Brief communication: Lower-bound estimates for residence time of energy in the atmospheres of Venus, Mars and Titan
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Abstract. The residence time of energy in a planetary atmosphere, τ, which was recently introduced and computed for the Earth's atmosphere (Osácar et al., 2020), is here extended to the atmospheres of Venus, Mars and Titan. τ is the timescale for the energy transport across the atmosphere. In the cases of Venus, Mars and Titan, these computations are lower bounds due to a lack of some energy data. If the analogy between τ and the solar Kelvin–Helmholtz scale is assumed, then τ would also be the time the atmosphere needs to return to equilibrium after a global thermal perturbation.
2021 ◽
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1962 ◽
Vol 66
(624)
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pp. 764-766
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2002 ◽
Vol 110
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pp. 182-185
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1975 ◽
Vol 117
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pp. 313-332
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