We present Monte Carlo radiative transfer models for B335, S140, and rho Op
hiuchi A that simulate the emission line arising from the 557 GHz 1(10)-->1
(01) ground-state transition of ortho-(H2O)-O-16. These models reproduce th
e line profiles with a combination of turbulent and macroscopic motions, an
d are consistent with gravitational infall in rho Oph A. We cannot, however
, discriminate infall from outflow for S140. Our models are consistent with
ortho-H2O abundances relative to H-2 of 2 x 10(-8) and 4.5 x 10(-9) in S14
0 and rho Oph A, respectively, and an upper limit of 4 x 10(-6) (3 sigma) i
n B335, assuming the ratio ortho-H-2/para-H-2 = 0.1. We quantify the impact
of dust continuum emission on the derived abundances.