A tornado has a center of low pressure.
The center of a tornado is an area of intense low pressure.
No one really know pressure can vary for the type or category of a tornado.
Tornadoes are produced by thunderstorms, which are generally associated with low pressure systems.
Tornadoes have low air pressure at their center, known as the "eye" of the tornado. This sudden drop in air pressure can contribute to the destructive forces of a tornado by causing buildings to implode and trees to snap.
If by type you mean Fujita (F) scale rating, then generally the stronger the tornado the lower the pressure.
A tornado produces low pressure, but it is not a pressure system in and of itself.
The pressure inside a tornado is low compared to its surroundings, though exactly how low pressure can get in a tornado is unknown as few measurements have been taken, but it is generally accepted that the lower the pressure in a tornado, the stronger it is. Wind in a tornado moves in a circular fashion very rapidly, so the tornado is actually a type of powerful vortex. On rare occasions these winds can exceed 200 or even 300 mph (320 or 480 km/h). In addition winds in a tornado move upward very quickly at speeds similar to those of the rotation. Air near the tornado spirals inward
Tornadoes are usually associated with especially powerful thunderstorms called supercells.
A hurricane is associated with low air pressure.
No, thunderstorms do not have a low pressure center. Thunderstorms are a type of weather system associated with intense convective activity, but they typically do not have the organized circulation patterns seen in low pressure centers like those found in tropical cyclones or mid-latitude cyclones.
Cyclones and decreasing air pressure are associated with wind, clouds, and precipitation.
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