An area of disorganized showers and thunderstorms is associated with a surface trough of low pressure over the north-central Gulf of Mexico.
Surface pressures remain high, and environmental conditions do not appear favourable for significant development before this system moves inland over the central Gulf Coast in a day or so.
Regardless of development, the system could produce heavy rainfall and gusty winds over portions of the central Gulf Coast from southeastern Louisiana to the western Florida Panhandle.
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