Hey I'm back - looks like Gert's circulation is very close to the coast. And that all the convection on Franklin's upper level circ is being sheered off to the south, but clearly the two circulations are still moving in tandem. That is so weird. I am just learning about all this but I never would have thought this type of a situation was possible.
Now how does the interaction between the circulations work when they are still coupled but physically separated like this? What would a cross section of the storm look like?
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