CAS Logo


 

Center for Atmospheric Sciences
 
Channels


Outreach

Outreach Overview
Outreach Partnerships
Current Outreach Programs

- Science on a SphereTM
  Science on a SphereTM Overview
  SOS Docents Schedule
  SOS Locations
  Hurricane PBL Module


Related Items

SOS @ NOAA
Dataset Pictures and Movies
SOS @ The National Maritime Center
SOS @ Maryland Science Center
SOS @ NASA Goddard
SOS @ Science Museum of Minnesota




 


Typhoons
The North Atlantic Basin includes the Atlantic Ocean, the Caribbean Sea and the Gulf of Mexico. Most hurricanes that form in the Atlantic basin begin as easterly waves that begin of the coast of Africa. The winds in these waves are basically from the east, but you can see how the winds vary by looking at the blue lines.

map2

Sea surface temperatures are very important in determining a hurricane's strength. The position of the Bermuda High is also important. To see how these variables may affect a hurricane's strength and movement check out this Hurricane Applet from the University of Wisconsin. Directions are at the bottom of the page if you want to see what the sea surface temperatures and the steering winds are.

If conditions are right - warm water, only weak winds aloft, the easterly wave may develop a closed circulation where we will see westerly winds on its south side. When this happens we have a tropical depression. When the winds reach 34 knots (39 mph), we have a tropical storm, and when they reach 64 knots, we have a hurricane. Hurricanes are steered by the winds around the subtropical high. To see how this works and also to look at the importance of water temperature, try this interactive Hurricane Applet from the University of Wisconsin.

You can also help determine the strength of a hurricane by seeing how cold its cloud tops are. Infrared satellite imagery lets us do this. To learn even more about how satellite images can help, see the page entitled "What does the brightness of a cloud mean on the TV weather shows?".

Hurricanes move with a forward speed, usually around 10 to 15 knots when they are traversing the tropical ocean. Forward speed can increase greatly as a hurricane moves into mod-latitudes.

A hurricane's tangential wind speed is a measure of the actual wind speed the hurricane possesses - these are the winds that cause the damage and push the ocean up ahead of the hurricane causing the storm surge.

See the University of Wisconsin simulation on how tangential winds are affected by the change in pressure near a hurricane

To learn a little about Atlantic hurricane climatology check out NOAA's page on Tropical Cyclone Climatology.

Historical tracks of hurricanes going back many years is can be found at NOAA's Archive of Hurricane Seasons.

Additional Hurricane Background Information:
The University of Illinois Online Meteorology Guide offers background readings along with well developed graphics and QuickTime movies to illustrate the formation and behavior of hurricanes. This is a rather extensive site and may take a up to 120 minutes to get a good grasp of the content.

Another very fine resource for hurricanes with good graphics is the USA Today's "All About Hurricanes Guide".

 

 

Scenarios | Hurricanes, Typhoons and Other Tropical Cyclones | Hurricanes in the North Atlantic Basin | Hurricanes and the Bermuda High Activity | Satellite Tracking of Hurricanes | Storm Surge | African Dust, El Nino, and Hurricanes

Teacher Pages

 
 
 
 
Center for Atmospheric Sciences, Hampton University, Hampton, Virginia 23668 - phone :757.727.5108 - fax :757.727.5090