ozonepete wrote:
Really good points. I guess my biggest problem with the whole thing is that merges are very rare for two systems that are this distinct. 99% of the time one dies out or is absorbed into the other rather than a "merge." Having said that, your point about the surface west winds is important and I admit I forgot about that. Still, the western one could just as easily start dying down as the eastern one works down to the surface. That's why I said I'm really hoping that RECON is getting all of the data. This could be a huge advancement for our understanding of the physics.
Its a really complex issue, but I think Aric is along the right lines when it comes to this system, and when it comes to formative stages of a system, I really pay attention to his thoughts, probably the best non-pro metin the formative stages.
As Aric said it'll be more of a stacking, thats why i said earlier to expect to behave in a similar way to a sheared system and expect the convection and MLC to rapidly transfer westwards whilst the LLC sorta gets dragged NNE from the western area and they'll merge something like that.
Its something you sometimes see in the W.Caribbean when you have a monsoonal gyre there, but its pretty uncommon in the Atlantic, at least to this extreme.
Ps, the fact the NHC mentioned it in thier update suggest they at least know its there.