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On Sunday, it was still a tropical storm, with a center of circulation 35 miles west-northwest of Victoria, Tex.
Hurricane hunter flights had difficulty finding the center of circulation as the storm encountered a high shear environment.
The convection separated from the center of circulation.
Forecasters experienced difficulty in locating the exact center of circulation.
The center of circulation quickly became devoid of convection.
By later that day, the convection wrapped around the center of circulation.
The center of circulation approached within 17 mile of the coast of Mexico on June 22.
A central dense overcast developed, and a well-defined rainband wrapped around the center of circulation.
The center of circulation had become disorganized, with several small cloud swirls within the larger circulation.
Twelve hours later, the center of circulation became exposed from the convection.
Deep convection developed near the center of circulation, signifying a developing system.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com