Tropical Storm Julio quickly weakened over land, although it initially maintained strong convection near its center.

The storm had some strong convection and an eye-like feature (a clearing at the center).

Over the next two weeks, strong convection would develop before sunrise but dissipate by sunset.

The wave was accompanied by a weak center of low pressure and patches of moderate to strong convection.

Early on November 25, Kenneth weakened to a remnant low, with its circulation void of any strong convection.

It has strong vertical convection resulting to a redundant participation band and weak winds.

While at major hurricane status, Ivan kept very strong convection in its core with a well-defined eye.

With continued strong convection, Henriette maintained its strengthening and was predicted to reach hurricane strength.

A weak area of low pressure was found embedded within a large area of scattered moderate and isolated strong convection.

On June 16, strong convection with spiral banding developed over the depression, although it failed to strengthen further.