Abstract

The results of supervisions under the wind heaving in the shallow zone of reservoirs are given. The role of morphometry in the wave’s height formation process is shown. It is given also the coherence among the shores processing parameters, wave’s energy and the coefficients, which characterize the influence of the coastline’s morphometry.

Keywords: shoals, shallow zone, soundings, water reservoir, shores destroying, the Kama reservoir, wind heaving, waves, wave’s energy, the morphometry of coastline, the process of shore’s formation, types of shoals