Abstract
The effect of the wind speed on salt diffusion was studied by observations of the longitudinal distribution of Cl concentration in the surface layer of the Ishikari River, which shows highly stratified flow. The measurements were carried out during the dry season. Also, the time series of Cl concentration in the surface layer of two points in the river course are compared with each other and with the time series of wind speed at the points. This comparison appears to enable the prediction of surface salinity distribution.
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