During the Holderness Experiment of 1994-1995 and 1995-1996, data were coll
ected by a coastal deployment of an X-band radar with simultaneous deployme
nts of various moored and bottom-mounted wave measurement devices. The rada
r data consist of sequences of images of the sea surface at intervals of 1.
5 h over several months. Three-dimensional wave number-frequency spectra we
re derived from the sequences of captured images using an analysis method d
eveloped by Young et al. [J. Geophys. Res. 90(C1) (1985) 1049]. Some aspect
s of this analysis were refined. An empirical transfer function was derived
relating the radar image spectra to the wave spectra measured by other ins
truments. A new calibration procedure for obtaining wave height from the ra
dar spectra was also derived. The radar spectra were compared with directio
nal spectra collected by a bottom-mounted InterOcean S4DW directional wave-
current meter and with Datawell Waverider data. The capabilities of X-band
radar in a coastal situation are discussed including the derivation of wate
r depth required to optimise the analysis. (C) 2001 Elsevier Science B.V. A
ll rights reserved.