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myrzilka [38]
3 years ago
7

The scale height of the atmosphere (H) is a variable that meteorologists often use to do conversions from altitude to pressure.

Physics
1 answer:
julsineya [31]3 years ago
5 0

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.

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