A thunderstorm does not become a tornad; it produces one. To start off, in most cases the storm must encounter strong wind shear, or a shift in wind speed and direction with altitude. This sets the storm rotating, turning it into a supercell. If the storm develops in the right manner, a downdraft may descend from the rare portion of the storm and wrap around the mesocyclone, or rotating updraft of the storm. This causes the mesocyclone or a portion of it to tighten and intensify, forming a tornado.
A tornado forms within a supercell thunderstorm, which is a type of severe thunderstorm with a rotating updraft called a mesocyclone. The tornado typically descends from a rotating wall cloud that is located beneath the base of the storm.
Tornadoes are typically associated with severe thunderstorms, which are characterized by towering clouds known as cumulonimbus clouds. It is unlikely for a tornado to form without the presence of clouds, as tornadoes require specific atmospheric conditions and interactions that usually occur within a thunderstorm system.
It is impossible to predict where the next tornado will occur.
Before a tornado occurs, the atmosphere needs to be unstable, with warm, moist air at the surface and cold, dry air aloft. Wind shear is also crucial, as it creates the rotation necessary for a tornado to form. Storm systems or supercell thunderstorms often provide the ideal conditions for tornado development.
Funnel clouds form when a tornado or developing tornado pulls in moist air. As the air is pulled inward it experiences a pressure drop which cools it to the point that the moisture condenses. For how tornadoes form see the link below.
A tornado can happen when the wind spins in a circle, wind spins around near and during a thunderstorm, and when hot and cold air meet. Most tornadoes happen May - August, summer for most people. But be aware, tornadoes can happen any time, anywhere, and in any thunderstorm or hurricane
A tornado forms within a supercell thunderstorm, which is a type of severe thunderstorm with a rotating updraft called a mesocyclone. The tornado typically descends from a rotating wall cloud that is located beneath the base of the storm.
The weather that precedes a tornado, including heavy rain and hail generally occurs in the front part of a supercell thunderstorm, with the tornado closer to the back.
For a hurricane: warm sea surface temperatures and little to no wind shear For a thunderstorm: convective instability and a lifting mechanism to start convection For a tornado: strong thunderstorms and strong winds shear.
If severe thunderstorm and tornado watches didn't exist, then people would be less likely to know about potential weather hazards. As a result, more people would likely be hurt or killed by severe thunderstorms and tornadoes.
A thunderstorm does not become a tornado, it produces them. How exactly thunderstorm produce tornadoes, but this is the best theory so far. First you need a special kind of thunderstorm called a supercell. This is a powerful, rotating thunderstorm. The rotation is especially strong at an updraft called a mesocyclone. If the strong strengthens fast enough a special kind of downdraft may descend from the back of the storm and wrap around the bottom part of the mesocyclone. This forces it to become smaller and can bring it down to the ground. As the rotation gets smaller it speeds up, producing a tornado.
Tornadoes are typically associated with severe thunderstorms, which are characterized by towering clouds known as cumulonimbus clouds. It is unlikely for a tornado to form without the presence of clouds, as tornadoes require specific atmospheric conditions and interactions that usually occur within a thunderstorm system.
In some cases one tornado will dissipate completely, and then a completely new tornado will form afterward from the same thunderstorm. This is called a tornado family.
The formation of tornadoes is complicated.First, a condition called wind shear, in which the speed or direction of the wind changes with altitude. If the shear is strong enough it can essentially tilt a thunderstorm, this separates the updraft and downdraft of the thunderstorm, preventing them from interfering with one another. This allows the storm to become stronger and last longer.Additionally, if the wind shear is strong enough it can start the air rolling in what is called horizontal vorticity. This horizontal vorticity can then be turned vertical by a thunderstorm's updraft. When this happens, the thunderstorm may start rotating. The rotation is especially strong in an updraft called a mesocyclone. If the storm intensifies rapidly enough, a relatively warm downdraft called a rear-flank downdraft or RFD can wrap around the bottom part of the mesocyclone. This can then tighten and intensify its rotation and bring it down to the ground to produce a tornado.
If we did not know the weather conditions than we could get into big disasters. For example, if we knew that there might be a thunderstorm coming there way or there was a tornado warning, we would be prepared for what might happen.
Microbursts are spawned by heavy to severe thunderstorms (if the microburst results in strong enough winds, the thunderstorm will become severe by definition).
A tornado can hit a house, but cannot happen indoors.