You must change the direction of the air flow, This is done by converting the downward pressure upward. You either need to use a forced air fan to change direction of the downdraft or to divert the air that normally flows downward into an upward motion by causing the downward air to be diverted into upward air chambers forcing the air upward. WindKat cowls has come up with a pretty good idea for solving this problem with chimneys. They say it is the most anti-downdraft cowl on the market. You can find them on the Web.
It depends. It is an updraft in most tornadoes, but in some tornadoes there is a downdraft at the center much like that in the eye of a hurricane.
The Dissipating stage, in which the downdraft overcomes the updraft and the clouds dissipate.
Not directly. A tornado forms in the updraft of a thunderstorm, but other forces, such as a downdraft are at work.
The tilted updraft is due to wind shear; a difference in the speed and direction of wind with altitude. The tilting of the updraft in a severe thunderstorm separates the updraft and downdraft, which prevents rain-cooled air from choking off the updraft. As a result the storm can become stronger.
The process is not fully understood. But, to start off, you need a special kind of thunderstorm called a supercell. Supercells form when the speed and direction of the wind changes significantly with latitude, a condition called wind shear. This tilts thunderstorms, separating the updraft of the storm from the downdraft. This allows the updraft to intensify without the downdraft choking it off, allowing the storm to grow stronger and last longer. Usually the updraft is in the back of the storm while the downdraft is in the front. The wind shear also sets the thunderstorms rotating. The rotation is particularly present in a powerful, rotating updraft called a mesocyclone. As the bottom of the mesocyclone intensifies and pressure drops it triggers a new downdraft near the back of the storm descends and wraps around the mesocyclone, tightening and intensifying the rotation to produce a tornado.
No. Its is the other way around. Thunderstorms usually dissipated when the downdraft overpowers the updraft. The updraft is what drives a thunderstorm.
updraft is superior. simple physics
The tornado itself is a powerful, rotating updraft. However, some tornadoes have a downdraft at their centers.
A supercell is a kind of thunderstorm cell. A thunderstorm cell consists of a convective unit with its own updraft and downdraft. A supercell is the most powerful type of storm cell with a strong, rotating updraft and distinct updraft and downdraft regions.
It depends. It is an updraft in most tornadoes, but in some tornadoes there is a downdraft at the center much like that in the eye of a hurricane.
updraft and downdraft
The Dissipating stage, in which the downdraft overcomes the updraft and the clouds dissipate.
Not directly. A tornado forms in the updraft of a thunderstorm, but other forces, such as a downdraft are at work.
The tilted updraft is due to wind shear; a difference in the speed and direction of wind with altitude. The tilting of the updraft in a severe thunderstorm separates the updraft and downdraft, which prevents rain-cooled air from choking off the updraft. As a result the storm can become stronger.
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.
Supercells differ from ordinary in a few important ways. The updraft of a supercell is stronger than that of an ordinary thunderstorm. That updraft also rotates, which is not see in ordinary storms. Finally, a supercell as separate updraft and downdraft areas.
The process is not fully understood. But, to start off, you need a special kind of thunderstorm called a supercell. Supercells form when the speed and direction of the wind changes significantly with latitude, a condition called wind shear. This tilts thunderstorms, separating the updraft of the storm from the downdraft. This allows the updraft to intensify without the downdraft choking it off, allowing the storm to grow stronger and last longer. Usually the updraft is in the back of the storm while the downdraft is in the front. The wind shear also sets the thunderstorms rotating. The rotation is particularly present in a powerful, rotating updraft called a mesocyclone. As the bottom of the mesocyclone intensifies and pressure drops it triggers a new downdraft near the back of the storm descends and wraps around the mesocyclone, tightening and intensifying the rotation to produce a tornado.