The aim of this paper is to test the effectiveness of feature models i
n ocean acoustic forecasting. Feature models are simple mathematical r
epresentations of the horizontal and vertical structures of ocean feat
ures (such as fronts and eddies), and have been used primarily for ass
imilating new observations into forecasts and for compressing data. In
this paper we describe the results of experiments in which the models
have been tested in acoustic terms in eddy and frontal environments i
n the Iceland Faeroes region. Propagation-loss values were obtained wi
th a 2D parabolic-equation (PE) model, for the observed fields, and co
mpared to PE results from the corresponding feature models and horizon
tally uniform (range-independent) fields. The feature models were foun
d to represent the smoothed observed propagation-loss field to within
an rms error of 5 dB for the eddy and 7 dB for the front, compared to
10-15-dB rms errors obtained with the range-independent field. Some of
the errors in the feature-model propagation loss were found to be due
to high-amplitude 'oceanographic noise' in the field. The main conclu
sion is that the feature models represent the main acoustic properties
of the ocean but do not show the significant effects of small-scale i
nternal waves and finestructure. It is recommended that feature models
be used in conjunction with stochastic models of the internal waves,
to represent the complete environmental variability.