“…Here, ice is the radius of the iced conductor, m; h is the heat-exchange coefficient [18], W/(m 2 ⋅K); oi is the outer surface temperature of the ice layer [18], ∘ C; air is the ambient temperature, ∘ C; ice is the density of ice, kg/m 3 ; f is the latent heat for melting ice ( f = 335,000 J/kg); m is the volume of melted ice per unit length, m 2 ; ice is the volume of the ice layer per unit length, m 2 ; ice is the specific heat of ice, J/(kg⋅ ∘ C); and ice is the temperature of the ice layer, which can be simplified as ( oi /2air ) [18], ∘ C. The entire equation can be expressed as…”