Deep convection increased near the center, and banding features began developing.

However, banding features and outflow improved at the same time.

However, a large convective banding feature developed to the north of the system.

At the same time, banding features became better organized.

Early on September 12, the system developed increased banding features over the eastern half of its circulation.

Despite the presence of wind shear it developed banding features.

By 25 February, the low developed a banding feature.

By 25 February, the low developed a banding feature in which the highest winds were located.

It quickly developed banding features, and organized into a tropical disturbance.

Around this time, a satellite picture showed a genuine eye beginning to form and banding features became apparent.