Estimates of the directional wave spectrum have been obtained from a data buoy in the southwest approaches to the British Isles. Four years of simultaneous wave and wind data measured at the data buoy were screened for conditions approaching full development. The observed frequency spectra were made nondimensional using the similarity law of Kitaigorodskii and then averaged over six wind speed classes. Comparisons are made with the Pierson-Moskowitz spectrum for fully developed seas. For wind speeds (at the 10 m level) below 16 m s−1, the average spectrum lies consistently below the Pierson-Moskowitz form, while for higher wind speeds the spectra in the region of the peak have similar values to this spectrum. Similarly, values of the nondimensional wave energy are significantly lower than the Pierson-Moskowitz value for wind speeds less than 16 m s−1. For higher wind speeds, the nondimensional wave energy is close to the Pierson-Moskowitz value. The directional spread was studied using two parame... Abstract Estimates of the directional wave spectrum have been obtained from a data buoy in the southwest approaches to the British Isles. Four years of simultaneous wave and wind data measured at the data buoy were screened for conditions approaching full development. The observed frequency spectra were made nondimensional using the similarity law of Kitaigorodskii and then averaged over six wind speed classes. Comparisons are made with the Pierson-Moskowitz spectrum for fully developed seas. For wind speeds (at the 10 m level) below 16 m s−1, the average spectrum lies consistently below the Pierson-Moskowitz form, while for higher wind speeds the spectra in the region of the peak have similar values to this spectrum. Similarly, values of the nondimensional wave energy are significantly lower than the Pierson-Moskowitz value for wind speeds less than 16 m s−1. For higher wind speeds, the nondimensional wave energy is close to the Pierson-Moskowitz value. The directional spread was studied using two parame...