The Clausius Clapeyron equation (dP/dT = L/TΔV) quantifies the relationship between pressure and temperature of a parcel substance during a phase change (IE: evaporation, condensation, freezing, sublimation, etc). It can be useful in solving for theta-e, moist adiabatic LR, etc, depending on what constants and/or inputs you have.
But it’s irrelevant to what we’re talking about because it contains no spatiotemporal variables. You’re trying to sound smart by invoking thermodynamic equations that you clearly do not understand.
I had forgotten about June 2008. A few days later we had the Yuge storm in early July. I have the T bolded on my records for the late June event also. Means it was a good one.