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.
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Generated May 3, 2024, 8:27:31 AM EDT
When in doubt, take the word of the National Hurricane Center