Introduction

2016 ◽  
pp. 1-8
Author(s):  
Paul Huddie
Keyword(s):  
Black Sea ◽  
Russian Empire ◽  
The Black Sea ◽  
Western Balkans ◽  
Crimean War ◽  
Black Sea Region ◽  
The North ◽  
The Russian Empire ◽  
North Western

The year 2014 marked the 160th anniversary of the beginning of the Crimean War, 1854–6. It was during that anniversary year that the names of Crimea, Sevastopol, Simferopol and the Black Sea re-entered the lexicon of Ireland, and so did the terms ‘Russian aggression’, ‘territorial violation’ and ‘weak neighbour’. Coincidentally, those same places and terms, and the sheer extent to which they perpetuated within Irish and even world media as well as popular parlance, had not been seen nor heard since 1854. It was in that year that the British and French Empires committed themselves to war in the wider Black Sea region and beyond against the Russian Empire. The latter had demonstrated clear aggression, initially diplomatic and later military, against its perceived-to-be-weak neighbour and long-term adversary in the region, the Ottoman Empire, or Turkey. As part of that aggression Russia invaded the latter’s vassal principalities in the north-western Balkans, namely Wallachia and Moldavia (part of modern-day Romania), collectively known as the Danubian Principalities. Russia had previously taken Crimea from the Ottomans in 1783....

scholarly journals FEATURES OF CHANGES IN THE NUMBER AND DENSITY OF RODENTS IN MOSAIC AGRICULTURAL LANDSCAPE OF NORTH-WESTERN BLACK SEA IN 1961-2016

2017 ◽  
Vol 73 (1) ◽  
pp. 20-24
Author(s):  
S. Sushko ◽  
I. Nakonachnuj
Keyword(s):  
Black Sea ◽  
Agricultural Landscape ◽  
Steppe Zone ◽  
Agricultural Landscapes ◽  
The Black Sea ◽  
Black Sea Region ◽  
The North ◽  
Dry Steppe ◽  
Anthropogenic Development ◽  
North Western

Reflects the results of the stages of the study of bioclimatic and landscape-nanotechnik characteristics of the steppe zone of the North-Western part of the black sea region, as the formation of mosaic agrozootehnice mixed natural agroinnova Genesis. It is recommended to differentiate the dry steppe pjone only the territory South of the interfluve of the Dniester-Dnieper. A retrospective analysis allowed to argue that a significant amount of anthropogenic development in the process of transformation of the steppes into agricultural lands, stimulated a radical break with zonal ecosystems. This transformation of biocenosis occurred against the background of climate aridization and under the influence of anthropogenic actions. A structured approach to analytical generalization allowed to update selected issues and became the basis for the study. The obtained results allowed axiomatic to say about the deterioration of the conditions of existence for the available biotic complex, and also significantly affects the seasonal conditions of existence of rodents in the field of agricultural landscapes, directly and indirectly limiting their population status.

scholarly journals Tendencies of long-term changes of temperature fields, salinity and water level of the North-Western part of the Black Sea

2019 ◽  
pp. 84-94
Author(s):  
N. Berlinsky ◽  
R. Gavriluk ◽  
O. Danilenko
Keyword(s):  
Water Temperature ◽  
Sea Level ◽  
Black Sea ◽  
Temperature Increase ◽  
The Black Sea ◽  
Sea Level Fluctuations ◽  
The North ◽  
Long Term Changes ◽  
North Western

The paper analyzes the variability of hydrological characteristics of the North-Western part of the Black for different temporal scales: long-term, seasonal and synoptic. The traditional methods of geographic investigations, such as comparative-geographic, retrospective and cartographic methods, were used. When analyzing sea level data packages and thermohaline characteristics mathematical methods, including statistical, correlation and regression analysis, were used. As a result of the conducted research quantitative estimates of tendencies of long-term changes of the thermohaline characteristics and level in the North-Western part of the Black Sea were received. Over the period of 1982-2005 an increase of water temperature in the North-Western part of the Black Sea was observed: in winter water temperature in the surface layer increased by 2оC, in the bottom layer – by more than 2оC. Over the period of 1990-2005 an increase of an average annual water temperature in Odesa area constituted 1,2°C. The most considerable and statistically significant temperature increase took place during the summer hydrological season: an average summer temperature increased during this period by 2,7оC. During transitional seasons (autumn and spring) there was also a tendency of temperature increase, however, statistically significant trend was observed only during the autumn period. There is a statistically significant negative trend observed for long-term changes of salinity. For the period of 1990-2005 an average annual salinity decreased by 1.36 ‰. A tendency of salinity decrease was observed for all seasons of the year, however, statistically significant trends are observed only in winter and summer. A close relationship between long-term changes in water salinity and runoff of the Dnieper River was also established. A sea level rise is observed at all stations of the North-Western part of the Black Sea. Over the period of 1947-2012 an average annual sea level in Odesa increased by 14 cm. An analysis of climatic changes of wind-induced sea level fluctuations showed that the frequency of surges of varying intensity remained almost unchanged, however, the frequency of sweeps changed significantly. Over the period of 1980-2012, as opposed to the period of 1947-1979, the frequency of minor sweeps (no more than 30 cm) increased, and the frequency of significant (more than 30 cm) and very significant (more than 50 cm) sweeps, on the contrary, decreased by about 5%-6%. Changes of wind-induced sea level fluctuations' character harmonize with wind direction and wind speed over the North-Western part of the Black Sea.

scholarly journals Long term trends in the sea surface temperature of the Black Sea

Ocean Science ◽  
2010 ◽  
Vol 6 (2) ◽  
pp. 491-501 ◽  
Author(s):  
G. I. Shapiro ◽  
D. L. Aleynik ◽  
L. D. Mee
Keyword(s):  
Surface Temperature ◽  
Sea Surface Temperature ◽  
Black Sea ◽  
Sea Surface ◽  
The Black Sea ◽  
The North ◽  
Sst Variability ◽  
Long Term Trends ◽  
Cooling Trend

Abstract. There is growing understanding that recent deterioration of the Black Sea ecosystem was partly due to changes in the marine physical environment. This study uses high resolution 0.25° climatology to analyze sea surface temperature variability over the 20th century in two contrasting regions of the sea. Results show that the deep Black Sea was cooling during the first three quarters of the century and was warming in the last 15–20 years; on aggregate there was a statistically significant cooling trend. The SST variability over the Western shelf was more volatile and it does not show statistically significant trends. The cooling of the deep Black Sea is at variance with the general trend in the North Atlantic and may be related to the decrease of westerly winds over the Black Sea, and a greater influence of the Siberian anticyclone. The timing of the changeover from cooling to warming coincides with the regime shift in the Black Sea ecosystem.

scholarly journals Amphipod (Crustacea, Amphipoda) Communities in the North-Western Part of the Black Sea

2016 ◽  
Vol 50 (5) ◽  
pp. 387-394
Author(s):  
S. A. Kudrenko
Keyword(s):  
Species Composition ◽  
Community Composition ◽  
Black Sea ◽  
The Black Sea ◽  
Published Data ◽  
Amphipod Species ◽  
Quantitative Parameters ◽  
The North ◽  
North Western

Abstract The data about the community composition, number and biomass of amphipods in three gulfs of the North-Western Black Sea are presented. The amphipod communities of the gulfs of Yahorlyk, Karkinit, and Tendra were studied and the species composition was compared with the previously published data. For each particular gulf, the list of amphipod species was composed. The quantitative parameters of the amphipod communities in the studied localities in different years were described.

scholarly journals The historiography of the Kazakhs’ Junior Horde incorporation into the Russian Empire (the pre-revolutionary period)

2016 ◽  
Vol 5 (4) ◽  
pp. 122-126
Author(s):  
Gulbanu Bolatovna Izbassarova
Keyword(s):  
Black Sea ◽  
18Th Century ◽  
Russian Empire ◽  
The Black Sea ◽  
Character Assessment ◽  
The Russian Empire ◽  
Concept Change ◽  
Academy Of Sciences ◽  
First Time ◽  
Revolutionary Period

The Kazakhs Junior Horde, due to external - internal political reasons was the first one who became the part of Russian Empire. Chinggizid Abulkhair was an initiator of the Kazakh society incorporation into the structure of the Russian Empire. The aggravation of the Kazakh-Bashkir, Kazakh-Kalmyk, Kazakh-Dzungar relations leads to a search for a strong overlord. At the beginning of the 18th century, after the Prut campaign, the interests of the Russian Empire moved from the Black Sea to Asia, which is south-east direction. Formation of the imperial concept, change in the concept of Russias historical mission on the international scene forms new strategic and political aims of the Russian Empire. The Academy of Sciences founded in 1724 by the emperor Peter I as well as representatives of local administrations started to explain to the Russian public the acquisition of new lands policy. The reflection of this event to the Russian historiography of the XVIII-XIX centuries is studied in this article. The attention is paid to the study of a concept of citizenship, an interpretation of its character, assessment of the Kazakh khan Abulkhair, the accession initiator by pre-revolutionary historiography representatives. The article considers views of P.I. Rychkov, A.I. Levshin, who are for the first time in their writings, on the basis of archival, authentic sources, gathered a wealth of factual material, scientifically substantiated opinions on the issue of incorporation.

History of the Russian Empire in the context of theoretical and legal analysis (To the 300th anniversary of the Russian Empire)

2021 ◽  
pp. 186
Author(s):  
Nadezhda S. Nizhnik
Keyword(s):  
The United States ◽  
Russian Empire ◽  
The Arctic ◽  
The Black Sea ◽  
Scientific Conference ◽  
Legal Analysis ◽  
The North ◽  
Internal Affairs ◽  
The Russian Empire ◽  
The Baltic

The review of the XVIII International Scientific Conference "State and Law: evolution, current state, development prospects (to the 300th anniversary of the Russian Empire)" was held on April 29-30, 2021 at the St. Petersburg University of the Ministry of Internal Affairs. The Russian Empire existed on the political map of the world from October 22 (November 2), 1721 until the February Revolution and the overthrow of the Monarchy on March 3, 1917. The Russian Empire was the third largest state that ever existed (after the British and Mongolian Empires): It extended to the Arctic Ocean in the north and the Black Sea in the south, to the Baltic Sea in the west and the Pacific Ocean in the east. The Russian Empire was one of the great powers along with Great Britain, France, Prussia (Germany) and Austria-Hungary, and since the second half of the XIX century – also Italy and the United States. The capital of the Russian Empire was St. Petersburg (1721 - 1728), Moscow (1728 - 1732), then again St. Petersburg (1732 - 1917), renamed Petrograd in 1914. Therefore, it is natural that a conference dedicated to the 300th anniversary of the formation of the Russian Empire was held in St. Petersburg, the former imperial capital. The conference was devoted to problems concerning various aspects of the organization and functioning of the state and law, a retrospective analysis of the activities of state bodies in the Russian Empire. The discussion focused on various issues: the character of the Russian Empire as a socio-legal phenomenon and the subject of the legitimate use of state coercion, the development of political and legal thought, the regulatory and legal foundations of the organization and functioning of the Russian state in the XVIII century – at the beginning of the XX century, the characteristics of state bodies as an element of the mechanism of the imperial state in Russia, the organizational and legal bases of the activities of bodies that manage the internal affairs of the Russian Empire, as well as the image of state authorities and officials-representatives of state power.

Architecture of One-Apsidal Churches of North Black Sea Coast VI-XII c.

2018 ◽  
Vol 931 ◽  
pp. 790-796
Author(s):  
Viktoria V. Pishchulina
Keyword(s):  
Black Sea ◽  
The Black Sea ◽  
Byzantine Empire ◽  
Black Sea Region ◽  
The North ◽  
Black Sea Coast ◽  
The Crimea ◽  
The One ◽  
Sea Coast

A one-apsidal hall church is always a reflection of so-called “vulgar” Christianity, thus revealing the important peculiarities of the spatial culture of the region where it is erected. In this region we can mark two periods when such temples were built: VI-VII c. and X-XII c. The first period is associated with the missionary activity by Byzantine Empire, Antioch, Caucasian Albania which was conditioned by both geopolitical interests (Byzantian Empire, Antioch) and the shift of The Great Silk Way to the north (Caucasian Albania). The second, as the research has shown, is connected with the migration of the peoples of Abkhazia, the abzakhs to this territory in the XII-XIII c. and the development of contacts with the Crimea. In the North Black Sea Region the one-apsidal hall church appears as early as in the VI c. – in the territory of Abkhazia we know about ten such temples. The temples of this type in the area of Big Sochi are dated back to the VII-VIII c. In the first Abhzaian temples we can reveal the influence of denominational centers – Byzantian Empire, Antioch, Caucasian Albania. In the temples of the Black Sea coast of both periods – introduction of the samples from Abkhazia.

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