Air pressure in a tornado is lower than that of its surroundings. Pressure deficits inside tornadoes have been measured as much as 194 millibars less than the surroundings.
Yes the pressure drops as the tornado forms and progresses. The tornado's lowest pressure is in the center.
Air in a tornado is rapidly drawn upward. This creates low pressure as more air rushes in to replace it. However this can ever completely fill the pressure deficit until the upward movement stops.
Air in a tornado, move upward rapidly creating a low pressure at its center. This low pressure essentially sucks air in.
The air pressure inside a tornado is very low.
The low pressure inside a tornado draws air inward, accelerating it to great speeds. Once air is in the circulation the low pressure at the center keeps it on a somewhat circular path.
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.
A tornado's central pressure is lower than the surroundings. In a strong tornado it may be 50 to 100 millibars lower. The actual pressure will, of course, depend on what the pressure of the surroundings are, which can vary with elevation and the tornado's parent storm system.
Pressure decreases sharply, reaching its lowest at the center of the tornado. This pulls air toward the center of the tornado and then drawn into the tornado's updraft. The tornado spins as it originates from a larger circulation called a mesocyclone.
The air pressure drops sharply in a tornado
Generally, it doesn't. Air generally moves up in a tornado. When the funnel of a tornado descends, the air is not moving down. The funnel itself is due to the pressure drop inside a tornado. This cools the air that is drawn into it, causing moisture in it to condense into a cloud. As the tornado forms and intensifies, the pressure and core temperature drop, allowing condensation to occur at a lower altitude. In some tornadoes, however, air does move down in the center of a tornado. This occurs when a tornado is spinning so rapidly that air spiraling in from the sides cannot reach the center. Instead, air is drawn downward through the center.
Air pressure in a tornado is lower than in the surroundings. Verifiable pressure drops of up to 100 millibars, about 10% of sea level pressure, have been recorded inside tornadoes.
Winds spiral in toward the low pressure center of a tornado an build up great speed due to this pressure gradient. However, as they get into the outer part of the tornado's core they are actually spinning so fast that the low pressure cannot pull this air in any further. So the air at the center remains relatively calm. A similar phenomenon is what creates the eye of a hurricane.