science lessons for eanassir:
Hurricanes need four conditions to form:
* low air pressure
* warm temperatures
* moist ocean air
* tropical winds (near the equator).
Hurricanes form in the tropics, over warm ocean water (over 80ºF or 27ºC) and at latitudes between 8° and 20°, Hurricanes form mostly from June through November (hurricane season). These powerful storms are fueled by the heat energy that is released when water vapor condenses (turns into liquid water -- rain).
A hurricane goes through many stages as it develops:
1. It starts as a tropical wave, a westward-moving area of low air pressure.
2. As the warm, moist air over the ocean rises in the low air pressure area, cold air from above replaces it. This produces strong gusty winds, heavy rain and thunderclouds that is called a tropical disturbance.
3. As the air pressure drops and there are sustained winds up to 38 miles per hour, it is called a tropical depression.
4. When the cyclonic winds have sustained speeds from 39 to 73 miles per hour, it is called a tropical storm (storms are given names when they begin to have winds of this speed).
5. The storm becomes a hurricane when there are sustained winds of over 73 miles per hour.
The End of a Storm:
When a hurricane travels over land or cold water, its energy source (warm water) is gone and the storm weakens, quickly dying.
Defining a Hurricane
To understand how a hurricane works, you have to understand the basic principles of atmospheric pressure. The gases that make up Earth's atmosphere are subject to the planet's gravity. In fact, the atmosphere weighs in at a combined 5.5 quadrillion tons (4.99 quadrillion metric tons). The gas molecules at the bottom, or those closest to the Earth's surface where we all live, are compressed by the weight of the air above them.
The air closest to us is also the warmest, as the atmosphere is mostly heated by the land and the sea, not by the sun. To understand this principle, think of a person frying an egg on the sidewalk on a hot, sunny day. The heat absorbed by the pavement actually fries the egg, not the heat coming down from the sun. When air heats up, its molecules move farther apart, making it less dense. This air then rises to higher altitudes where air molecules are less compressed by gravity. When warm, low-pressure air rises, cool, high-pressure air seizes the opportunity to move in underneath it. This movement is called a pressure gradient force.
These are some of the basic forces at work when a low-pressure center forms in the atmosphere -- a center that may turn into what people in the North Atlantic, North Pacific and Caribbean regions call a hurricane. What else is happening? Well, as we know, warm, moist air from the ocean's surface begins to rise rapidly. As it rises, its *water vap*or condenses to form storm clouds and droplets of rain. The condensation releases heat called latent heat of condensation. This latent heat warms the cool air, causing it to rise. This rising air is replaced by more warm, humid air from the ocean below. And the cycle continues, drawing more warm, moist air into the developing storm and moving heat from the surface to the atmosphere. This exchange of heat creates a pattern of win*d that circulates around a center, like water going down a drain.
But what about those signature ferocious winds? Converging winds at the surface are colliding and pushing warm, moist air upward. This rising air reinforces the air that's already ascending from the surface, so the circulation and wind speeds of the storm increase. In the meantime, strong winds blowing the same speed at higher altitudes (up to 30,000 feet or 9,000 meters) help to remove the rising hot air from the storm's center, maintaining a continual movement of warm air from the surface and keeping the storm organized. If the high-altitude winds don't blow at the same speed at all levels -- if wind shears are present -- the storm becomes disorganized and weakens.
*Even higher in the atmosphere (above 30,000 feet or 9,000 meters) high-pressure air over the storm's center also removes heat from the rising air, further driving the air cycle and the hurricane's growth. As high-pressure air is sucked into the low-pressure center of the storm, wind speeds increase. Then you have a hurricane to contend with.
How a Hurricane Forms
You never hear about hurricanes hitting Alaska. That's because hurricanes develop in warm, tropical regions where the water is at least 80 degrees Fahrenheit (27 degrees Celsius). The storms also require moist air and converging equatorial winds. Most Atlantic hurricanes begin off the west coast of Africa, starting as thunderstorms that move out over the warm, tropical ocean waters.
A hurricane's low-pressure center of relative calm is called the eye. The area surrounding the eye is called the eye wall, where the storm's most violent winds occur. The bands of thunderstorms that circulate outward from the eye are called rain bands. These storms play a key role in the evaporation/condensation cycle that feeds the hurricane.
The rotation of a hurricane is a product of the Coriolis force, a natural phenomenon that causes fluids and free-moving objects to veer to the right of their destination in the Northern Hemisphere and to the left in the Southern Hemisphere. Imagine flying a small plane directly south. While you're moving southward, the planet is rotating. If you plotted a flight from the North Pole to the equator on a map, the path will appear to curve to the right.
So in the Northern Hemisphere, winds deflect to the right. In the Southern Hemisphere, they deflect to the left. This wind deflection gets storms spinning. As a result, hurricanes in the Northern Hemisphere rotate counterclockwise and clockwise in the Southern Hemisphere. The force also affects the actual path of the hurricane, bending them to the right (clockwise) in the Northern Hemisphere and to the left (counterclockwise) if you're south of the equator. If you can't remember, just move within five degrees of the equator; the Coriolis force is too weak there to help form hurricanes.
Hurricanes often begin their lives as clusters of clouds and thunderstorms called tropical disturbances. These low-pressure areas feature weak pressure gradients and little or no rotation. Most of these disturbances die out, but a few persevere down the path to hurricane status. In these cases, the thunderstorms in the disturbance release latent heat, which warms areas in the disturbance. This causes the air density inside the disturbance to lower, dropping the surface pressure. Wind speeds increase as cooler air rushes underneath the rising warm air. As this wind is subject to the Coriolis force, the disturbance begins to rotate. The incoming winds bring in more moisture, which condenses to form more cloud activity and releases latent heat in the process.
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