Fig. 3: Seasonal evolution of SST patterns in association with IOD and ENSO. | npj Climate and Atmospheric Science

Fig. 3: Seasonal evolution of SST patterns in association with IOD and ENSO.

From: Indian Ocean Dipole and ENSO’s mechanistic importance in modulating the ensuing-summer precipitation over Eastern China

Fig. 3

Composite seasonal evolution of SST anomalies (contours, °C) from autumn to the ensuing summer based on the years when a–d only IOD occurs, e–h only El Niño occurs, and i–l IOD and ENSO occur together. Dotted areas have statistical significance at the 95% confidence level.

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