scholarly journals Hazardous Exogenous Geological Processes of Coastal Zone of Azov Sea

Author(s):  
O.V. Ivlieva ◽  
L.A. Bespalova ◽  
A.E. Tsygankova ◽  
S.A. Misirov
Author(s):  
A.G. Shmidko ◽  
◽  
G.A. Shmidko ◽  

The study of the geoecological problems of the coastal zone of the Taganrog Bay is still not given due attention by the administrative authorities. Although it is the deterioration of the geoecological situation that deserves special attention. In this regard, the assessment of the development of modern ecological and geological processes is an urgent task. The coast of the Taganrog Bay has an exceptionally advantageous geographical position, and has a significant natural resource potential, which contributes to the development of various types of economic activities and causes a deep transformation of the natural complex of the coastal zone


Formulation of the problem. According long- term data analyses under the slides zone in Ukrainian part of the Azov sea sustainable processes had been marked. Landslides are most active in autumn and spring. The activation of landslides occurs under the influence of man-made and natural factors. The most significant factor is coastal abrasion. Review of previous publications. It was established that the air temperature and precipitation, the temperature and salinity of sea waters and the hydrometeorological regime of the coastal zone and the water balance of the Black and Azov seas as well depends on climatic changes. The rising of the sea level has intensified over the past decades. These changes found a response in the coastal zone that reacted to them and acquired corresponding trends. Purpose is to determine the reasons for the formation of dynamically unstable sectors and the possibility of protecting the shores on the Ukrainian coast in the Azov Sea, the subject is landslide processes, as the result of the abrasion of the shores, the object is the variability of the natural and anthropogenic conditions of the Ukrainian coast of the Azov Sea in the area of interaction between the sea and land. Methods. Analyses of images space and temporal dynamic of Earth remote sensing satellites by DigitalGlobe, USGS LandLook and Sentinel were used and also retrospective long term of hydrometeorological data and standard statistical methods. Results. The places (areas) with pronounced coastal dynamic processes on the Ukrainian coast of the Azov Sea were identified, that require special attention: two in the Kherson region, five in the Zaporozhye region and four in Donetsk. In the coastal zone of the Azov Sea the rate of abrasion from 1 to 4 m per year (in exceptional cases up to 15 m per year) was marked. In a period of significant level rises, the flooding of ports, berths, the destruction of hydraulic engineering structures, storage facilities, and residential buildings is possible. Also, during the period of the significant decreasing of the sea level, the already limited depth of the approach channels decreases again, that disrupts the operation of the fleet. Conclusions. Investigations of the current state of the Ukrainian coastal zone of the Azov Sea, that is significant importance for the sustainable the economy development, the recreational region’s potential and the social level of the population. It has been established that in the eastern regions of the Azov coast of Ukraine there are a deficit of sediments and a high degree of variability of the abrasion form of the coastal-sea relief is noted, and an excess of sediments are formed in the western and northwestern regions.


Author(s):  
A.D. Khаvanskiy ◽  
◽  
V.V. Latun ◽  
O.A. Khoroshev ◽  
Yu.Yu. Merinova ◽  
...  

The main factors of the formation of hazardous coastal processes have been established, 38 functional areas and a zone of impact of hazardous abrasion and landslide processes predicted for a 20-year period have been identified in the coastal zone of the Azov Sea by their uniform combination in the coastal zone of the Azov Sea. In the forecasted area, 112 socio-economic objects have been identified that are exposed to hazardous abrasion and landslide processes. A methodology has been developed and the socio-economic risk of manifestation of abrasion and landslide processes in the coastal zone of the Azov Sea has been assessed. The highest values of the socio-economic risk of abrasion and landslide processes occur in abrasion and abrasion-landslide areas of the coast with a high speed abrasion, a large number of capital construction projects and a high value of material losses. For socio-economic objects in the risk zone, an enlarged calculation of the possible economic damage was made. The value of the predicted (in the future for 20 years) total economic damage from the consequences of the manifestation of abrasion and landslide processes in the coastal zone of the Azov Sea will amount to 756,7 million rubles, of which 114,4 million rubles will fall on the northern coast of the Taganrog Bay, 156,8 million rubles – to the southern coast of the Taganrog Bay and 485,6 million rubles – to the southeast coast of the Azov Sea. The most dangerous areas of abrasion and landslide processes for capital construction sites are: on the northern shore of the Taganrog Bay – Botsmanovsky, with damage to capital structures – more than 50 million rubles, Zolotokosovsky – more than 16 million rubles; Kuchugurskiy – more than 17 million rubles – on the southeast coast of the Azov Sea.


2004 ◽  
Vol 1 (1) ◽  
pp. 27-85 ◽  
Author(s):  
F. T. Mackenzie ◽  
A. Lerman ◽  
A. J. Andersson

Abstract. The global carbon cycle is part of the much more extensive sedimentary cycle that involves large masses of carbon in the Earth's inner and outer spheres. Studies of the carbon cycle generally followed a progression in knowledge of the natural biological, then chemical, and finally geological processes involved, culminating in a more or less integrated picture of the biogeochemical carbon cycle by the 1920s. However, knowledge of the ocean's carbon cycle behavior has only within the last few decades progressed to a stage where meaningful discussion of carbon processes on an annual to millennial time scale can take place. In geologically older and pre-industrial time, the ocean was generally a net source of CO2 emissions to the atmosphere owing to the mineralization of land-derived organic matter in addition to that produced in situ and to the process of CaCO3 precipitation. Due to rising atmospheric CO2concentrations because of fossil fuel combustion and land use changes, the direction of the air-sea CO2 flux has reversed, leading to the ocean as a whole being a net sink of anthropogenic CO2. The present thickness of the surface ocean layer, where part of the anthropogenic CO2 emissions are stored, is estimated as of the order of a few hundred meters. The oceanic coastal zone net air-sea CO2 exchange flux has also probably changed during industrial time. Model projections indicate that in pre-industrial times, the coastal zone may have been net heterotrophic, releasing CO2 to the atmosphere from the imbalance between gross photosynthesis and total respiration. This, coupled with extensive CaCO3 precipitation in coastal zone environments, led to a net flux of CO2 out of the system. During industrial time the coastal zone ocean has tended to reverse its trophic status toward a non-steady state situation of net autotrophy, resulting in net uptake of anthropogenic CO2 and storage of carbon in the coastal ocean, despite the significant calcification that still occurs in this region. Furthermore, evidence from the inorganic carbon cycle indicates that deposition and net storage of CaCO3 in sediments exceed inflow of inorganic carbon from land and produce CO2 emissions to the atmosphere. In the shallow-water coastal zone, increase in atmospheric CO2 during the last 300 years of industrial time may have reduced the rate of calcification, and continuation of this trend is an issue of serious environmental concern in the global carbon balance.


2021 ◽  
Vol 26 (1(38)) ◽  
pp. 11-27
Author(s):  
N. A. Berlinskyi ◽  
R. V. Gavriluk ◽  
M. A. Sahaidak

Azov is freezing sea it means that forecast of the time of the beginning and the end of ice fields formation needs. The ice condition limited of maritime safety. Modern condition of ice regime in the Azov Sea has been considered. The navigation of the Ukrainian ports Berdjansk and Mariupol depends on ice regime, duration and ice cover thickness. For the passage of vessels along the sea approach channels and recommended courses in the winter, the use of icebreakers is required. The demolition of confining buoys by ice fields and their restoration is reflected in the economic opportunities of the ports. Purpose of the article is to establish the characteristic winter periods of the last decade, taking into account the climatic changes for the rational using of the results of the impact on the economic activity of the marine infrastructure and hydrographic services. The specific purpose of this publication is to evaluate the displacement of the means of navigation equipment – buoys in the winter, taking into account meteorological factors. The authors set the following tasks: 1) to identify periods and vectors of buoys; 2) to define wind and ice characteristics in separate periods; 3) to reveal the basic meteorological cause of the movement of the buoys. It is important to note that there are no similar publications concerning this region. It became very actual after the climate change period was marked. The reserach is based on the data of direct and remote observations, the dates of ice formation in the area of seaports of Ukraine (Berdyansk and Mariupol) the characteristics of ice, the end of freezing, the opening and clearing of ice from the water areas of ports and bays and using the information from NAVTEX warning system, the archival materials of the weather site meteo.ua. The features of the physicochemical properties of sea water during ice formation and the general circulation of the waters of the Azov Sea are examined, which is linked with the influence of fresh runoff of Don and Kuban rivers. In the period 2013–2021 the observations were made on the displacement of navigation aids (buoys) during the winter periods from the approach channels of the port of Mariupol and Berdjansk as well as noticed buoys from the Azov-Don Marine Channel (Russian Federation). The characteristic of winter periods and conditions during the last decade are considered taking into account the influence of climatic changes. It is noted that the ice regime of the Sea of Azov is closely related with the sum of average daily air tem peratures over the sea for the season and wind power. According to this criterion, winters are usually divided into three types: severe, moderate and mild. Over the past 30 years, there were only two severe winters in the Azov Sea in 2005–2006 and 2011–2012. During these winters, the Azov Sea was completely ice covered. The influence of the ice regime to the coastal zone was examined, because it is very important for the industrial and economic needs of state building. To maintain the safety of navigation and reduce economic losses, it is necessary to consider the possibility of removing buoys, which are most often displaced by ice drift. Long-term average observations indicate the beginning of ice formation in Mariupol on December 14, and in Berdyansk on December 20. The Taganrog Bay and the ice accumulation areas are cleared of ice most recently – March 20–28. Under modern climatic changes (increasing the frequency of mild winters, actual costs for the operation of ships, hydrographic, icebreakers, etc.) are expected to be an order of magnitude lower than standard indicators.


Author(s):  
Anatoly Filobok ◽  
Anatoly Filobok ◽  
Tatiana Volkova ◽  
Tatiana Volkova ◽  
Vera Minenkova ◽  
...  

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.


Author(s):  
Lyudmila Bespalova ◽  
Lyudmila Bespalova ◽  
Olga Ivlieva ◽  
Olga Ivlieva ◽  
Alla Tsygankova ◽  
...  

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.


2020 ◽  
Vol 175 ◽  
pp. 06008 ◽  
Author(s):  
Alexander Khavansky ◽  
Vladimir Latun ◽  
Oleg Khoroshev ◽  
Yuliya Merinova ◽  
Ludmila Nedoseka

The methodology was developed and the socio-economic risk of the manifestation of abrasion and landslide processes in the coastal zone of the Azov Sea was evaluated. The methodology includes assessing the degree of danger of coastal processes and determining possible material losses. The numerical index of socio-economic risk is calculated as the product of point estimates of these parameters. The main factors of dangerous coastal processes formation have been established, according to their similar combination in the coastal zone of the Azov Sea, 42 functional areas and the impact zone of hazardous abrasion and landslide processes predicted for a 20-year period have been identified. In the forecast zone, 112 socio-economic objects were identified that are subject to the influence of dangerous abrasion and landslide processes. For these socio-economic objects, using the standard set of tools of the public GIS service “Cadastral map of Rosreestr”, an enlarged calculation of possible economic damage has been made. The highest values of the socio-economic risk of the manifestation of abrasion and landslide processes in the coastal zone of the Azov Sea fall on abrasion and abrasion-landslide sections of the coast with a high rate of abrasion, a large number of capital construction projects and a high value of material losses.


Hacquetia ◽  
2016 ◽  
Vol 15 (2) ◽  
pp. 79-104 ◽  
Author(s):  
Vitaliy Коlomiychuk ◽  
Denys Vynokurov

Abstract Syntaxonomy of the class Festuco-Brometea in Ukraine has barely been still explored. There are some scattered and local data, mainly within the Forest-Steppe zone, which need to be compiled and critically reviewed. Similarly, the Azov Sea coastal zone, which, despite the considerable diversity of habitats, remains unstudied phytosociologically. We have carried out large-scale comparisons of relevés from the Sea of Azov coastline with data from other regions of Ukraine, Europe, and Russia. In total, 2336 relevés were used for the analysis. For the analysis, Modified TWINSPAN classification was used. Diagnostic species were determined by means of the phi fidelity index. In total, 9 associations and 4 subassociations, belonging to four alliances, were identified and categorised as follows: Artemisio-Kochion prostratae (ruderalized steppes), Artemisio tauricae- Festucion valesiacae (saline steppe vegetation on sites affected by the sea or saline ground water), Stipo lessingianae-Salvion nutantis (forb-bunchgrass steppe vegetation) and Tanaceto millefolii-Galatellion villosae (bunchgrass steppes). The last alliance is proposed as a new one.


Sign in / Sign up

Export Citation Format

Share Document