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WFO Lake Charles, LA   Spring 2004
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How Hurricanes Form
By Mark Bacon, Meteorologist Intern

Hurricane formation is usually initiated in the tropics, typically at latitudes around 10 degrees north of the equator. In the late summer and early fall, the water temperatures exceed 80 degrees. This provides the heat and moisture needed for thunderstorm development. 
Converging surface winds along a tropical wave can cause grouping of thunderstorms.
Converging surface winds along a tropical wave can cause grouping of thunderstorms.  Photo courtesy of NASA.
Thunderstorms (which are commonly found in the tropics anyway) can be bunched together by weak waves of low pressure in the easterly surface winds.  When such a cluster of thunderstorms forms in the presence of jet stream winds or other forms of shear, they are not able to organize any further. However, given light winds both near the surface and aloft the group can remain and intensify.
 

With such intensification under way, latent heat is released as the thunderstorms condense water from vapor to liquid form (think of it this way, boiling water on a stove changes water from liquid to vapor and requires the input of heat, whereas water changing from vapor to liquid releases large amounts of energy). The combination of the heat release and the upward motion of the thunderstorms induce a mid-level low pressure within the complex of storms, now called a tropical disturbance. The presence of the mid level low draws up more warm and moist air and a feedback begins to develop. In the Northern Hemisphere the Coriolis force causes low pressure and thus the group of thunderstorms to begin to rotate counter-clockwise.  Usually by this time the system is called a tropical depression. Further strengthening will cause the more familiar swirling appearance of a tropical storm and eventually a hurricane.

 

Once formed, even a strong hurricane must remain in areas of light winds aloft. Otherwise its orderly spiral bands will begin to get sheared. This will weaken the system as a whole. Landfall also quickly weakens the storm both by causing friction and by cutting off the supply of warm and moist air at the surface.

Hurricane Lili Oct. 2002
Hurricane Lili Oct. 2002  Photo Courtesy NHC

 

Want to learn more? Check out the Hurricane FAQ Page at the National Hurricane Center

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Page last modified: April 4, 2004

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