Tropical Systems

Hurricane Patricia reached estimated maximum winds of 345 km/h in October 2015, making it the most intense tropical cyclone ever observed in the West.

A detailed look at the systemic engineering flaws and levee breaches that caused catastrophic flooding in New Orleans during Hurricane Katrina.

Learn why bomb cyclones explode through rapid pressure drops and jet stream interactions. Discover how explosive cyclogenesis fuels these intense storms.

Hurricane categories explained using the Saffir-Simpson wind scale to help you prepare for storm damage and intense wind speeds.

Learn how the Fujiwhara effect and interacting cyclones cause two storms to orbit a shared centre and change their paths. Discover how binary systems work.

Learn how does the eye of a hurricane form through angular momentum, centrifugal force, and adiabatic warming in this meteorology guide.

Learn how do tropical storms form through warm water, low wind shear, and the Coriolis effect. See how these atmospheric factors create severe weather.

Explore how do hurricanes form through warm ocean waters, convection, and the Coriolis effect.

Learn how the eyewall replacement cycle creates concentric eyewalls, triggers inner core collapse, and expands the wind field of intense cyclones.

Learn the science of how do tropical cyclones form through warm water, latent heat, and the Coriolis effect. See the conditions required for genesis.

Learn how do tropical depressions form from disturbances via warm water and the Coriolis effect.