A new source function which parametrically represents the combined eff
ects of wind forcing, wave-wave interactions and dissipative losses, i
s suggested for the wind wave transport equation. The new source funct
ion has a tan hyperbolic form with four tunable wind dependent coeffic
ients. Its forecast performance for duration limited cases is compared
with that of the conventional source function (viz, the Complimentary
Error Function type) through the numerical integration of the wave tr
ansport equation. With the new source function, the wave height foreca
st errors are found to be < 8% with respect to known wave growth nomog
rams, while the errors are 15-28% for the conventional source function
.