  We present here an empirical method aimed at decreasing the error in the
significant wave height calculated through the Wave Watch model. The errors are
calculated as the difference between the modeled and the locally observed
measurement. We hypothesize that this error would be reduced if the model used
a well calibrated method to account for thermal variations within the surface
boundary layer. We compared then this error for 2015 to the air sea temperature
difference in order to find a potential relationship among them. The
statistical analysis performed show a clear correlation between these
variables, hinting for the need of introducing a correction for stability based
on a linear relationship between the error and the air ocean temperature
difference.
