I was wondering if the high level winds are, basically, westerlies (from the SW), then why am I seeing the area south of Epsilon where cloud tops are trailing to the W?
I was wondering could this be the dissipating low that was just south of it, because it didn't seem like outflow, except just immediately south of the center.
Also, it seems like the convection around the center has died off a bit. But it looks like Epsilon is going to be in an area of decreased shear for awhile, so that it'll build up some steam again overnight.
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