 Located in an environment of strong wind shear, much of the convection in the system was located well to the southeast of the poorly defined center of circulation.The depression moved northeastward and made landfall near Tampa, Florida on June 26 shortly before dissipating over land.The depression, in combination with an upper-level trough to its west, produced heavy rainfall to the east of its path, peaking at 33.43 inches (849 mm) in Cuba and 25 inches (635 mm) in Florida.