AJC3 wrote:Hurricaneman wrote: The GFS depicts low shear and does little with it so that in itself makes no sense. And this may be another for the Bahamas which in no way if fair as they’ve been hit 2x in 2 weeks and maybe Florida needs to watch in case of a similar solution to the HWRF intensity wise with the GFS track. The HWRF intensity wise stood head and shoulders above the rest with Dorian so it can’t be discounted
From what I saw on visible satellite on Saturday, up until now, I don't think the issue was shear, but the presence of dry air aloft. The tell-tale sign to me was those arcus clouds that raced WNW-NW away from the area of convection on the east side of the wave axis. You don't get large surface outflow boundaries accelerating outward like that in the deep tropics unless you have some mid level dry air. That having been said, to the west, the 00Z RAOBs from Port-of-Spain and Point-a-Pitre were quite moist, and really didn't show much dry air aloft at all. So if dry air aloft had been a problem, it won't be for much longer.
How exactly does the mid level dry air lead to the formation of the arcus clouds? (apologies for my ignorance)