Abstract. The experimental homogeneous nucleation rate data, J exp (T,S), for water are compared with a steady state Monte Carlo nucleation rate model, J MC (T,S), in which the small cluster energies of formation are determined from a discrete sum of Monte Carlo generated Helmholtz free energy differences, ≤f c (n). This formalism includes the ≥ln(n) term of Fisher, where for the critical water clusters (n* > 20 molecules) we use ≥ = 2.2. It is shown that the ≤f c (n) scale like [T c /T -1] and that the discrete summation over n = 2,3,…8 produces a term that cancels the temperature dependence of the monomer flux factor. The result is a scaled form for the nucleation rate, J scaled (T,S) = J o exp[-(16↓/3)[τ(T c ./T-1)] 3 /(lnS) 2 , where J o = 10 26 cm -3 s -1 and τ = 1.47 (close to the value predicted by liquid water bulk surface tension). This form has the same T dependence as the data of Viisanen, Strey and Reiss and gives an improved prediction for the data of Miller, Kassner and Anderson.