The Physical Environment

                                                       
Contents | Glossary | Atlas |  Index | Blog | Podcasts| Earth Online | Updates

Weather Systems

Hurricanes

Hurricane FloydFigure WS.26 Hurricane Floyd approaches the eastern seaboard of the United States
(Source: NOAA Click image to enlarge)

A hurricane (or typhoon) is a large rotating cyclonic system born in the tropics. They are the largest and most destructive storms on Earth. Most associate high winds with the devastation that these massive storms create, yet dangerous flooding, tornadoes, lightning often accompany or are spawned by a hurricane.


Hurricane Formation

A hurricane develops from a tropical disturbance once it reaches sustained winds in excess of 75 mph (65 knots) . Most hurricanes form poleward of 10o latitude as the Coriolis effect is too weak closer to the equator. Hurricanes form in a uniform mass of warm air over tropical oceans with temperatures of 80o F (26.5o C) through a depth of 200 feet (60 meters). Hurricanes thus do not exhibit fronts like extratropical cyclones of the mid- and high latitudes. The "fuel" for a hurricane comes from the enormous amount of latent heat released from the warm ocean water. video iconSee NASA's "Birth of a Hurricane" for more about Atlantic Ocean hurricanes.

Hurricane structureFigure WS.27 Internal structure of a hurricane (Source: NOAA)

A hurricane is a warm-core low pressure system that weakens rapidly with altitude to be replaced by anticyclonic airflow above the hurricane. The center or eye of the hurricane is an area of nearly cloudless skies, subsiding air, and light winds. The eye ranges from 12 to 40 miles across (20 - 65 kilometers). At the periphery of the eye is a ring of cumulonimbus clouds that produce torrential rains and extremely strong winds.  Surrounding the core of storms are the typical spiraling rain bands. The Saffir-Simpson hurricane intensity scale is used to classify hurricanes.

As a hurricane moves over a colder surface or land, it loses its source of energy and dissipates. However, the system can remain an organized storm for several days as it moves inland, inundating the interior with rainfall causing severe flooding. Destructive tornadoes often accompany hurricanes as the move ashore.

Figure WS.28 Hurricane Katrina takes aim at the United States.
Hurricane Katrina
struck the Gulf coast of the United States
wreaking havoc in Louisiana, Mississippi and Alabama.
Courtesy NASA

 

 

 

Previous | Continue     


Contents |Glossary | Atlas Index  |  Blog | Podcasts Updates | Top of page

WebActive: Active Learning on the Web

About TPE | Who's Using TPE |  Earth Online

Please contact the author for inquiries, permissions, corrections or other feedback.

For Citation: Ritter, Michael E. The Physical Environment: an Introduction to Physical Geography.
2006. Date visited.  http://www.uwsp.edu/geo/faculty/ritter/geog101/textbook/title_page.html

© 2003-2008
Michael Ritter (tpeauthor@mac.com)
Last revised 06/21/07