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Tropical Storms Tropical Cyclone • Tropical cyclones are large, rotating, lowpressure storms that form over water during summer and fall in the tropics • The strongest of these storms in the Atlantic Ocean are known as hurricanes! ITCZ • Intertropical Convergence Zone Warm tropical waters near the equator… FORMATION – Tropical cyclones require two basic conditions to form: • An abundant supply of very warm ocean water • Some sort of disturbance to lift warm air and keep it rising Cyclone Movement • Tropical cyclones move according to the wind currents that steer them. Anatomy of Hurricane What is INSIDE? – The eyewall is a band immediately surrounding the eye that contains the strongest winds in a hurricane. –Once a hurricane, the development of a calm center of the storm, called an eye, takes place. Stages of Tropical Cyclones 1. A disturbance in the ITCZ zone lifts warm air near tropical waters 2. Cyclonic winds circle around a low pressure center = tropical depression 3. Wind Speeds reach 65 km/hr = Tropical Storm 4. Wind Speeds reach 120 km/hr = Hurricane Saffir-Simpson Scale • Criteria 1. Wind Speed 2. Damage Level 3. Pressure 4. Storm Surge Running out of Energy… – A hurricane will last until it can no longer produce enough energy to sustain itself. This usually happens when: • The storm moves over land and no longer has access to the warm ocean surface from which it draws its energy. • The storm moves over colder water. Storm Surge A storm surge occurs when hurricane-force winds drive a mound of ocean water, sometimes as high as 6 m above normal sea level, toward coastal areas where it washes over the land. Summary • Use the following terms in your summary! 1. 2. 3. 4. 5. ITCZ Eye & Eyewall Saffir-Simpson Scale Storm Surge “your choice” Match the following terms with their definitions. ___ ___ ___ ___ tropical depression hurricane eyewall storm surge A. a tropical cyclone with wind speeds of at least 65 km/h B. the band that has the highest wind speeds in a hurricane C. a tropical cyclone with wind speeds of at least 120 km/h D. a mound of winddriven water that washes over coastal lands