Spectral characteristics of wind-generated waves in labortaory are pre
sented on the basis of a systematic measurement in a large-scale wind-
wave channel and compared with those in the field. A marked characteri
stics of the measured spetra is the existence of secondary spectrum-pe
ak. The dependence of spectral peak-frequency, peak-value and zeroth-o
rder moment on wind speed and fetch are presented and found roughly si
milar to those in the field represented by the JONSWAP spectrum, regar
dless of the differences in coefficient. The spectral slope beta at hi
gh-frequencies are found somewhat greater than those of field wind-wav
es in both cases of deep and shallow waters. Except for the low-freque
ncy part, the spectral forms measured in different wind conditions are
similar and fit for the JONSWAP spectrum with gamma = 6 and beta = 5.
5. Some relevant problems are discussed.