Differences in temperature between air and water influence the stabili
ty of the atmospheric boundary layer. The altered structure of the bou
ndary can affect the rate of growth of surface gravity waves. An exten
sive data set, collected under a wide range of well-documented atmosph
eric stability conditions, is investigated to quantify this effect. It
is found that in unstable conditions, wind wave growth is enhanced, w
hereas in stable conditions, it is reduced. A correction, which can be
applied to common fetch-limited growth curves, is developed which can
account for atmospheric stability. In extreme cases, the error (in te
rms of energy) introduced by the neglect of stability effects can be a
s much as 50%. (C) 1998 Elsevier Science B.V. All rights reserved.