Tornadoes require severe thunderstorms to form. Such storms usually occur along a boundary between warm, moist air and either cool air, dry air, or a combination of the two. Tornadoes also require wind shear, which is where wind speed and direction vary with altitude. By a somewhat complicated process this wind shear gives storms the rotation they need to produce tornadoes. These rotating storms are called supercells.
Two main weather conditions exist to create a tornado: instability in the atmosphere and wind shear in the lower atmosphere. In the case of a tornado, instability refers to the presence of warm air closer to the Earth's surface and cooler air further above the surface. Wind shear refers to instances when the wind direction changes, and wind speed increases, with height. These conditions usually exist only ahead of a cold front and low pressure system, and are especially found in thunderstorms. The spinning motion of tornadoes is often caused by the interaction between the updrafts and downdrafts in the thunderstorm and the wind shear. The conflicting drafts cause the wind shear to tilt, and an upright tornado vortex is formed.
Tornadoes, simply put, are produce by complicated interactions of wind current in a supercell thunderstorm.
A tornado gets its energy from the the thunderstorm that produces it. Most tornadoes are a product of thunderstorms with strong, rotating updrafts. These rotating updrafts get their energy from a combination of water vapor and wind shear. The water vapor is the main fuel of the storm. Thunderstorms work by drawing warm, moist air upwards from near the ground. As the air rises it cools and the water vapor condenses, releasing huge amounts of energy in the process. The wind shear, meaning difference in wind speed and direction with altitude, gives a storm the spin it needs to produce tornadoes.
Global winds affect the general weather patterns in many regions. In areas that have high frequencies of tornadoes, wind patterns and regional topography often lead to warm moist air masses colliding with cooler air and/or drier air, thus producing strong thunderstorms that can potentially produce tornadoes. Such regions also often have a lot of wind shear, which occurs when the speed and direction of wind changes with altitude. This can give storms the rotation needed to produce tornadoes. Finally, global winds affect the direction that tornadoes usually travel. For example, due to the prevailing winds most tornadoes in the United States travel from southwest to northeast.
Condensation and wind shear are both needed for tornadoes to form. Tornadoes can form along stationary fronts as well.
Ultimately, the two primary causes of tornadoes are convective instability, which leads to thunderstorms, and wind shear, which gives those storms the rotation they need to produce tornadoes.
wind shear- earth science
wind shear causes the formation of a tornado if you have a strong thunderstorm.
That itself does not cause tornadoes, but a similar phenomenon is a factor in tornado formation. When wind at different altitudes blows in different speeds and directions, the air in between and start to roll horizontally. This is called wind shear. Again, wind shear alone cannot produce a tornado, but it is an important factor in how tornadoes form.
The jet stream produces wind shear, or differences in wind speed and direction with changing height. Wind shear is a necessary ingredient for producing tornadoes, but on its own it can't do much. To get tornadoes you need thunderstorms. When thunderstorms develop in strong enough wind shear they can start to rotate. This rotation can the develop into a tornado. But this sort of rotation cannot be produced by wind shear alone.
The jet stream is a band of fast winds several miles above the ground. This strong wind creates wind shear, which can affect thunderstorms. First, the wind shear alters the circulation of air in the thunderstorm so that it can become stronger and last longer. Second, if the setup is right, wind shear can set a storm rotating, allowing it to produce tornadoes.
thunderstorms, strong winds (usually), and wind shear
Wind shear can help turn an ordinary thunderstorm into a dangerous one that can spawn tornadoes.
Tornadoes are more common in April, May, and June than in February or March. The two most fundamental ingredients needed for making tornadoes are instability and wind shear. Instability occurs when the lower atmosphere is warm and moist and cools quickly with increasing height. Instability allows thunderstorms to form. Wind shear occurs when the speed and direction of wind changes with altitude. Wind shear tends to be strongest in winter and weakest in summer, while the opposite is true of instability. The most ideal combination of wind shear and instability generally occurs in the spring.
Wind shear.
Condensation and wind shear are both important in tornado formation. Tornadoes develop from thunderstorms, which are powered by the energy released from condensation. Wind shear is what gives thunderstorms the rotation then need to produce tornadoes. Tornado-producing storms may form along a stationary front, but are more common along cold fronts.