Answer:
True
Explanation:
The given statement is true because the scale height of the atmosphere (H) is a vertical distance over which the pressure and density of an atmosphere decrease by a certain factor. The scale height of the atmosphere has a constant value of 8,000 m and it often refers to the height one must ascend to achieve a certain value of density or pressure.
Thus, the scale height of the atmosphere (H) is a variable that meteorologists often use to do conversions from altitude to pressure.
