Consider a thin parcel of air at an arbitrary height z in the atmosphere (z= 0 corresponds to sea-level). It has thickness Az, cross-sectional area A, and mass density p. Assume gravity (g) is constant, and there is no wind, so the parcel is neither rising nor falling. There are three relevant forces: - The upward force F, acting on the bottom of the parcel. This is caused by air pressure P, from below. - The downward force F, acting on the top of the parcel. This is caused by air pressure P; from above. The weight force of the parcel itself, due to gravity.
Consider a thin parcel of air at an arbitrary height z in the atmosphere (z= 0 corresponds to sea-level). It has thickness Az, cross-sectional area A, and mass density p. Assume gravity (g) is constant, and there is no wind, so the parcel is neither rising nor falling. There are three relevant forces: - The upward force F, acting on the bottom of the parcel. This is caused by air pressure P, from below. - The downward force F, acting on the top of the parcel. This is caused by air pressure P; from above. The weight force of the parcel itself, due to gravity.
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