IT is called CONVECTION
When the movements of air are vertical, either updrafts or downdrafts, they are called convection currents. These currents are responsible for transferring heat and moisture in the atmosphere, influencing weather patterns and cloud formation.
there are four options 1. wind 2. air current 3. air turbulence 4. air mobility
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.
convection cell
Tornadoes usually form from a type of thunderstorm called a supercell, which has a rotating updraft called a mesocyclone. A downdraft at the back of the storm, called the rear-flank downdraft or RFD is believed to wrap around the tornado, tightening and intensifying it to produce a tornado.
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.
Rising and sinking air is called up draft and down draft, respectively.
For the most part a tornado is actually an updraft as it is connected with the rotating updraft of its parent thunderstorm. However there are two downdrafts that are related to tornadoes. The first is the rear-flank downdraft of a thunderstorm. This downdraft is induced by rain and wraps around the rotating updraft of a supercell thunderstorm. This is believed to tighten and intensify the mesocyclone to produce a tornado. Another, less common downdraft occurs when a tornado undergoes something called vortex breakdown. The center of a tornado has low pressure, which draws air inward and upward, but in a very intense tornado the air is spinning so fast that it cannot reach the center so the low pressure draws air downward, forming a downdraft in the center of the tornado. This is a similar mechanism to what produced they eye of a hurricane.
The storm that produces tornadoes (called a supercell) has a powerful, rotating updraft called a mesocyclone. The storm takes on this rotation when wind speed and/ or direction changes with altitude. This can start air rolling in what is called horizotnal vorticity. This horizontal rotation can then get turned vertical and become joined with a thunderstorms updraft to start it rotating on a vertical axis.Tornadoes get their rotation from a rotating updraft called a mesocyclone. The tornado actually originates from the mesocyclone. The mesocyclone is part of a type of powerful thunderstorm called a supercell.The supercell gets its rotation when the wind speed or direction changes with altitude. This starts air rolling horizontally. This horizontal rolling can then get turned vertical by a thunderstorm updraft, which in turn starts the updraft rotating.
The upward movement of warm air is called convection. This process occurs as warm air rises due to its lower density compared to cooler air, creating vertical air currents in the atmosphere.
Air moving up is called "updraft," while air moving down is referred to as "downdraft." Updrafts typically occur in weather phenomena like thunderstorms, where warm air rises rapidly, whereas downdrafts can occur when cool, dense air descends. Both processes are essential in atmospheric dynamics and play significant roles in weather patterns.
A geodetic instrument called an extensometer or tiltmeter is used to measure tiny vertical or horizontal movements of markers set up on opposite sides of a fault. These instruments can detect even small changes in the Earth's crust, helping to monitor potential fault movements and seismic activity.