It is noted that the positive values of d ln L/dTc used here required further investigation, but it is unfortunate that there are few complete observational studies for determining the temperature-dependent cloud LWC. There is also no complete observational data for quantifying the temperature dependence of the cloud droplet effective radius and cloud geometrical thickness. Based on Eqs. (2) and (3), the value of d ln D/dT can be estimated by dliiD dT

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