Four of the five storms developed from the intertropical convergence zone.

The location of the intertropical convergence zone varies over time.

The wave remained very close to the intertropical convergence zone for the next several days without any further development.

On Earth, the intertropical convergence zone is confined to the tropics.

By the middle of the dry season, the intertropical convergence zone moves south of Chad, taking the rain with it.

A disturbance that was part of the intertropical convergence zone developed several centers of circulation.

The area is also called the Intertropical Convergence Zone.

A disturbance in the intertropical convergence zone developed a circulation on August 29 and organized into a tropical depression two days later.

Most storms form in warm waters several hundred miles north of the equator near the Intertropical convergence zone from tropical waves.

The whole country is influenced by the Intertropical Convergence Zone during January.

Moving northwest, the system developed slowly as it was embedded within the Intertropical Convergence Zone.

Intertropical Convergence Zone, may affect thousands of Indians living in the coastal regions.

Throughout its duration, the depression never completely separated from the Intertropical Convergence Zone.

On October 18, a vortex in the intertropical convergence zone was determined to be a tropical storm through the use of satellite pictures.

This in turn, is influenced by the northward movement of the Intertropical Convergence Zone.

The system soon became unidentifiable within the Intertropical Convergence Zone, preventing quick development.

There does seem to have been the predicted southward shift in the global band of thunderstorms called the Intertropical convergence zone.

The intertropical convergence zone spawned a tropical depression on October 30 to the southwest of Haiti.

Eight-E developed a second center of circulation, which became dominant, and then became bound up in the intertropical convergence zone.

Occasional aberrant northward excursions of the intertropical convergence zone may boost precipitation in some years.

A scattered area of strong convection developed, partially in association with the Intertropical Convergence Zone.

Seasonal rainfall is driven mainly by the migration of the Intertropical Convergence Zone.

Thunderstorm activity slowly increased as the wave interacted within the Intertropical Convergence Zone.

Enhanced by the Intertropical Convergence Zone, a band of deep convection wrapped into the storm.

Tropical Depression Sixteen-E formed from a disturbance in the intertropical convergence zone.