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Hurricane Hut

About Hurricanes
Tropical Terminology
Active Storms
About Hurricanes
About Us
Atlantic Basin Storm Archives
East Pacific Storm Archives
Hurricane Naming
Retired Hurricane Names
Hurricane Elena of 1985, a Strong Hurricane

The Basics

A hurricane is one of nature's most awesome forces. Scientists at the National Center for Atmospheric Research estimate that a hurricane releases heat energy at the rate of 50 to 200 trillion watts - about the amount of energy released by exploding a 10-megaton nuclear bomb every 20 minutes. Hurricanes are found all over the world, and are not always called hurricanes. In the North Pacific Ocean hurricanes are called Typhoons, and in the South Pacific and South Indian Ocean they are called Cyclones. Whatever the name, a storm must have winds greater than 73 mph to be classified as a hurricane.

The Mechanics

Impressive Outer Bands of Hurricane Katrina

A hurricane is basically a large storm, relatively speaking. Hurricanes are powered by warm water, and moist air, which is why they are found in tropical areas. Hurricanes are a large, rotating system of clouds and thunderstorms which can cause tremendous damage, the clouds from the hurricane eventually form outer spiral bands as the storm becomes stronger. This is called outflow, and helps the storm grow in size and strength acting as a chimney for the storm. The outflow releases the dry air that the hurricane stripped the moisture of. Without this release, the hurricane would not be able to thrive. These high outer bands and clouds give the hurricane its swirling appearance. Moist air is critical in maintaining a powerful hurricane. The outer bands are generally able to keep dry air from entering the circulation, but when dry air is able to wrap its way into the eye, the hurricane is in trouble. When the dry air enters the eye, it destroys the storms, and weakens the storm. Without convection near the eye, the winds die down and the hurricane weakens.

The Eye

The Tiny Eye of Wilma

The eye of the storm is the calm center of the storm, which is usually calm and sometimes completely cloud free. Stronger hurricanes tend to have larger eyes, and some weak hurricanes never develop a clear and distinct eye. The eye is the area of sinking air inside the storm and is the center of cirulation. Eyes of hurricanes range greatly in size, sometimes as large as 125 miles in diameter. Hurricane Wilma of 2005 had one of the smallest eyes ever recorded, due to the incredibly rapid intensification. The eye later widened as Wilma underwent eyewall replacement cycles. Although the eye is the calmest area of the storm, just outside the eye is the powerful eyewall; which is where the worst of the storm is found. The eyewall is the strongest convection of the storm, wrapped around the eye. This is where the highest winds, heaviest rains, and most powerful convection of the storm is found. Most damages by hurricanes are caused when the eyewall passes over land. In strong hurricanes, the eyewall is very symmetrical, wrapping completely around the eye. In weaker storms, the eyewall may not even exist and may be unevenly distributed around the eye. This is sometimes due to wind shear which blows the storm out of proportion, restricting thunderstorms in certain areas. When the outerbands begin to gather intense convection, robbing the center of such, this is known as an eyewall replacement cycle and usually weakens the storm temporarily. The outer eyewall eventually replaces the inner eyewall, usually resulting in a larger sized eye.