IMO, the circulation is WAY too broad and diffuse, and its center decoupled from the ITCZ, to support anything getting going -- just because a big atmospheric eddy has a cyclonic nature to it doesn't mean that it's a candidate for generating convection, let alone anything resembling tropical development.cycloneye wrote:Convection still is not consolidated as a circule but it's deep convection and beyond 40w waters are even more warm so let's watch it definitly and yes this thread will still be running.
You're much more likely to see something (if anything) form at the top end of the ITCZ buckle-up in the SE quadrant of the diffuse wave.