Fig. 4: Feedback of intraseasonal ITF transport on SST anomalies.
From: Indonesian Throughflow promoted eastward propagation of the Madden-Julian Oscillation
MJO-associated seawater temperature (shadings; °C) and ocean currents (vectors; cm s–1) averaged over the upper 20 m during boreal winter for (A) NESM_OITF, (B) differences between NESM_OITF_NISV and NESM_OITF. C, D Same as in (A, B) except for profiles of seawater temperature (shadings; °C) and ocean currents (vectors; cm s–1) along the transection (labeled as the purple lines and solid circles in (A)). Stippled points in (A) and (C) represent significant signals of seawater temperature at 95% confidence level.
