No, the dark base of a tornado is called the funnel cloud. The wall cloud is a lowered cloud base associated with rotating updrafts that sometimes precede tornado formation.
Cloud base refers to the altitude above the ground at which the lowest portion of a cloud is observed. Cloud ceiling, on the other hand, is the height above the ground of the lowest cloud layer covering more than half of the sky. Cloud base is the specific altitude at which a cloud starts, while cloud ceiling is the overall height of the lowest cloud layer in the sky.
If the dewpoint temperature were lower, the height of the cloud base would generally be higher. This is because the air would need to cool further before reaching saturation, allowing clouds to form at higher altitudes. Conversely, a higher dewpoint temperature would lead to a lower cloud base height.
This is the dew point temperature, where the air becomes saturated with moisture and water vapor starts to condense into liquid water or fog at the cloud base.
The mesocyclone is typically located next to the wall cloud, in the rear portion of the thunderstorm updraft. The wall cloud is the lowering, rotating cloud that often forms at the base of a supercell thunderstorm where the mesocyclone is present.
celiometer
The ceilometer was invented by Alexander Thom in the 1930s. It is a meteorological instrument used to measure the height of a cloud base above the ground.
A nephoscope is an instrument used to measure the altitude and angle of clouds in the sky by visually tracking their movement relative to the instrument. By observing the movement of clouds against the gridded field of view of the nephoscope, the observer can estimate the cloud base height and direction.
No. An anemometer measures wind speed. A ceilometer measures the height of cloud base.
The answer depends on whether you wish to measure its height, base sides or base area, its mass, its albedo or whatever. There is no single instrument which will serve in all cases.
No, the dark base of a tornado is called the funnel cloud. The wall cloud is a lowered cloud base associated with rotating updrafts that sometimes precede tornado formation.
The funnel of a tornado always connects to cloud base and typically all the way to the ground (the circulation of a tornado can reach the ground even if the funnel does not). Cloud base height is variable but in a tornado supercell is usually about 3000 feet to a mile above the ground. The circulation of the tornado usually goes a great distance above cloud base and can reach heights of more than 4 miles.
Base x Height = Area
Height measures the distance from the base or bottom to the top of an object, typically referring to how tall something or someone is. In humans, height is commonly measured in feet and inches or in centimeters.
Cloud base refers to the altitude above the ground at which the lowest portion of a cloud is observed. Cloud ceiling, on the other hand, is the height above the ground of the lowest cloud layer covering more than half of the sky. Cloud base is the specific altitude at which a cloud starts, while cloud ceiling is the overall height of the lowest cloud layer in the sky.
Wall cloud.
A wall cloud is a large rotating cloud formation that extends beneath the storm cloud base, often found in severe thunderstorms and tornadoes. It appears as a lowering and rotating cloud base typically at the rear of the storm. Wall clouds are closely associated with supercell storms and can sometimes indicate an increased likelihood of tornado formation.