THE ABRASION-BAY COAST MORPHODYNAMICS UNDER THE DIFFERING INTENSITY OF THE WAVE ACTION (IN TERMS OF THE NORTH KALININGRAD PENINSULA, THE SOUTH-EAST BALTIC)
https://doi.org/10.15356/0435-4281-2016-2-41-40
Abstract
The study is based on estimation of abrasion-embayed coast lithodynamics on the basis of bathymetric data and equilibrium profi le of the underwater coastal slope. Model of R. Dean and model of storm relief deformations were used. Based on the underwater coastal slope relief comparison with Dean’s equilibrium profi le the principles of large-scale regionalization of the coastal zone were put forward. The comparison with storm relief deformations was led to conclude that maximum of relief transformation is occur under extreme heaving and lead to irregular distribution of sandy sediments in the central part of the bay. In the following, these relief transformations are the cause of the intensifi cation of abrasion processes under the less powerful storms.
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For citations:
Korzinin D.V. THE ABRASION-BAY COAST MORPHODYNAMICS UNDER THE DIFFERING INTENSITY OF THE WAVE ACTION (IN TERMS OF THE NORTH KALININGRAD PENINSULA, THE SOUTH-EAST BALTIC). Geomorfologiya. 2016;(2):41-40. (In Russ.) https://doi.org/10.15356/0435-4281-2016-2-41-40
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