There is no specific term for the winds in a tornado, though tornadoes are recorded separately from other wind events. The area where the winds are spinning may be referred to as the circulation, though this term can apply to other wind vorticies as well.
There is no particular instrument used for measuring tornado intensity. Ratings are based primarily on damage assessment. Occasionally doppler radar has measure wind speeds inside a tornado, but such measurements are rare.
The air pressure in a tornado is lower than that outside the tornado. That is why the wind blows toward the funnel.
This is called wind shear.
Such a violent whirlwind is called a tornado.
That varies. If you are close enough to be in the area of the tornado's inflow then the wind will blow almost directly towards the tornado, perhaps a little to the right of that direction. In that case the wind direction will depend on where the tornado is relative to you. If you are beyond the inflow area for the tornado, then nothing about the wind direction would indicate the approaching tornado.
The rotation in a tornado is driven by the wind shear, which is the change in wind speed and direction with height. This wind shear creates a horizontal rotation that is then tilted vertically by updrafts in the storm, leading to the spinning motion of the tornado.
It is believed that there is a calm "eye" at the center of a tornado. But mostly the winds in a tornado are very strong.
Not directly. But changes in wind speed and direction in altitude, called wind shear, plays an important role in tornado formation.
There is no particular instrument used for measuring tornado intensity. Ratings are based primarily on damage assessment. Occasionally doppler radar has measure wind speeds inside a tornado, but such measurements are rare.
Wind speeds inside of a tornado can vary greatly, with the most intense tornadoes having wind speeds exceeding 200 mph (322 km/h). The wind speeds near the center of the tornado, known as the eyewall, are typically the strongest, while the winds may be more variable toward the tornado's outer edges.
The main part of the circulation of a tornado when the strongest winds occur is called the core.
The speed of the winds in a tornado is called the tornado's wind speed. It is usually measured using the Enhanced Fujita (EF) scale, which categorizes tornadoes based on the estimated wind speed. The wind speed can vary greatly depending on the tornado's intensity, with stronger tornadoes having faster wind speeds.
The air pressure in a tornado is lower than that outside the tornado. That is why the wind blows toward the funnel.
Air and debris spin inside a tornado. The strong updrafts and rotation of the storm system can lift and move large objects, such as trees and even vehicles.
This is called wind shear.
Wind speed in a tornado is usually estimated using the damage caused by the tornado's winds and the Fujita scale, which categorizes tornadoes based on their intensity. Meteorologists may also use Doppler radar data to estimate wind speeds within a tornado. Direct measurement of wind speed in a tornado is rare due to the dangerous and unpredictable nature of tornadoes.
The air inside a tornado is cooler than its surroundings. This is not due to the wind or the fact that it comes from the sky, but from the fact that the pressure in a tornado is low. As air enters a tornado it is decompressed rapidly, and cools as a consequence. This is predicted by gas laws. In many cases the temperature inside a tornado is less than the dew point, which is why the funnel forms.