Fig. 6: Evolution of rainfall and horizontal wind anomalies.
From: Boosting effect of strong western pole of the Indian Ocean Dipole on the decay of El Niño events
Same as Fig. 2, but for rainfall anomalies (shading; units: mm day−1) and 850-hPa wind anomalies (vector; units: m s−1). Only the wind vectors with wind speed significantly exceeding the 95% confidence level are plotted.
