Thermodynamics
Newton's Law of Cooling
Rate of cooling proportional to temperature difference. Solution: T(t) = T_env + (T₀ - T_env)e^(-ht).
Variables
dT/dtK/s
Rate of temperature change
Cooling rate
h1/s
Cooling constant
Depends on surface and medium
TK
Object temperature
Current temperature
T_envK
Environment temperature
Ambient temperature
Derivation
Empirical law for convective cooling. Valid when temperature difference is small.
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