A tornado produces very low pressure.
Generally the lower the pressure inside a tornado (compared with its surroundings) the stronger and more destructive the winds are. For example, if the pressure surrounding two tornadoes is 960 millibars, a tornado with a central pressure of 860 millibars will be stronger than one with a pressure of 900 millibars.
Winds in a tornado are extremely high because the pressure at the center of the tornado is much less than its surroundings, and this pressure drop occurs over a very small distance. Differences in pressure are what cause most winds. The greater the pressure difference over a given area, the greater the wind speed.
All wind on Earth is ultimately driven by pressure differences. As a general rule, the more the pressure changes over a given distance, the stronger the wind can be. A tornado is a small center of intense low pressure. That pressure drop occurs over a very short distance, which causes air to rush into the tornado rapidly and reach very high speeds in and near the core.
High pressure systems can inhibit tornado formation by creating stable atmospheric conditions that suppress the development of thunderstorms, which are a necessary ingredient for tornadoes. When high pressure dominates an area, it can limit the availability of moisture and wind shear needed to fuel tornado activity. However, high pressure can also sometimes enhance tornado potential by creating strong boundaries with low pressure systems, leading to favorable conditions for tornado formation along these boundaries.
High air pressure aloft can increase wind shear, which is a key factor in tornado rotation. Wind shear is the change in wind direction and speed with height, and when it increases due to high pressure systems, it can enhance the rotational capabilities within a storm system and potentially lead to tornado formation.
cool, dry weather
A high pressure center is characterized by cool dry air, as it is associated with descending air that warms and dries as it sinks towards the surface.
A high pressure center of dry air is called an anticyclone
Since a tornado is columnar in nature its center is best defined as the tornado's axis of rotation, which also corresponds with the lowest pressure. The actual height of the midpoint varies with how high up the tornado extends, with stronger tornadoes usually extending further up into the parent storm.
A high pressure systems has a high pressure center.
Generally the lower the pressure inside a tornado (compared with its surroundings) the stronger and more destructive the winds are. For example, if the pressure surrounding two tornadoes is 960 millibars, a tornado with a central pressure of 860 millibars will be stronger than one with a pressure of 900 millibars.
Winds in a tornado are extremely high because the pressure at the center of the tornado is much less than its surroundings, and this pressure drop occurs over a very small distance. Differences in pressure are what cause most winds. The greater the pressure difference over a given area, the greater the wind speed.
The rotation of air around a high pressure center is called anticyclonic flow. It is characterized by air moving in a clockwise direction in the Northern Hemisphere and counterclockwise in the Southern Hemisphere.
A tornado actually produces low pressure rather than high pressure. The greatest pressure drop recorded in a tornado was 100 millibars or about 10%. However, this was recorded from a probe at the edge of the tornado, and even then, there have been stronger tornadoes than that one.
it is a tornado
All wind on Earth is ultimately driven by pressure differences. As a general rule, the more the pressure changes over a given distance, the stronger the wind can be. A tornado is a small center of intense low pressure. That pressure drop occurs over a very short distance, which causes air to rush into the tornado rapidly and reach very high speeds in and near the core.
Tornadoes typically form in areas of low pressure because it creates a pressure gradient that can lead to the rotation needed for a tornado to develop. High pressure systems typically bring less instability and moisture, making them less conducive to tornado formation.