Field Observation for Spreading of Fuji River Water in the inner part of Suruga Bay
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概要
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The study was carried out to investigate the dynamics of the fresher-water plumes by Fuji River outflow by using the field measurements in the inner pert of Suruga Bay. The Fuji River water spreads over a deep continental slope as a surface-advected plume and extends several km. According to the three dimensional current data collected using shipboard acoustic Doppler current profiler (ADCP), anticyclonic eddy at the river mouth is not generated. It was found that the intrusion of Kuroshio warm water prevented the spreading of the Fuji river water to east area of inner part of bay. Residual current, such as wind driven current or intrusion of the oceanic current, have a strong effect to the fresher-water plume.
- Japan Society of Civil Engineersの論文
Japan Society of Civil Engineers | 論文
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