| Clark |
| (Meteorologist) |
| Sat Sep 01 2007 09:29 PM |
Re: Area of Interest - Invest 98L
|
That convection is likely going to help tighten up the broad, elongated, ENE-WSW oriented circulation associated with the storm, even given the shear in place. From there, the circulation/wind can draw those fluxes from the ocean's surface and start to build a tropical cyclone. Fairly classic case of the early steps of a developing tropical cyclone, even if it doesn't develop due to the shear and/or the occasional dry air burst.