This work deals with the uncertainties invoked in modeling the directi
onality of waves in the calculation of wave-induced toad effects. In t
he short term, modeling of the spreading function defining the wave sh
ort-crestedness is addressed, including the dependence of these functi
ons on the significant wave height. In the tong-term formulations, the
directionality of the wave climate data and its effect on the wave-in
duced loads are discussed. The effect of accounting for directionality
in the long-term formulations is quantified by a modeling factor obta
ined with reference to calculations that do not include wave direction
ality.