MODERN ABRASION PROCESSES OF THE AZOV SEA COAST

2017 ◽  
Author(s):  
Lyudmila Bespalova ◽  
Lyudmila Bespalova ◽  
Olga Ivlieva ◽  
Olga Ivlieva ◽  
Alla Tsygankova ◽  
...  
Keyword(s):  
Storm Surges ◽  
Anthropogenic Factors ◽  
Geological Processes ◽  
Azov Sea ◽  
Natural And Anthropogenic Factors ◽  
Sea Coast

The Azov Sea Coast is subjected to a complex of hazardous exogenous geological processes, landslides and abrasion being the most important ones. Both natural and anthropogenic factors contribute to the development and intensification of these processes. These processes are currently growing due to an increased frequency of storm surges.

MODERN ABRASION PROCESSES OF THE AZOV SEA COAST

2017 ◽  
Author(s):  
Lyudmila Bespalova ◽  
Lyudmila Bespalova ◽  
Olga Ivlieva ◽  
Olga Ivlieva ◽  
Alla Tsygankova ◽  
...  
Keyword(s):  
Storm Surges ◽  
Anthropogenic Factors ◽  
Geological Processes ◽  
Azov Sea ◽  
Natural And Anthropogenic Factors ◽  
Sea Coast

The Azov Sea Coast is subjected to a complex of hazardous exogenous geological processes, landslides and abrasion being the most important ones. Both natural and anthropogenic factors contribute to the development and intensification of these processes. These processes are currently growing due to an increased frequency of storm surges.

ESTIMATION OF RECREATIONAL POTENTIAL BASED ON THE DYNAMIC PROCESSES, NATURAL AND ANTHROPOGENIC FACTORS

2017 ◽  
Author(s):  
Anatoly Filobok ◽  
Anatoly Filobok ◽  
Tatiana Volkova ◽  
Tatiana Volkova ◽  
Vera Minenkova ◽  
...  
Keyword(s):  
Coastal Zone ◽  
Black Sea ◽  
Anthropogenic Factors ◽  
Dynamic Processes ◽  
Geological Processes ◽  
Natural Factors ◽  
Black Sea Coast ◽  
Krasnodar Region ◽  
Natural And Anthropogenic Factors ◽  
Sea Coast

This article is devoted to the estimation of recreational potential based on the dynamic processes, natural and anthropogenic factors of the Azov-Black Sea coast of Krasnodar region as an example. Bioclimatic figures are considered as the dynamic processes and natural factors, the degree of the development of exogenous geological processes. Anthropogenic factors are represented by the multi aspect business activities in the coastal zone.

ESTIMATION OF RECREATIONAL POTENTIAL BASED ON THE DYNAMIC PROCESSES, NATURAL AND ANTHROPOGENIC FACTORS

2017 ◽  
Author(s):  
Anatoly Filobok ◽  
Anatoly Filobok ◽  
Tatiana Volkova ◽  
Tatiana Volkova ◽  
Vera Minenkova ◽  
...  
Keyword(s):  
Coastal Zone ◽  
Black Sea ◽  
Anthropogenic Factors ◽  
Dynamic Processes ◽  
Geological Processes ◽  
Natural Factors ◽  
Black Sea Coast ◽  
Krasnodar Region ◽  
Natural And Anthropogenic Factors ◽  
Sea Coast

This article is devoted to the estimation of recreational potential based on the dynamic processes, natural and anthropogenic factors of the Azov-Black Sea coast of Krasnodar region as an example. Bioclimatic figures are considered as the dynamic processes and natural factors, the degree of the development of exogenous geological processes. Anthropogenic factors are represented by the multi aspect business activities in the coastal zone.

AN ARTIFICIAL BEACH AS A MEANS FOR SEA COAST PROTECTION FROM STORM SURGES (BY THE EXAMPLE OF THE EASTERN GULF OF FINLAND)

2017 ◽  
Author(s):  
Igor Leontyev ◽  
Igor Leontyev ◽  
Tatiana Akivis ◽  
Tatiana Akivis
Keyword(s):  
Storm Surges ◽  
Gulf Of Finland ◽  
Beach Sand ◽  
Medium Sand ◽  
Material Loss ◽  
Beach Width ◽  
Intense Storm ◽  
The Gulf Of Finland ◽  
Beach Volume ◽  
Sea Coast

A model of an artificial beach is suggested for protection of coasts under erosion due to intense storm surges. It is shown that the coarser beach sand results in decrease of the beach width and growth of nourishment volume. At the same time relative material loss due to long-shore sediment transport diminishes too. The model has been applied to three sections of the coasts of Kurortny district of S.-Petersburg (eastern part of the Gulf of Finland). It recommends medium sand for the beaches construction. Modeling of extreme storms effect shows only minor deformations for designed beach profiles. For the beaches more than 1 km long even in 30-50 years more than a half of the initial beach volume conserves without additional nourishment.

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