#3 Postby Beam » Tue Aug 28, 2007 8:57 pm
Annular hurricanes are the disc- or donut-shaped storms that feature a large eye, an intense ring of convection, perfectly symmetrical outflow, and little to no banding. They are essentially a perfect heat engine, and have no need for ERCs.
A classic annular hurricane would be Isabel of 2003, and another, more notable one, though it may be debatable, is Katrina of 2005. As to how and why they form, the only thing I've been able to observe is that they tend to happen over large areas of open water in low shear environments, and seem to appear in the late stage of an ERC in an already symmetrical and intense system, except a large, donut-hole eye appears where the outer eyewall is, rather than the outer eyewall replacing the inner one as is typical.
This is usually followed by rapid intensification, with much fewer fluctuations in strength due to the lack of ERC's and the near-perfect organization of the system. This, combined with the fact that the larger eyewall produces a greater radius of devastating winds and surge, makes an annular storm far more dangerous than a typical hurricane, if it can maintain that structure until landfall.
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