Ntxw wrote:DorkyMcDorkface wrote:Ntxw wrote:The standing wave is definitely different than the last 4-5 seasons. So we shouldn't expect the same players for better or for worse. MC-> WPAC standing wave is moody for the Atlantic, MC being good for deep tropics later on but as it shifts slightly east, it can take away from Africa.
I think it's a combination of the very strong background Niña forcing combined with the -IOD. 2020 had a +IOD combined with a developing Niña which essentially supercharged the WAM (albeit for the worse if anything because it resulted in a messy MDR at times filled with sloppy monsoon troughs, very large TWs and waves crashing into each other because trades were next to nonexistent). Last year I believe the IOD was more neutral-ish so the effect was lesser to an extent - I think the Atlantic Niño might have played more of a role in that regard.
If you compare this year to the composite of June/July for recent La Niña years with -IOD you'll see that this year isn't too dissimilar, with the bulk of the rising cell over the SE IO/MC. In other words I feel we are seeing something closer to what you'd expect for a typical Niña, as -ENSO is usually paired with -IOD which causes that ascent in that region.
https://i.ibb.co/ggWZ48G/jgdjj-U6f1x.png
https://i.ibb.co/7vH6SLX/compday-RUUvi-G4b83.gif
I ran some similar narr and along with your graphics there are subtle differences in the Pacific west to east, not a totally exact match. It's a huge basin so even a 50/50 difference is significant, imo. If the the rising motion has to split between MC and WPAC it'll be a lot of back and forth between favorable vs unfavorable.
Yea this is great discussion. Come ASO, we will find out how much the IOD forced eastern standing wave affects the season. As Cat5 said there is definitely a possibility that we get more compact waves rather than large monsoon troughs which could aid TCG.