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Its Derivation and Application in Meteorology
The equilibrium between water and water vapor depends upon the temperature of the system. If the temperature increases the saturation pressure of the water vapor increases. The rate of increase in vapor pressure per unit increase in temperature is given by the Clausius-Clapeyron equation. Let p be the saturation vapor pressure and T the temperature. The Clausius-Clapeyron equation for the equilibrium between liquid and vapor is then
where L is the latent heat of evaporation, and Vv and Vl are the specific volumes at temperature T of the vapor and liquid phases, respectively.
More generally the Clausius-Clapeyron equation pertains to the relationship between the pressure and temperature for conditions of equilibrium between two phases. The two phases could be vapor and solid for sublimation or solid and liquid for melting.
The material below is an examination of the application of the Clausius-Clapeyron equation to meteorology where the most relevant systems are water and water vapor and salt water and water vapor. But the equation also applies to ice and water vapor and ice and water. Finally there is a derivation of the Clausius-Clapeyron equation from thermodynamic principles.
Note that Vv is much greater than Vl so that to a good approximation
Furthermore the ideal gas equation applies to the vapor; i.e.,
where R is the universal gas constant.
In differential form this is
If L is independent of temperature then the solution to the differential equation is
where c1 is a constant.
The shape of this function is given below:
The empirical curves have the opposite curvature but clearly the equation dp/dT = L/(RT²/p) = Lp/T² indicates that as temperature increases the slope (dp/dT) decreases. Of course, the empirical curves take into account that the latent heat L can change with temperature, but the change in L with T is relative small. There is a fundamental discrepancy between the Clausius-Clapeyron Equation and the empirical relationships and the published derivations of the equation blithely show an empirical curve in which dp/dT increases with T and an equation in which dp/dT is inversely proportional to T. However this discrepancy will be left unresolved here and the implications of the Clausius-Clapeyron equation will will be further explored.
For some purposes the density of the vapor is of more interest than the pressure. By the ideal gas equation, the molecular density D is given by
The shape of this latter relationship for some arbitrary values of the parameters is shown below:
It is a surprise that there would be a case such that as the temperature goes up the density of decreases. This needs to be checked for generality.
The ideal gas equation indicates that density would go down as temperature increases if pressure remained constant. Even if pressure increases with temperature the density will decrease if the increase in pressure is not enough to offset the direct effect of the temperature increase on density. In differential terms the ideal gas equation is
The Clausius Clapeyron equation, when the specific volume of the liquid is assumed to be zero, gives
Thus the effect of a temperature increase on molecular density depends upon the magnitude of the latent heat of vaporization compared to RT.
The latent heat of vaporization for water is 2.257×106 J/kg. The gas constant for water vapor in SI units is 461.5 J/(kg K) so at T=300 K, RT=1.3845×105 J/kg. Thus L/RT=16.3 and hence dD/D=15.3(dT/T) so if (dT/T)=1/300 then dD/D = 15.3/300=.051.
Thus the relationship between density and temperature should look more like the following:
(To be continued.)
The derivation will be given for a liquid-vapor equilibrium interface but it equally well applies to the interface between any two phases.
Let sv and sl be the specific entropy of the vapor and liquid phases, respectively. The pressure and temperature of the two phases are equal. The chemical potential μ is equal on either side of the phase boundary curve. Therefore the changes dμ in the chemical potential for movements along the phase boundary curve are also equal. This means that
Solving for dp gives
But the change in entropy Δs for the phase change is just L/T so
This is the Clausius-Clapeyron equation.
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