21cm and 16cm.what is the difference in height?
To calculate volume simply do length x width x height
Messure it,
The height and longer diagonal do not provide enough information to calculate the sides.
If you cannot estimate the height then, unless it is a very specific shape, you cannot calculate the volume.
Geopotential altitude is a measure of height above a reference level in the Earth's atmosphere that takes into account the variation of gravitational acceleration with altitude. It provides a more accurate representation of the vertical position of an object in the atmosphere compared to geometric altitude, which does not account for variations in gravity. Geopotential altitude is commonly used in aviation and meteorology to standardize altitude measurements.
The name of the line on a map that joins places of equals height is "the contour." Contour lines are lines of equal elevation, whereas isohypse are lines of equal geopotential height.
An atmospheric wave is a periodic disturbance in the fields of atmospheric variables like surface pressure or geopotential height, temperature, orwind velocity) which may either propagate
Altitude in an aircraft is generally measured by the hydrostatic equation: p=rho*g*h, where p is the pressure at the point of measurement, rho is the density at the point of measurement, g is the acceleration due to gravity at the point and h is the height from a reference to that point (the reference is generally taken as sea level). Aircrafts use the hydrostatic equation to determine the height/ altitude because pressure can be easily measured with a pitot tube that planes have. So using a pitot tube the airplanes measure the pressure and with that they can put it into the equation and solve for the height. However, gravity is not the same at different altitudes and changes with respect to the altitude. It is very difficult for an airplane to measure gravity in the air. Therefore airplanes generally measure geopotential altitude. The geopotential altitude uses gravity at sea level and takes it to be constant. Whereas geometric altitude uses gravity at the point of measurement. Therefore P = rho*g0*h(geopotential) where g0 is the gravity at sea-level and h(geopotential) is the geopotential altitude and P=rho*g*h(geometric) where g is the gravity at the point of measurement and h(geometric) is the geometric altitude or the actual height above sea-level Notice that the pressure and rho are common in both equations -by floyd617
They are found everywhere. These are also known as planetary waves, and are simply waves in the geopotential height field of the atmosphere. There are typically 3-7 of the at any given time circling the hemisphere.
How can you calculate height of airport traffic control tower?
Of what?
21cm and 16cm.what is the difference in height?
You just cube the height....like height to the 3rd power (height*height*height)
Probably. The northern hemisphere geopotential height pattern appears to be reloading into a prolonged -NAO again, or in other words, the same pattern that brought cold and snow earlier this winter appears to be set to repeat shortly.
You can calculate the volume by multiplying height, width, and mass. Then, divide the mass by the density to find the volume. Finally, calculate the length by dividing the volume by the height and width.
To calculate volume simply do length x width x height