scholarly journals THE ENERGY POTENTIAL OF BLACK SEA IN ROMANIAN SEASIDE AREA

2021 ◽  
Vol 2021 (2) ◽  
pp. 27-32
Author(s):  
VALENTINA JALAN ◽  
DUMITRU DINU ◽  
RALUCA RĂDULESCU
Keyword(s):  
Black Sea ◽  
Optimal Choice ◽  
The Black Sea ◽  
Marine Geology ◽  
Energy Potential ◽  
Wave Regime ◽  
Capture Process ◽  
Energy Technologies ◽  
Free Data ◽  
Strong Winds

The Black Sea is considered a relatively calm sea, the optimal choice for the capture process is influenced by the wave regime and its peculiarities. This sea is characterized by winds that blow towards land with greater intensity in January causing the sea to be more agitated and with less power in May, June and July, when the sea was the calmest of the year. It should be noted that the frequency of strong winds is 38%, and of those of low speed of 1m/s of only 1.5%. For the collection of oceanographic and meteorological information, data provided by the Gloria platform located in front of Romania’s coast were is used, as well as records from the three offshore buoys anchored in the Romanian seaside area and which are part of the EMSO EUXINUS research infrastructure managed by National Institute for Research and Development on Marine Geology and Geoecology - GeoEcoMar. In addition, free data such as those provided by the site of the research institute Grigore Antipa were easily accessed. Presently there are three fixed platforms in the Black Sea. Wave energy is underexploited, both worldwide and in the Black Sea. The potential of this type of energy is huge, and the environmental impact is low compared to other renewable energy technologies.

Wave energy potential and variability for the south west coasts of the Black Sea: The WEB-based wave energy atlas

2020 ◽  
Vol 154 ◽  
pp. 136-150 ◽  
Author(s):  
Bilal Bingölbali ◽  
Halid Jafali ◽  
Adem Akpınar ◽  
Serkan Bekiroğlu
Keyword(s):  
Black Sea ◽  
Wave Energy ◽  
The Black Sea ◽  
The South ◽  
Energy Potential ◽  
Web Based ◽  
South West ◽  
The Web

scholarly journals ANALYZING FLOW ENERGY POTENTIAL OF THE BOSPHORUS STRAIT

2018 ◽  
pp. 76
Author(s):  
Mehmet Özturk ◽  
Cihan Sahin ◽  
Yalcin Yuksel
Keyword(s):  
Black Sea ◽  
Lower Layer ◽  
The Black Sea ◽  
Sea Of Marmara ◽  
Energy Potential ◽  
Flow Energy ◽  
Strong Current ◽  
Layered Flow ◽  
Current Flows ◽  
Current Energy

Ocean currents represent a potentially notable, currently untapped, reservoir of energy. The regions with strong current velocities such as narrow straits connecting two water bodies exhibit high current energy (power) potential especially where the water depths are relatively shallow (EECA, 2009). The Bosphorus, connecting the Black Sea to the Sea of Marmara, is a typical narrow sea strait that generally exhibits a two-layered flow pattern: the upper layer current flows south towards the Sea of Marmara while the underlying current flows in opposite direction towards the Black Sea (Yüksel et al., 2008). The predominant mechanisms for the upper and lower layer flows are the higher water level of the Black Sea and the denser water of the Sea of Marmara, respectively.

scholarly journals A BEM for the Hydrodynamic Analysis of Oscillating Water Column Systems in Variable Bathymetry

Energies ◽  
2020 ◽  
Vol 13 (13) ◽  
pp. 3403 ◽  
Author(s):  
Kostas Belibassakis ◽  
Alexandros Magkouris ◽  
Eugen Rusu
Keyword(s):  
Boundary Element Method ◽  
Water Column ◽  
Black Sea ◽  
Bottom Topography ◽  
The Black Sea ◽  
Device Performance ◽  
Oscillating Water Column ◽  
Energy Potential ◽  
Hydrodynamic Analysis

In this work, a novel Boundary Element Method (BEM) is developed and applied to the investigation of the performance of Oscillating Water Column (OWC) systems, taking into account the interaction of the incident wave field with the bottom topography. The modelling includes the effect of additional upwave walls and barriers used to modify the resonance characteristics of the device and improve its performance as the U-OWC configuration. Numerical results illustrating the effects of depth variation in conjunction with other parameters—such as chamber dimensions as well as the parameters associated with the turbine and power take-off system—on the device performance are presented and discussed. Finally, a case study is presented regarding the potential installation of an OWC in a selected port site in the Black Sea, characterized by a good wave energy potential, on the coast of Romania.

scholarly journals ASSESSMENT OF THE ENERGY POTENTIAL OF THE WAVES IN THE BLACK SEA

2018 ◽  
Vol 8 (3) ◽  
pp. 5-10
Author(s):  
Carmen Gasparotti ◽  
◽  
Eugen Rusu ◽  
◽  
◽  
...  
Keyword(s):  
Black Sea ◽  
The Black Sea ◽  
Energy Potential ◽  
The Waves

Wave climate in the Black Sea: description and trend evaluation using new ECMWF-ERA5 reanalysis and wave-current interaction.

2021 ◽  
Author(s):  
Salvatore Causio ◽  
Piero Lionello ◽  
Stefania Angela Ciliberti ◽  
Giovanni Coppini
Keyword(s):  
Black Sea ◽  
Wave Spectrum ◽  
Atmospheric Stability ◽  
Wave Model ◽  
Wave Climate ◽  
The Black Sea ◽  
Wave Direction ◽  
Wave Regime ◽  
Sea Temperature ◽  
Discrete Interaction

<p>This study analyzes the evolution of the wave climate in the Black Sea basin in a 31-year long hindcast (1988-2018) performed with the third-generation wave model WaveWatchIII v5.16, forced by the ECMWF-ERA5 reanalysis winds at 30km of spatial resolution and 1-hour frequency. The wave model is implemented on a grid covering the whole Black Sea, with 3km grid step and is off-line coupled with a NEMO based hydrodynamical model. The wave spectrum is discretized using 24 directional sectors, and 30 frequencies, with 10% increment starting from 0.055Hz. The model is implemented to solve deep water processes, following the WAM Cycle4 model physics, with Ultimate Quickest propagation scheme and GSE alleviation, which is implemented in WWIII. Wind input and dissipation are based on Ardhuin et al. (2010), wave-wave interactions are based on Discrete Interaction Approximation. Currents and air-sea temperature difference are provided to the wave model to account for Doppler shift and atmospheric stability above the sea. Model validation and statistical analysis have been carried out to describe the wave climate of the Black sea, considering the following wave fields: significant wave height (Hs), mean wave period (Tm) and mean wave direction. Statistics as Mean, Maximum, 5<sup>th</sup> percentile and 95<sup>th</sup> statistics have been computed to produce monthly climatologies. The work considers also the evaluation of trends for Hs and Tm, and the evaluation of tendency in the occurrence frequency of mean and max fields for Hs and Tm.</p><p>There is no evidence about an overall trend in Hs and Tm, but tendencies can be highlighted in some months and seasons. The most evident trend occurs in Summer on the whole wave spectrum, with reduction of Hs and Tm in the Eastern basin, and increasing in the South-Western basins. Even the evaluation of occurrence frequencies suggests that Black Sea is subjected to a change in the wave regime.</p>

scholarly journals A joint evaluation of wave and wind energy resources in the Black Sea based on 20-year hindcast information

2017 ◽  
Vol 36 (2) ◽  
pp. 335-351 ◽  
Author(s):  
Liliana Rusu ◽  
Daniel Ganea ◽  
Elena Mereuta
Keyword(s):  
Wind Energy ◽  
Black Sea ◽  
Wave Energy ◽  
Energy Resources ◽  
The Black Sea ◽  
Time Interval ◽  
Renewable Energy Resources ◽  
Energy Potential ◽  
Wave Hindcast ◽  
Joint Evaluation

In this study, a joint evaluation of the wind and wave energy over the Black Sea basin is performed for a 20-year time interval. The importance of such a study is enhanced by the fact that the potential of the wave energy cannot be considered high compared to the large oceans, while the wind conditions over the Black Sea can be considered significant in various areas. The wind fields from the U.S. National Centers for Environmental Prediction were used for wind energy estimation. A high resolution wave hindcast database, as resulted from the simulations performed with the Simulating WAves Nearshore model, is used for a detailed analysis of the wave energy potential in the basin of the Black Sea. The reliability of the wave simulation results was increased by means of some data assimilation methodologies. The variability and complementarity of these renewable energy resources was investigated. The analysis showed that there exist some suitable areas for combined wind-wave exploitation.

scholarly journals Comment on “Holocene sedimentation in the southwestern Black Sea: Interplay between riverine supply, coastal eddies of the Rim Current, surface and internal waves, and saline underflow through the Strait of Bosphorus” by O. Ankindinova, A. E. Aksu, R. N. Hiscott [Marine Geology, 420 (2020) 106092]

2020 ◽  
Vol 81 (2) ◽  
pp. 77-88
Author(s):  
Ivan Genov
Keyword(s):  
Phase Change ◽  
Internal Waves ◽  
Black Sea ◽  
The Black Sea ◽  
Marine Geology ◽  
86Sr Ratio ◽  
Ocean Water ◽  
Principle Of Superposition ◽  
The Holocene ◽  
The Stability

Ankindinova et al. (2020) describe a series of hydrological events that have led to sedimentation and stratigraphic variations in the gradual sinking of the Black Sea shelf during the Holocene. A key aspect of the study is the attempt to provide a reliable stratigraphic basis for proving of a transgression in the basin throughout the Holocene. However, the conclusions of this approach run counter to the stratigraphic rules: redeposition and significant hiatus in the transgressive phase change of depth of sediment core location (M05-03P) – principle of superposition; merging of transgressive and regressive deposits into a common stratigraphic unit (contradicts the sequential stratigraphy). For this reason, the stability of the conclusion of Ankindinova et al. (2020) for the totally transgressive Holocene development of the Black Sea is doubtful. In addition, the study is based on the interpretation that the increase in the 87Sr /86Sr ratio is solely dependent on ocean water inflow, which is not always correct for enclosed and semi-enclosed basins.

scholarly journals Genoese Traces in the Black Sea Coast of Turkey’s Forts

X ◽  
2020 ◽  
Author(s):  
Nurhilal Burak
Keyword(s):  
Black Sea ◽  
The Black Sea ◽  
Historical Documents ◽  
Marmara Sea ◽  
Trade Routes ◽  
Black Sea Coast ◽  
Strong Winds ◽  
The Republic ◽  
Sea Coast

The Black Sea is an interior sea and located between Bulgaria, Romania, Moldova, Ukraine, Russia, Georgia and Turkey. The Black Sea flows through the Bosporus and reaches the Marmara Sea. Strong winds and stream has seen in the Black Sea in most of times in a year. Because of that natural bays were preferred while the ports and settlements were established. Republic of Genoa has started to plan the trade routes that will be carried out on the Black Sea coast since the Treaty of Nymphaeum signed in 1261. The settlements of the Genoese colonies along the Black Sea coast were not simultaneous. From 1266 onwards, there had been a growth of about 200 years. They intervened in some of the defense structures in these ports. They have placed their own coat of arms on the walls of the defensive structures they had built or repaired. The information is obtained about the colonies in these ports from the trade records which kept by Genoese (Massaria di Caffa, Massaria di Pera), the maritime maps (portolans) produced in those centuries and the medieval historians. The scope of this paper is to be examined that between Bulgaria and Georgia borders the Black Sea port of Turkey’s remaining strongholds which Genoese used for trade. Historical documents and maps will be used as well. In the light of these methods, the ports used by the Republic of Genoa on the shores of the Black Sea, established colonies and construction activities in the thirteenth - fifteenth centuries will be examined.

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