D4-1 Hurricanes
The swirling structure of Hurricane Isabel is clearly visible in this view taken from the International Space Station in 2003.

Hurricanes are intense tropical storms with a strong rotating wind pattern. All hurricanes have a low pressure center. Hurricanes must have wind speeds in excess of 119km/h (74 mph) in order to be classified as hurricanes. Hurricanes are characterized by numerous thunderstorms that are accompanied by strong winds and rain. They are the most destructive storms on Earth.

A hurricane typically develops over the warm oceans of the tropics. It initially starts out as a group of thunderstorms that gradually begin to circulate around a low pressure system. In the northern hemisphere, this results in a characteristic counterclockwise pattern due to the Coriolis effect. This storm gradually picks up energy from the water that it travels over; the stored energy in the warm water as it first evaporates and then condenses acts as the energy source for future storm development. Such a storm is known as a tropical depression as long as its wind speed does not exceed 61 km/h (38 mph). If the storm continues to gain in intensity and achieves a wind speed between 61 and 119 km/h (i.e. 38–74 mph), it becomes known as a tropical storm. The storm finally achieves hurricane status when it achieves sustained wind speeds in excess of 119 km/h (74 mph).

A cross-section showing the internal structure of a hurricane.

The rotating structure of a hurricane is characterized by a prominent physical feature known as the eye of the hurricane. The eye is the calm center of a hurricane.

The relative intensity of a hurricane is categorized by a chart known as the Saffir-Simpson Scale.

Saffir-Simpson Scale
Hurricane Category Pressure (mb or hPa) Wind Speed Damage
    km/h mph  
         
1 ≥ 980 119–153 74–95 minimal
2 965–979 154–177 96–110 moderate
3 945–964 178–209 111–130 extensive
4 920–944 210–250 131–155 extreme
5 <920 >250 >155 catastrophic

A hurricane begins to lose its intensity after landfall. This is because it has lost its main source of energy: the heat stored in the warm waters of the tropics.