The response of an isothermal atmosphere
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R. L. Moore
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Article
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1974
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Springer
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English
โ 800 KB
The steady-state vertical-velocity response of an isothermal atmosphere to pressure fluctuations of arbitrary period and horizontal wavelength at its base is derived in the approximation of dissipationless polytropic motion in the atmosphere. It is pointed out that, since only upward modes can be ex