Potential Tropical Cyclone Three is gradually becoming better organized in the central Gulf of Mexico. The surface circulation has become well-defined, and convection is beginning to take on a curved-band appearance to the NE of the center. However, strong southwesterly wind shear continues to keep the storm lopsided, with the majority of wind and rain occurring well north and east of the center. Rainfall has already begun along the north gulfcoast, and will continue over the next couple of days. This heavy rain will be the primary impact of PTC3 along much of the gulf coast. Due to the aforementioned shear, PTC3 is not expected to strengthen much over the next couple days, but will likely acquire sufficient convective organization to be classified as a subtropical or tropical cyclone.
The system is currently interacting and partially merging with a mid-level low over the NW Gulf of Mexico. This low tilts NW with height, and the upper-level low remains just off the upper Texas coast. PTC3 is not expected to move fully beneath the upper low, thus moderate SW shear is expected to remain over the system until landfall along the TX or LA coastline sometime on Thursday. Due to growing proximity of PTC3 to the upper low, convective heating beneath the PV anomaly may cause shear to lessen some just before landfall. Some slight intensification is possible at that time, but the system is not currently expected to have enough time prior to landfall to take full advantage of it. The now robust low-level circulation is expected to become more symmetric, with moisture and potentially tropical storm-force winds wrapping around to the western semicircle. Thus, although most impacts currently remain north and east of the center, by the time of landfall, impacts may extend both to the east and to the west of the storm center when it crosses the coast.
Maximum Winds: 35 kt Gusts: 45 kt
Minimum Central Pressure: 999 mb
Environmental Pressure: 1007 mb
Radius of Circulation: 210 NM
Radius of Maximum Wind: 110 NM
Eye Diameter: N/A34 kt Wind Radii by Quadrant: