The next day, a small area of deep convection developed.

During the next six hours, Frank became much better organized with a large area of very deep convection near the center.

An eye, embedded within the deep convection, developed later in the day.

On July 2, deep convection began to join with the wave.

After several days, an associated area of low pressure gained deep convection and organization.

At that time, the center became exposed and lacked deep convection.

The central area of deep convection moved across every island in the archipelago.

Once in the Pacific, the system began to organize and develop deep convection.

This is because that the center was initially believed to be further north, closer to the deep convection.

The cyclone turned to the south, and lost its associated deep convection.