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.
The tornado itself is a powerful, rotating updraft. However, some tornadoes have a downdraft at their centers.
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.
When winds intensify, the force released can cause the updrafts to rotate
A tornado usually forms from a mesocyclone, which occurs in the updraft or rear portion of some thunderstorms.
A tornado starts from the mesocyclone, or strong, rotating updraft, of a supercell. A supercell is a type of especially powerful, rotating thunderstorm.
The tornado itself is a powerful, rotating updraft. However, some tornadoes have a downdraft at their centers.
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.
Tornadoes usually weaken if cold or dry air starts feeding into the updraft of the thunderstorm that drives the tornado. This causes the updraft, and thus the tornado, to lose power.
The tornado is part of the updraft of a thunderstorm that has become focused and very intense. The pressure inside a tornado is lower than in the surroundings, so air is dran into the tornado and then upwards by the updraft.
No. All thunderstorms require an updraft, but that updraft does not need to rotate. A supercell is not a rotating updraft, but rather a particular kind of thunderstorm with a rotating updraft.
No, the rotation of a tornado is stronger than its updraft.
A tornado develops when the rotating updraft of a thunderstorm becomes focused on a smaller area. The updraft of the tornado draws air upwards, creating a center of low pressure.
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.
When winds intensify, the force released can cause the updrafts to rotate
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.
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.