Abstract
The water was released on a small river of the Leningrad region, observations of the water level dynamics and calculations of wave subsidence and discharge transformation were carried out. Also, we compared the wave parameters with the values, which were obtained by using the model of unsteady water movement. Calculations of the flood control were made on the adapted model for the Shirokii Channel and the Khemchik River.
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Schedule a callMore From: IOP Conference Series: Earth and Environmental Science
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