Definition
A thermodynamic process is called adiabatic if there is no heat exchange between the considered air or fluid parcel and its surroundings. Consequently, temperature changes are induced by a change in pressure. This process is a key point to determine the temperature gradient of planetary atmospheres and also of oceans.
In planetary atmospheres, an air parcel drifted upward cools and expands due to the decrease in atmospheric pressure. The rate at which the temperature falls is quantified by the adiabatic lapse rate(Pierrehumbert 2010; Wallace and Hobbs 2006). If the partial pressure of the condensable gas is below the saturation pressure, the process is called dry adiabatic, and its lapse rate is −dT/dz. = g/cp where g is gravity acceleration and cp the heat capacity of the gas. Indicative lapse rate values of different planets are given in Table 1.
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Chaverot, G. (2021). Adiabatic Processes. In: Gargaud, M., et al. Encyclopedia of Astrobiology. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-27833-4_5504-1
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