It soon dissipated due to continued shear and land interaction.

After a tremendous burst of convection over southern Taiwan, land interaction severely weakened the system.

Conditions were initially unfavorable for development, due to strong upper-level wind shear and land interaction.

Although the storm remained offshore, land interaction caused significant weakening.

Due to a combination of land interaction and increasing wind shear, Easu continued to weaken.

After weakening slightly because of land interaction, the cyclone slowly re-intensified as it pulled away from the island.

The combination of land interaction and wind shear caused dissipation that day.

After many hours of land interaction, Fay began to weaken.

Because of land interaction, Fanapi moved southwest, again turned west and weakened into a severe tropical storm.

It struggled against land interaction, however, and did not strengthen considerably, remaining poorly organised.