The Physical Environment

                                                       
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Weather Systems

Hurricane Risk and Hazards

The Saffir-Simpson hurricane intensity scale is used to classify hurricanes. Though much damage from hurricanes is due to  the strong wind and tornadoes they often spawn when making land fall, it is the storm surge that creates the most. The storm surge is the high water level that accompanies a hurricane as it comes ashore. The storm surge is created by the force of the wind pushing up the water level. Storm surges cause flooding of low lying areas and much damage to property and life.  Weak hurricanes can produce storm surges of 3 to 6.5 feet (1 to 2 meters), while intense systems can create high water levels of over 16.5 feet (5 meters). The Bathurst Bay hurricane produced a 13 m (about 42 ft) surge in Bathurst Bay, Australia in 1899.

 

storm surgeFigure WS.29 Storm surge from Hurricane Eloise that struck the Florida coast in 1975
(Source: NOAA)

Flooding from a hurricane storm surge that hit Galveston, Texas on September 8, 1900 killed 6,000 people. On November 13, 1973 the vast coastal plain of Bangladesh was inundated with storm surge flooding that claimed an estimated 300,000 lives by drowning.

 

Figure WS.30 The Storm Surge
Courtesy National Geographic

The greatest risk for hurricanes in the United States is for those living along the sotheastern Atlantic seaboard where the warm waters of the Gulf stream provides fuel for storms. Hurricanes rarely affect the west coast with only four storms striking California in the last hundred years. Storms that do affect the west coast are usually remnants of tropical cyclones. Two primary reasons for so few incidences of tropical cyclones are cool coastal waters and the the direction of the prevailing winds. The presence of cold coastal water inhibits the formation or diminishes the strength of any storm that approaches land. Water temperatures along the coast of southern California rarely rise above 24 °C (75 °F) and usually don't get above 17 °C (63 °F). The upper level steering winds in the eastern Pacific winds move storms away from the coast. Tropical cyclones in the eastern Pacific generally move north-westward or westward due to steering by the prevailing upper level winds, which takes them far out to sea and away from the west coast of North America. Many living inland from the coast may feel relatively secure from the ravages of a hurricane. But as it moves onshore, severe tunderstorms, lightning, and tornadoes becomes a threat.

Hurricane risk in the United States

Figure WS.31 Hurricane risk for the United States

 

Hurricanes and Global Warming

Because warm water fuels hurricanes, recent trends in global warming and rising ocean temperatures increase the risk for more intense storms. There is debate as to whether global warming is responsible for the high number of intense storms experienced in 2005 or if it is part of a natural cycle of hurricane intensity.

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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