The tornado itself is a powerful, rotating updraft. However, some tornadoes have a downdraft at their centers.
There are a couple ways in which a tornado can form, both involving the updraft of a thunderstorm. In the classic model of tornado formation, the updraft of the thunderstorm starts rotating due to interaction with wind shear (differences in wind speed and direction with altitude) and may be influenced by the general rotation of the parent storm system. The tornado then develops from this rotating updraft. In the other model, by which landspouts and most waterspouts form, a broad-level circulation at the ground gets caught in the updraft of a developing thunderstorm, becoming narrower and more intense.
A tornado usually forms from a mesocyclone, which occurs in the updraft or rear portion of some thunderstorms.
The tornado forms from the already existing updraft of a thunderstorm. The thunderstorm has (and actually develops from) an updraft that occurs as a result of an ai mass being warmer, moister, and thus less dense than either the surrounding air or an adjacent air mass.
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.
The updraft of a tornado may help somewhat in stabilizing the atmopshere, but the parent thunderstorm normally would do that anyway.
Usually a tornado will have a strong updraft at its center, but some tornadoes sometimes have a gentle downdraft at the center instead while the powerful updraft is limited to the area surrounding it. This is analogous to the eye and eyewall of a hurricane.
No, the rotation of a tornado is stronger than its updraft.
There are a couple ways in which a tornado can form, both involving the updraft of a thunderstorm. In the classic model of tornado formation, the updraft of the thunderstorm starts rotating due to interaction with wind shear (differences in wind speed and direction with altitude) and may be influenced by the general rotation of the parent storm system. The tornado then develops from this rotating updraft. In the other model, by which landspouts and most waterspouts form, a broad-level circulation at the ground gets caught in the updraft of a developing thunderstorm, becoming narrower and more intense.
A tornado forms from the rotating updraft of a thunderstorm. The updraft of the tornado creates low pressure that causes air to spiral inward (usually counterclockwise int he northern hemisphere and clockwise in the southern) and then upward.
Air in a tornado moves up because the tornado forms in the updraft portion of a thunderstorm.
Air enters a tornado through the updraft at the storm's center. The intense rotating updraft pulls in surrounding air, creating a spiraling column of wind. This process continues to strengthen as more air is drawn in, fueling the tornado's development.
How a tornado ends is not fully understood. It is thought, however, that cold air coming out of a thunderstorm (called outflow) undercuts the mesocyclone, the rotating updraft that drives the tornado. This chokes off the supply of warm air that feeds the updraft.
The rotating updraft within a thunderstorm, known as a mesocyclone, is responsible for creating the conditions that can lead to a tornado. When this rotating air column tightens and extends to the ground, it can form a tornado.
A tornado usually forms from a mesocyclone, which occurs in the updraft or rear portion of some thunderstorms.
A normal tornado is a violently rotating column of air the descends from the rotating updraft of a thunderstorm. A fire tornado or firewhirl, which is technically not a tornado, is a vortex of smoke and/or flame that forms at ground level from the updraft of an intense fire. Firewhirls can potentially produce winds equivalent to an EF0 or EF1 tornado, but the main threat is their ability to spread a fire further.
A tornado is a very intense vortex of air. Air spirals in towards the low pressure at the center of the tornado and is then drawn upwards. Most tornadoes form from a larger vortex called a mesocyclone, which is part of the updraft of some thunderstorms. At some point this vortex tightens and intensifies to form a tornado.
A thunderstorm will cause a tornado. The thunderstorm clouds are the Cumulonimbus clouds. The majority of thunderstorms that produce tornadoes are in a special class called supercells. These are the most powerful thunderstorms on earth and are noted for having a rotating updraft called a mesocyclone.