pcbjr
Member
changes!Thanks! To briefly summarize the main points from what I just said...
a) The QBO and Indonesian convective anomalies are coupled, and their interactions should be viewed as such instead of cause-and-effect
b) The observed higher than normal Indonesian convection is primarily due to ENSO, but the westerly QBO is significantly contributing.
c) The MJO initiated by the recent sudden stratospheric warming event may have jump started a series of processes and reactions that could cascade into completely disintegrating the above normal Indonesian convection that's been observed for most of this winter. We really need to closely monitor these changes going forward, because we're at the time of the year where ENSO is more responsive to higher frequency variability like the MJO. The point I'm really trying to get across here is that the MJO tends to have the most significant effect on ENSO at this time of the year, in and around the Northern Hemisphere's spring equinox.
Thanks, Webb!