band by computing DMI variance for each calendar month for each band.

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