The tornado itself is vertical when it first forms. The rotation that forms it starts out as what is called horizontal vorticity. This vorticity can get caught in the updraft of a thunderstorm, tilting it into a vertical position. The new vertical rotation joins with the updraft to become a mesocyclone. Under the right conditions the mesocyclone can tighten and intensify to produce a tornado.
The visible funnel of a tornado is the result of moist air being pulled into the vortex. The low pressure in the tornado causes a temperature drop, which in turn causes the moisture to condense. Temperature continues to drop as the air rises in the tornado, causing more moisture to condense at higher altitudes..
The rotation originate from the speed and direction of the wind changing with altitude. This sets air rolling horizontally. This horizontal rolling can be turn vertical by the updraft of a thunderstorm. This can then tighten and intensify to form a tornado.
The principle of conservation of angular momentum causes a spinning column of air to turn to a vertical position. As the air rises, its size decreases due to conservation of angular momentum, causing the column to rotate and eventually orient vertically. This process is known as vortex stretching.
It varies. The tornado can vary in vertical extend from as little as 10,000 feet to as much as 60,000 feet. More violent tornadoes tend to be taller.
The mesocyclone developed from horizontally rolling air that get caught in the updraft of a thunderstorm and turned vertical.
The lift for vertical motion in a tornado is primarily caused by the strong updrafts within the rotating column of air. As the warm, moist air is drawn into the tornado, it is forced to rise rapidly, creating low pressure and lifting the air upwards. This process contributes to the intense vertical motion and can lead to the formation of the characteristic funnel cloud.
The thunderstorm might go down and turn into a tornado and then when it hits the ocean it might turn into a hurricane
The visible funnel of a tornado is the result of moist air being pulled into the vortex. The low pressure in the tornado causes a temperature drop, which in turn causes the moisture to condense. Temperature continues to drop as the air rises in the tornado, causing more moisture to condense at higher altitudes..
The rotation originate from the speed and direction of the wind changing with altitude. This sets air rolling horizontally. This horizontal rolling can be turn vertical by the updraft of a thunderstorm. This can then tighten and intensify to form a tornado.
A storm can't turn into a tornado, it a thunderstorm can produce one.
It dose not turn like a tornado.
Tornadoes don't exactly split, but there are multiple vortex tornadoes. A multiple vortex tornado may appear to be composed of several smaller tornadoes but is still in fact one tornado. The process by which this happens is not fully understood, but it begins when a downdraft is forced down the center of the tornado, widening it. If the tornado has the right ratio of rotational speed to vertical speed it can develop a multiple vortex structure.
strong updrafts of air in the cumulonimbus cloud
Tornado damaged is caused by a tornado's powerful winds and objects carried y those winds.
The horizontal rotation is caused by wind shear, differences in wind speed and direction with altitude. This can create horizontal vorticity in the air. This horizontal rotation then gets caught in the updrafts of thunderstorms in the area, which turn this rolling into vertical rotating columns within the storms. Eventually, the rotation in the storm can tighten and intensify to produce a tornado.
The principle of conservation of angular momentum causes a spinning column of air to turn to a vertical position. As the air rises, its size decreases due to conservation of angular momentum, causing the column to rotate and eventually orient vertically. This process is known as vortex stretching.
A tornado can lose its strength when it moves over cooler water or land, or if it encounters strong winds that disrupt its circulation. Additionally, if the thunderstorm that spawned the tornado weakens or dissipates, the tornado will also lose strength.