02/28/2022, 1:07 pm EST
During the past 2-3 weeks the convective phase of the Madden Julian oscillation (MJO) has dominated the eastern Indian Ocean/West Indonesia tropics. The general rising air induced by convection along this stretch is replaced by increasing easterly trade winds arriving from the central/eastern equatorial Pacific. The trade wind increase in the central/eastern equatorial Pacific has caused up-welling of cool subsurface water to cause La Nina to gain some strength.