Black Sea coastal forecasting system

Abstract. The Black Sea coastal nowcasting and forecasting system was built within the framework of EU FP6 ECOOP project for five regions: the south-western basin along the coasts of Bulgaria and Turkey, the North-Western shelf along the Romanian and Ukrainian coasts, coastal zone around of the Crimea peninsula, the north-eastern Russian coastal zone and the coastal zone of Georgia. The system operates in the real-time mode during the ECOOP project and afterwards. The forecasts include temperature, salinity and current velocity fields. Ecosystem model operates in the off-line mode near the Crimea coast.

Download Full-text

THE CURRENT STATE OF THE BLACK SEA COASTAL GEOSYSTEMS IN THE NORTH-EASTERN SECTOR

Proceedings of International Conference "Managinag risks to coastal regions and communities in a changinag world" (EMECS'11 - SeaCoasts XXVI) ◽

10.31519/conferencearticle_5b1b945b3276d5.19077995 ◽

2017 ◽

Author(s):

Eugeny Godin ◽

Yury Goryachkin ◽

Vyacheslav Dolotov ◽

...

Keyword(s):

Observational Data ◽

Coastal Zone ◽

Black Sea ◽

The State ◽

The Black Sea ◽

Integrated Analysis ◽

Eastern Sector ◽

The North ◽

Current State ◽

North Eastern

This work is a multi-disciplinary research aimed to develop common approaches to estimating the current state and forecasting evolution of coastal geosystems. From 2010 to now, the state of coastal zone geosystems of the Crimean and Caucasian Russian coast has been studied. The research tasks are solved using up-to-date IT based integrated analysis of historical and new observational data.

Download Full-text

LONG-TERM MONITORING OF SEASONAL AND INTERANNUAL VARIABILITY OF HYDROLOGICAL STRUCTURE IN COASTAL ZONE OF THE NORTH-EASTERN BLACK SEA

Proceedings of International Conference "Managinag risks to coastal regions and communities in a changinag world" (EMECS'11 - SeaCoasts XXVI) ◽

10.21610/conferencearticle_58b4317195e3a ◽

2017 ◽

Author(s):

O. Podymov ◽

N. Kuzevanova ◽

A. Khvorosch ◽

...

Keyword(s):

Coastal Zone ◽

Black Sea ◽

Hydrogen Sulphide ◽

Sea Water ◽

The Black Sea ◽

Homogeneous Layer ◽

Marmara Sea ◽

The North ◽

North Eastern ◽

North Eastern Part

The work demonstrates the results of the 6-years complex ship-borne monitoring of coastal zone in the north-eastern part of the Black Sea, carried out by the Southern Branch of P.P.Shirshov Institute of Oceanology, RAS, on a marine cross-section at the Blue Bay (Gelendzhik) beam 1-2 times per month. Climatic changes and eutrophication exert a significant impact on the sea water at the coastal area. In case of the Black Sea these factors pile up with a permanent hydrogen sulphide contamination of the sea water below 80-200 meters depth (depending on the season and distance from the shore). Strong pycno-halocline at the depths from 70 to 160 meters, formed due to the inflow of high salinity water from the Marmara Sea, inhibits the mixing between the water layers and, as a result, also limits the oxygen transport into the deeper layers. The winter cooling reduces the pycno-halocline and enriches the top active layer, down to the cold intermediate layer (CIL), with oxygen and nutrients, which subsequently lead to a vernal phytoplankton bloom. Formation of the thermocline and upper quasi-homogeneous layer (UQL), caused by the water warming in spring, at large extent determines a thickness of phytoplankton-rich layer during the spring and summer seasons. The work demonstrates seasonal and interannual dynamics of the UQL, thermocline, CIL and hydrogen sulphide boundary position in the coastal zone of the north-eastern part of the Black Sea.

Download Full-text

LONG-TERM MONITORING OF SEASONAL AND INTERANNUAL VARIABILITY OF HYDROLOGICAL STRUCTURE IN COASTAL ZONE OF THE NORTH-EASTERN BLACK SEA

Proceedings of International Conference "Managinag risks to coastal regions and communities in a changinag world" (EMECS'11 - SeaCoasts XXVI) ◽

10.31519/conferencearticle_5b1b93b554e1b8.09734764 ◽

2017 ◽

Author(s):

O. Podymov ◽

N. Kuzevanova ◽

A. Khvorosch ◽

...

Keyword(s):

Coastal Zone ◽

Black Sea ◽

Hydrogen Sulphide ◽

Sea Water ◽

The Black Sea ◽

Homogeneous Layer ◽

Marmara Sea ◽

The North ◽

North Eastern ◽

North Eastern Part

The work demonstrates the results of the 6-years complex ship-borne monitoring of coastal zone in the north-eastern part of the Black Sea, carried out by the Southern Branch of P.P.Shirshov Institute of Oceanology, RAS, on a marine cross-section at the Blue Bay (Gelendzhik) beam 1-2 times per month. Climatic changes and eutrophication exert a significant impact on the sea water at the coastal area. In case of the Black Sea these factors pile up with a permanent hydrogen sulphide contamination of the sea water below 80-200 meters depth (depending on the season and distance from the shore). Strong pycno-halocline at the depths from 70 to 160 meters, formed due to the inflow of high salinity water from the Marmara Sea, inhibits the mixing between the water layers and, as a result, also limits the oxygen transport into the deeper layers. The winter cooling reduces the pycno-halocline and enriches the top active layer, down to the cold intermediate layer (CIL), with oxygen and nutrients, which subsequently lead to a vernal phytoplankton bloom. Formation of the thermocline and upper quasi-homogeneous layer (UQL), caused by the water warming in spring, at large extent determines a thickness of phytoplankton-rich layer during the spring and summer seasons. The work demonstrates seasonal and interannual dynamics of the UQL, thermocline, CIL and hydrogen sulphide boundary position in the coastal zone of the north-eastern part of the Black Sea.

Download Full-text

THE CURRENT STATE OF THE BLACK SEA COASTAL GEOSYSTEMS IN THE NORTH-EASTERN SECTOR

Proceedings of International Conference "Managinag risks to coastal regions and communities in a changinag world" (EMECS'11 - SeaCoasts XXVI) ◽

10.21610/conferencearticle_58b43163e44fb ◽

2017 ◽

Author(s):

Eugeny Godin ◽

Yury Goryachkin ◽

Vyacheslav Dolotov ◽

...

Keyword(s):

Observational Data ◽

Coastal Zone ◽

Black Sea ◽

The State ◽

The Black Sea ◽

Integrated Analysis ◽

Eastern Sector ◽

The North ◽

Current State ◽

North Eastern

This work is a multi-disciplinary research aimed to develop common approaches to estimating the current state and forecasting evolution of coastal geosystems. From 2010 to now, the state of coastal zone geosystems of the Crimean and Caucasian Russian coast has been studied. The research tasks are solved using up-to-date IT based integrated analysis of historical and new observational data.

Download Full-text

EXTREME WAVES IN THE NORTH-EASTERN PART OF THE BLACK SEA

Vestnik Yuzhnogo nauchnogo tsentra ◽

10.23885/1813-4289-2007-3-1-22-27 ◽

2007 ◽

Vol 3 (1) ◽

pp. 22-27

Author(s):

B.V. Divinsky ◽

◽

O.V. Pushkarev ◽

Keyword(s):

Black Sea ◽

The Black Sea ◽

Extreme Waves ◽

The North ◽

North Eastern ◽

North Eastern Part

Download Full-text

Verruca stroemia and Verruca spengleri (Crustacea: Cirripedia): distribution in the north-eastern Atlantic and the Mediterranean Sea

Journal of the Marine Biological Association of the United Kingdom ◽

10.1017/s0025315403006842h ◽

2003 ◽

Vol 83 (1) ◽

pp. 89-93 ◽

Cited By ~ 4

Author(s):

Paulo S. Young ◽

Helmut Zibrowius ◽

Ghazi Bitar

Keyword(s):

Mediterranean Sea ◽

Black Sea ◽

Geographic Distribution ◽

Deep Water ◽

Southern Spain ◽

The Black Sea ◽

The North ◽

North Eastern ◽

The Mediterranean ◽

Gorringe Bank

The geographic distribution of Verruca stroemia and V. spengleri are reviewed. Verruca stroemia ranges from the White, Barents, Norwegian, and North Seas south to Portugal to the Algarve and to Gorringe Bank. All of the records of this species from the Mediterranean Sea are considered to be V. spengleri. Verruca spengleri occurs in the Azores and Madeira archipelagos, in southern Spain (Cádiz), throughout the Mediterranean Sea from Gibraltar to Lebanon, and in the Black Sea. But a distinct deep-water Verruca species seems to occur in the deep Mediterranean.

Download Full-text

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

Materials Science Forum ◽

10.4028/www.scientific.net/msf.931.790 ◽

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.

Download Full-text