Abstract
This paper reports some results of a study of the effect of variation of salinity and air temperature on surface zone behavior in a laboratory tabk. The data shiws that the boundary between surface and gradient zones moves down as a result of increasing aslinity in the surface zone. The effect of daily imbient air temperature change over the range studied on flunctuation of boundary level between the surface and gradient zones can be negligible when the effect of wind and evaporation is fairly small. Wind and evaporation from surface water play an important role in the above effect. Wind and evaporation from surface water play an important role in the above effect.
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