Formation- Tropical Depression, Tropical Storm, and Hurricane
Formation-Tropical Depression
surface winds strengthen, flow more efficiently around and into the core of the system
Coriolis effect spins the storm counterclockwise
surface winds converge with the central core and warm, moist air is pushed rapidly upwards (like a chimney)
warm air reaches the dew point which leads to water vapor condensing which leads to latent heat being released
surrounding air heated, strong updrafts created, rate of upward flow of warm air increased
Formation-Tropical Storm and Hurricane
converging winds continue to spiral the core
rotating rising and falling air masses generated by the heat (fuel) they acquire from the ocean
tropical storm: tropical cyclone with wind speeds of 39-74 mph
once surface wind speeds are very high (>74 mph), the wind can’t reach the center of the storm anymore
Characteristics