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What is wind?
Wind is air in motion. It is produced by the uneven heating of the earth’s surface by the sun. Since the earth’s surface is made of various land and water formations, it absorbs the sun’s radiation unevenly. Two factors are necessary to specify wind: speed and direction.
What causes the wind to blow?
As the sun warms the Earth's surface, the atmosphere warms too. Some parts of the Earth receive direct rays from the sun all year and are always warm. Other places receive indirect rays, so the climate is colder. Warm air, which weighs less than cold air, rises. Then cool air moves in and replaces the rising warm air. This movement of air is what makes the wind blow.
What is a derecho?
A derecho is a widespread and long-lived windstorm that is associated with a fast-moving band of severe thunderstorms. They can produce significant damage to property and pose a serious threat life, primarily by downburst winds. To be classified as a derecho, the path length of the storm has to be at least 280 miles long. Widths may vary from 50-300 miles. Derechos are usually not associated with a cold front, but a stationary front. They occur mostly in July, but can occur at anytime during the spring and summer.
What is the jet stream?
The jet stream is a fast flowing, river of air found in the atmosphere at around 12 km above the surface of the Earth just under the tropopause. They form at the boundaries of adjacent air masses with significant differences in temperature, such as of the polar region and the warmer air to the south. Because of the effect of the Earth's rotation the streams flow west to east, propagating in a serpentine or wave-like manner at lower speeds than that of the actual wind within the flow.
What are the global wind patterns?
The equator receives the Sun's direct rays. Here, air is heated and rises, leaving low pressure areas behind. Moving to about thirty degrees north and south of the equator, the warm air from the equator begins to cool and sink. Between thirty degrees latitude and the equator, most of the cooling sinking air moves back to the equator. The rest of the air flows toward the poles.
What are the trade winds?
The trade winds are just air movements toward the equator. They are warm, steady breezes that blow almost continuously. The Coriolis Effect makes the trade winds appear to be curving to the west, whether they are traveling to the equator from the south or north.
What are the doldrums?
The doldrums is an area of calm weather. The trade winds coming from the south and the north meet near the equator. These converging trade winds produce general upward winds as they are heated, so there are no steady surface winds.
What are the prevailing westerlies?
Between thirty and sixty degrees latitude, the winds that move toward the poles appear to curve to the east. Because winds are named from the direction in which they originate, these winds are called prevailing westerlies. Prevailing westerlies in the Northern Hemisphere are responsible for many of the weather movements across the United States and Canada.
What are the polar easterlies?
At about sixty degrees latitude in both hemispheres, the prevailing westerlies join with the polar easterlies to reduce upward motion. The polar easterlies form when the atmosphere over the poles cools. This cool air then sinks and spreads over the surface. As the air flows away from the poles, it is turned to the west by the Coriolis effect. Again, because these winds begin in the east, they are called easterlies.
What is a sea breeze?
On a warm summer day along the coast, this differential heating of land and sea leads to the development of local winds called sea breezes. As air above the land surface is heated by radiation from the Sun, it expands and begins to rise, being lighter than the surrounding air. To replace the rising air, cooler air is drawn in from above the surface of the sea. This is the sea breeze, and can offer a pleasant cooling influence on hot summer afternoons.
What is a land breeze?
A land breeze occurs at night when the land cools faster than the sea. In this case, it is air above the warmer surface water that is heated and rises, pulling in air from the cooler land surface.
How is wind helpful to Earth?
Wind is the fastest growing source of electricity in the world. It's often one of the least expensive forms of renewable power available. Some experts say it can sometimes be the cheapest form of any kind of power. Generating power from the wind leaves no dangerous waste products behind. Best of all, its supply is unlimited.
How do windmills work?
Windmills work because they slow down the speed of the wind. The wind flows over the airfoil shaped blades causing lift, like the effect on airplane wings, causing them to turn. The blades are connected to a drive shaft that turns an electric generator to produce electricity.
What are some different types of wind names?
Many local wind systems have their own names. Here's a few!
chinook-(easterly off the Rocky Mountains)
santa ana-(easterly towards Southern California )
scirocco-(southerly from North Africa to southern Europe)
mistral-(northwesterly from central France to Mediterranean)
marin-(south-easterly from Mediterranean to France)
bora-(northeasterly from eastern Europe to Italy)
gregale-(northeasterly from Greece)
etesian-(northwesterly from Greece)
libeccio-(southwesterly towards Italy)
Beaufort ScaleThe Beaufort scale is an empirical measure for the intensity of the weather based mainly on wind power. The scale was created by the British naval commander Sir Francis Beaufort around 1806.
| Beaufort number | Wind
speed MPH |
Wind
Speed Knots |
Description | Sea conditions | Land conditions |
| 0 | <1 | <1 | Calm | Flat | Calm |
| 1 | 1-3 | 1-3 | Light air | Ripples without crests | Wind motion visible in smoke |
| 2 | 4-7 | 4-6 | Light breeze | Small wavelets | Leaves rustle |
| 3 | 8-12 | 7-10 | Gentle breeze | Large wavelets | Smaller twigs in constant motion |
| 4 | 13-18 | 11-16 | Moderate breeze | Small waves | Small branches begin to move |
| 5 | 19-24 | 17-21 | Fresh breeze | Moderate longer waves | Smaller trees sway |
| 6 | 25-31 | 22-27 | Strong breeze | Large waves with foam crests | Large branches in motion |
| 7 | 32-38 | 28-33 | Near gale | Sea heaps up and foam begins to streak | Whole trees in motion |
| 8 | 39-46 | 34-40 | Gale | Moderately high waves with breaking crests | Twigs broken from trees |
| 9 | 47-54 | 41-47 | Severe gale | High waves with dense foam | Light structure damage |
| 10 | 55-63 | 48-55 | Storm | Very high waves. The sea surface is white |
Trees uprooted. Considerable structural damage |
| 11 | 64-72 | 56-63 | Violent storm | Exceptionally high waves | Widespread structural damage |
| 12 | 73-82 | 64-71 | Hurricane | Sea completely white with driving spray. | Massive and widespread damage to structure |
Wind ActivitiesLesson Plan: Here is a great activity the shows students how the winds work across the globe.
Wind Experiment: Here is a great experiment that allows the kids to find out what's in the wind. The kids will be very surprised at what they see!
Anemometer Experiment: Here is another great experiment that lets kids make an anemometer or windvane.
Windsock Experiment: Here is an experiment that allows the kids to make a windsock.