The mesocyclone developed from horizontally rolling air that get caught in the updraft of a thunderstorm and turned vertical.
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 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.
A tornado is typically spawned from a supercell thunderstorm cloud, known as a mesocyclone. These types of clouds are characterized by a rotating updraft, which can produce the necessary conditions for tornado formation.
Tornadoes rotate because they form from a larger mass of rotating air. In most cases this rotation comes from a mesocyclone, the rotating updraft of a supercell thunderstorm. The mesocyclone can tighten and intensify to produce a tornado. Some tornadoes form from a broad, weak circulation at ground level, which gets caught in a thunderstorm updraft and turned into a narrower but stronger vortex.
Yes, tornadoes form from rotating air within thunderstorms, typically coming from a change in wind direction and an increase in wind speed with altitude known as wind shear. The fast-moving air within a tornado is due to the intense rotation of air spiraling around the tornado's core.
A mesocyclone is a rotating updraft within a thunderstorm, usually a supercell. Under the right conditions a mesocyclone will tighten and intensify to produce a tornado. The majority of tornadoes form this way.
A tornado is a violently rotating column of air extending from the base of a thunderstorm to the ground, often made visible by a funnel or cone shaped cloud. A tornado occurs when rolling air called wind shear is turned vertical by a thunderstorm. This creates a supercell, a storm with a strong, rotating updraft called a mesocyclone. Under the right conditions a downdraft can wrap around the mesocyclone, forcing the rotating into a tighter, more intense vortex: a tornado.
Before a tornado touches down it is called a funnel cloud, which looks like a tornado but does not reach the ground. A funnel cloud develops from the mesocyclone of a supercell thunderstorm. A supercell thunderstorm is characterized by the presence of a mesocyclone, which is a deep, continuously-rotating updraft.
A supercell is a powerful thunderstorm with a strong, rotating updraft called a mesocyclone. They don't so much develop into tornadoes as they produce them. How they do this is not fully understood, but it is believed that moist of the time a downdraft called a rear-flank downdraft or RFD wraps around the bottom part of the mesocyclone, tightening and intensifying it to form a tornado.
Basically. A wall cloud is a a visible portion of the mesocyclone of a supercell. The mesocyclone is the the rotating part of a supercell that can produce 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 originate from a rotating updraft called a mesocyclone in a supercell thunderstorm. The mesocyclone forms when air near the storm begins rolling horizontally. This horizontal rolling gets pulled into the updraft and turned vertical. The updraft then takes on this rotation to become a mesocyclone..
I think the word you're looking for is "vortex".
To be put briefly: rolling air called wind shear gets turned vertical by a thunderstorm's updraft. This starts the storm rotating, turning into a supercell. Under the right conditions this rotating updraft, called a mesocyclone, can tighten and intensify into a tornado.
A tornado is formed when wind shear turns a storm into a supercell, a kinds of long-lived thunderstorm with a rotating updraft called a mesocyclone. Under the right conditions a downdraft may descend from the back of the storm and wrap around the mesocyclone, turning it into a tornado.
A tornado usually forms from a large column of rotating air called a mesocyclone. A tornado therefore has quite a bit of angular momentum, so air spirals into the it.
First of all, the tornado is not called a supercell in the initial phases. The supercell is the larger thunderstorm that produces the tornado; it is not the tornado itself. In a supercell there is a rotating area of low pressure, primarily within the updraft portion of the storm, called a mesocyclone. At the most intense portion of the mesocyclone there is a rotating, low-hanging cloud called a wall cloud. Conditions within the thunderstorm cause a portion of the mesocyclone to tighten and intensify, and the circulation of the tornado begins to develop and descend toward the ground from the wall cloud.