Thermodynamic principles and empirical studies confirm that the change in entropy of a system is dependent on temperature, often calculated via heat capacity integrals over temperature ranges.
The claim that entropy change depends on temperature is a foundational thermodynamic principle (since dS = dQ/T, and entropy change over a temperature range involves integrating heat capacity divided by temperature). Multiple papers in the literature (e.g., papers 6, 7, and 11) explicitly calculate or discuss entropy as a function of temperature.