Later on June 28, a second center of circulation developed.

While strong winds were recorded, no circulation center was present.

Initially, several centers of circulation were associated with the system.

At this time, the cyclone had developed a center of circulation.

They form west of the circulation center and generally move from west to east.

Deep convection had developed in association with the low and was beginning to wrap around the center of circulation.

By later that day, the convection wrapped around the center of circulation.

However, the thunderstorm activity was exposed form the center of circulation.

Early on August 20, the system became more organized and developed a low-level circulation center.

The storm's circulation center remained poorly defined throughout its course.