Abstract: A pair of hot wire anemometers in an X-configuration was used in the boundary layer over the sea. Ten runs were analyzed to yield spectra and co-spectra of vertical and downwind components of velocity over a frequency range ...

Abstract: Further support to Kolmogoroff's theory of local isotropy is provided by hot-wire measurements of fluctuations of downwind velocities at a height of 1 to 2 m above the sea surface. The results agree with those obtained ...

Abstract: Measurements of the spectra of fluctuations in wind velocity over the sea sensed by three basically different instruments are described. One comparison shows good agreement between spectra from a thrust anemometer and cup ...