Closed-form evaluation of the zero-dimensional radiative-balance equilibrium. Setting absorbed solar πR²·S(1−α) = emitted longwave 4πR²·σT_eq⁴ and solving for T_eq yields the quartic root. Sympy canonical form: T_eq =…
Closed-form evaluation of the zero-dimensional radiative-balance equilibrium. Setting absorbed solar πR²·S(1−α) = emitted longwave 4πR²·σT_eq⁴ and solving for T_eq yields the quartic root. Sympy canonical form: T_eq =…