Academic literature on the topic 'Tidal Strait'

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Journal articles on the topic "Tidal Strait"

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Novico, Franto, Evi Hadrijantie Sudjono, Andi Egon, David Menier, Manoj Methew, and Munawir Bintang Pratama. "Tidal Current Energy Resources Assessment in the Patinti Strait, Indonesia." International Journal of Renewable Energy Development 10, no. 3 (2021): 517–25. http://dx.doi.org/10.14710/ijred.2021.35003.

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Indonesia is currently intensively developing its renewable energy resource and targets at least 23% by 2025. As an archipelago country, Indonesia has the potential to benefit from its abundant renewable energy resources from its offshore regions. However, the short tidal range of mixed semi-diurnal and the suitable tidal turbine capacity may hinder marine renewable energy development in Indonesian waters. This paper presents higher-order hydrodynamic numerical models to provide spatial information for tidal current resource assessment of the Patinti Strait. The present study applied the hydrographic and oceanographic method to produce input of the numerical model. Based on the selected simulation analysis, the highest current speed could be identified around Sabatang and Saleh Kecil Island with up to 2.5 m/s in P1 and 1.7 m/s in P4. Besides, the operational hours for the two observation points are 69% and 74.5%, respectively. The results indicate that this location is of prime interest for tidal turbine implementation as an energy source, for medium capacity (300 kW) and high capacity (1 MW).
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Kasajima, Yoshie, and Harald Svendsen. "Tidal features in the Fram Strait." Continental Shelf Research 22, no. 17 (2002): 2461–77. http://dx.doi.org/10.1016/s0278-4343(02)00132-2.

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Pratama, Munawir Bintang, Vengatesan Venugopal, Harman Ajiwibowo, Juventus Welly Ginting, and Franto Novico. "Modelling Tidal Flow Hydrodynamics of Sunda Strait, Indonesia." ILMU KELAUTAN: Indonesian Journal of Marine Sciences 25, no. 4 (2020): 165–72. http://dx.doi.org/10.14710/ik.ijms.25.4.165-172.

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In the past years, Indonesian people put more attention to Sunda Strait located between Java and Sumatra Islands, one of the busiest straits occupied with residential, recreational, fisheries, transportation, industrial and mining activities. Previous works on numerical modelling of tidal flow hydrodynamics of the Sunda Strait have resulted in good agreement against field data; however, the calibration of the models used was not described in detail. This paper presents the process of setting up the model, extensive calibration, validation and prediction of tidal currents for the Sunda Strait. A two-dimensional tidal-driven model is constructed using Delft3D, an open-source developed by Deltares. Four different bathymetry datasets, four different boundary condition configurations, and various bed roughness values are used, and their suitability in predicting tidal water level and current are investigated. It is found that changing the bathymetry and boundary conditions improve the model validation significantly. GEBCO_2019 bathymetry dataset outperforms the Batnas, even though it has a coarser resolution. For boundary conditions, the combination of water level and current velocity results in a better validation compares to using water level or current velocity only. However, the bed roughness shows an insignificant influence in predicting tidal conditions. The averaged current velocity is lower at the Southern than the Northern side of the strait due to a larger cross-section, consequence of deeper water. High tidal currents of magnitude around 2 m.s-1 are seen at the bottleneck of the strait.
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Firdaus, Ahmad M., Guy T. Houlsby, and Thomas A. A. Adcock. "Tidal energy resource in Larantuka Strait, Indonesia." Proceedings of the Institution of Civil Engineers - Energy 173, no. 2 (2020): 81–92. http://dx.doi.org/10.1680/jener.19.00042.

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Medeiros, Carmen, and Bjo¨rn Kjerfve. "Tidal characteristics of the Strait of Magellan." Continental Shelf Research 8, no. 8 (1988): 947–60. http://dx.doi.org/10.1016/0278-4343(88)90056-8.

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Sutherland, Graig, Chris Garrett, and Mike Foreman. "Tidal Resonance in Juan de Fuca Strait and the Strait of Georgia." Journal of Physical Oceanography 35, no. 7 (2005): 1279–86. http://dx.doi.org/10.1175/jpo2738.1.

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Abstract The resonant period and quality factor Q are determined for the semienclosed sea comprising Juan de Fuca Strait, Puget Sound, and the Strait of Georgia. The observed tidal elevation gain and phase change, from the Pacific Ocean to this inland sea, are fitted to the predictions of simple analytic models, which give a resonant period of 17–21 h and a Q of about 2. The low Q value, indicative of a highly dissipative system, is consistent with the need for numerical models for the area to employ large bottom friction coefficients. These include the effects of form drag.
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Orhan, Kadir, Roberto Mayerle, Rangaswami Narayanan, and Wahyu Pandoe. "INVESTIGATION OF THE ENERGY POTENTIAL FROM TIDAL STREAM CURRENTS IN INDONESIA." Coastal Engineering Proceedings, no. 35 (June 23, 2017): 10. http://dx.doi.org/10.9753/icce.v35.management.10.

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In this paper, an advanced methodology developed for the assessment of tidal stream resources is applied to several straits between Indian Ocean and inner Indonesian seas. Due to the high current velocities up to 3-4 m/s, the straits are particularly promising for the efficient generation of electric power. Tidal stream power potentials are evaluated on the basis of calibrated and validated high-resolution, three-dimensional numerical models. It was found that the straits under investigation have tremendous potential for the development of renewable energy production. Suitable locations for the installation of the turbines are identified in all the straits, and sites have been ranked based on the level of power density. Maximum power densities are observed in the Bali Strait, exceeding around 10kw/m2. Horizontal axis tidal turbines with a cut-in velocity of 1m/s are considered in the estimations. The highest total extractable power resulted equal to about 1,260MW in the Strait of Alas. Preliminary assessments showed that the power production at the straits under investigation is likely to exceed previous predictions reaching around 5,000MW.
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Wei, Zexun, Guohong Fang, R. Dwi Susanto, et al. "Tidal elevation, current, and energy flux in the area between the South China Sea and Java Sea." Ocean Science 12, no. 2 (2016): 517–31. http://dx.doi.org/10.5194/os-12-517-2016.

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Abstract. The South China Sea (SCS) and the Java Sea (JS) are connected through the Karimata Strait, Gaspar Strait, and the southern Natuna Sea, where the tides are often used as open boundary condition for tidal simulation in the SCS or Indonesian seas. Tides, tidal currents, and tidal energy fluxes of the principle constituents K1, O1, Q1, M2, S2, and N2 at five stations in this area have been analyzed using in situ observational data. The results show that the diurnal tides are the dominant constituents in the entire study area. The constituent K1 has the largest amplitude, exceeding 50 cm, whereas the amplitudes of M2 are smaller than 5 cm at all stations. The amplitudes of S2 may exceed M2 in the Karimata and Gaspar straits. Tidal currents are mostly of rectilinear type in this area. The semi-major axes lengths of the diurnal tidal current ellipses are about 10 cm s−1, and those of the semidiurnal tidal currents are smaller than 5 cm s−1. The diurnal tidal energy flows from the SCS to the JS. The semidiurnal tidal energy flows from the SCS to the JS through the Karimata Strait and the eastern part of the southern Natuna Sea but flows in the opposite direction in the Gaspar Strait and the western part of the southern Natuna Sea. Harmonic analysis of sea level and current observation also suggest that the study area is located in the antinodal band of the diurnal tidal waves, and in the nodal band of the semidiurnal tidal waves. Comparisons show that the existing models are basically consistent with the observational results, but further improvements are necessary.
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Wei, Z. X., G. H. Fang, R. D. Susanto, et al. "Tidal elevation, current and energy flux in the area between the South China Sea and Java Sea." Ocean Science Discussions 12, no. 6 (2015): 2831–61. http://dx.doi.org/10.5194/osd-12-2831-2015.

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Abstract. The South China Sea (SCS) and the Java Sea (JS) are connected through the Karimata Strait, Gaspar Strait, and the southern Natuna Sea, where the tides are often used as open boundary condition for tidal simulation in the SCS or Indonesian seas. Tides, tidal currents and tidal energy fluxes of the principle constituents K1, O1, Q1, M2, S2 and N2 at five stations in this area have been analyzed using in-situ observational data. The results show that the diurnal tides are the dominant constituents in the entire study area. The constituent K1 has the largest amplitude, exceeding 50 cm, whereas the amplitudes of M2 are smaller than 5 cm at all stations. The amplitudes of S2 may exceed M2 in Karimata and Gaspar Straits. Tidal currents are mostly of rectilinear type in this area. The major semi axis lengths of the diurnal tidal current ellipses are about 10 cm s−1, and those of the semi-diurnal tidal currents are smaller than 5 cm s−1. The diurnal tidal energy flows from the SCS to the JS. The semi-diurnal tidal energy flows from the SCS to the JS through the Karimata Strait and the eastern part of the southern Natuna Sea but flows in the opposite direction in the Gaspar Strait and the western part of the southern Natuna Sea. Harmonic analysis of sea level and current observation also suggest that the study area is located in the loop band of the diurnal tidal waves, and in the nodal band of the semi-diurnal tidal waves. Comparisons show that the existing models are basically consistent with the observational results, but further improvements are necessary.
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Khimchenko, E. E., D. I. Frey, and E. G. Morozov. "Tidal internal waves in the Bransfield Strait, Antarctica." Russian Journal of Earth Sciences 20, no. 2 (2020): 1–6. http://dx.doi.org/10.2205/2020es000711.

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Dissertations / Theses on the topic "Tidal Strait"

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HUNG, LUU QUANG. "NUMERICAL MODELING OF TIDAL EXCHANGE THROUGH THE TSUGARU STRAIT." 京都大学 (Kyoto University), 2012. http://hdl.handle.net/2433/157791.

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Atwater, Joel. "Limitations on tidal-in-stream power generation in a strait." Thesis, University of British Columbia, 2008. http://hdl.handle.net/2429/635.

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In the quest to reduce the release of carbon dioxide to limit the effects of global climate change, tidal-in-stream energy is being investigated as one of many possible sustainable means of generating electricity. In this scheme, turbines are placed in a tidal flow and kinetic energy is extracted. With the goal of producing maximum power, there is an ideal amount of resistance these turbines should provide; too little resistance will not a develop a sufficient pressure differential, while too much resistance will choke the flow. Tidal flow in a strait is driven by the difference in sea-level along the channel and is impeded by friction; the interplay between the driving and resistive forces determines the flow rate and thus the extractible power. The use of kinetic energy flux, previously employed as a metric for extractible power, is found to be unreliable as it does not account for the increased resistance the turbines provide in retarding the flow. The limits on extraction from a channel are dependant on the relationship between head loss and velocity. If head loss increases with the square of the velocity, a maximum of 38% of the total fluid power may be extracted; this maximum decreases to 25\% if head loss increases linearly with velocity. Using these values, the estimated power potential of BC's Inside Passage is 477MW, 13% of previous assessments. If a flow has the ability to divert through a parallel channel around the installed turbines, there are further limits on production. The magnitude of this diversion is a function of the relative resistance of impeded and diversion channels. As power extraction increases, the flow will slow from its natural rate. This reduction in velocity precipitously decreases the power density the flow, requiring additional turbine area per unit of power. As such, the infrastructure costs per watt may rise five to eight times as additional turbines are installed. This places significant economic limitations on utility-scale tidal energy production.
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Hart, Deirdre E. Physical Environmental &amp Mathematical Sciences Australian Defence Force Academy UNSW. "Eco-sedimentological environments of an inter-tidal reef platform, Warraber Island, Torres Strait." Awarded by:University of New South Wales - Australian Defence Force Academy. School of Physical, Environmental and Mathematical Sciences, 2003. http://handle.unsw.edu.au/1959.4/38731.

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This thesis examines functional relationships between the morphologic, hydrodynamic, ecological and sedimentological characteristics of the Warraber reef platform, an inter-tidal reef island system, Central Torres Strait, Australia (10[degrees] 12??? S, 142 [degrees] 49??? E). Hydrodynamic and sediment-transport experiments were conducted on the reef flat using current meters, water level recorders and directional sediment traps. Results showed dominantly SE flows during the dry season and more variable NW to SE flows during the wet season. Topography and reefal water levels modulated the direction and strength of currents and the generation of wind-waves on the reef flat as well as the passage of waves over the reef rim. These hydrodynamic conditions are sufficient to induce significant transport of moderately fast to slow settling sediment (&gt-5.25 symbol psi) on the reef flat, though the platform as a whole is a relatively closed transport system. Carbonate production was estimated based on the key ecological variables of live assemblage distribution and cover. Overall, only 24% of the reef flat was occupied by carbonate-producing organisms. The average estimated carbonate-production rate for the reef was 1.6 kgm -2y-1 (0.07-4.37 kgm-2y-1). Production is dominated by coral (73%), with subordinate proportions contributed by coralline algae (19%). And molluscs, foraminifera and Halimeda (&lt4%) though actual reef-flat sediments did not reflect this potential. Instead, they were dominated by molluscs (35-55%), coralline algae (16-26%), coral (8-13%), Halimeda (7-8%) and foraminifera (5-10%). Differential rates of carbonate to sediment conversion meant the reef-platform sediments were more closely related to the cover of live organisms than to the contribution of carbonate production by each parent organism. The settling properties of the least altered particles of the five commonest constituents were measured and these provided the basis for an eco-sedimentological model of the reef-platform system. Modelled textures were compared to the actual textures, indicating the degree of textural alteration resulting from a combination of biological and physical processes, including sediment production, hydraulic sorting and mechanical breakdown. This analysis, integrated with the hydrodynamic, exposure and other data, was used to determine reef-platform surface-sediment sources, sinks and transport pathways. In using both the textual and constituent compositional properties of sediments, as well as information on local biological and physical processes, the model approach developed offers progress towards an integrative, interdisciplinary analysis of carbonate environments.
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El-Geziry, Tarek Mohamed Ahmed. "Environmental impact assessment and process simulation of the tidal current energy resource in the Strait of Messina." Thesis, University of Edinburgh, 2010. http://hdl.handle.net/1842/4779.

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Interest in exploring renewable energy resources has increased globally, especially with recent worldwide intentions to maintain the global climate. Looking at the oceans as a vast sustainable clean energy resource to satisfy present high humankind energy demands has been strongly recommended. Several types of renewable energy resources exist in the oceans: waves, tides, thermal and salinity variations, currents, and offshore winds. Exploiting tidal currents is considered one of the most effective approaches to the generation of electricity. Tidal turbines are deployed beneath the sea surface to transfer the kinetic energy in tidal currents to mechanical energy suitable for ongoing conversion to electricity and subsequent transmission. However, choosing a suitable site to deploy these turbines is not a trivial process. Various constraints must be satisfied subject to basic criteria dependent upon local factors, technology limitation and economic consideration. In addition, an important issue to consider is taking care to harness energy from tidal currents with minimum possible impact on the surrounding environment. The present study justifies the nomination of the Strait of Messina as an exceptional tidal current energy resource within the Mediterranean Sea basin. The maximum tidal current velocity at spring peak tide through the Strait may exceed 3 m/s. This mainly results from the tidal phase-difference (180°) between the northern (Tyrrhenian Sea) and southern (Ionian Sea) tips of the Strait, associated with a difference of 0.27 m in tidal wave amplitudes. In addition, the complex coastline configuration of the Strait plays an important role in enhancing tidal current velocities. Therefore, the Strait of Messina fulfils the basic criterion (2 m/s tidal current velocity) to be considered as a valid tidal current energy resource. This massive tidal current energy resource is assessed in the present study. A detailed full desk-based Environmental Impact Assessment (EIA) study is performed using the interactive matrix approach in order to investigate the anticipated environmental impacts on the marine ecosystem of the Strait of Messina resulting from the harnessing of energy from its tidal currents. Through the EIA study the different environmental components, both biotic and abiotic, which may be affected by the energy extraction process, are explained. In addition, the proposed key project activities are listed; the likelihood of occurrence and the magnitude of impact interaction with the environmental components are evaluated. The final judgment matrix guides to make a right decision on the proposed project. From the resulted matrix, the major impacts do not exceed 10% of the total anticipated effects. The positive point is that all the expected impacts, including the majors, can be controlled and minimised to the lowest possible limits by applying a good monitoring programme. The University of Edinburgh “Tidal Flow Development (TFD)” numerical model is used to mimic the tidal environment of the Strait of Messina in different cases. The model successfully simulates the tidal flow regime within the Strait under some exceptional conditions. Modifications to the main numerical code and coefficients were necessary in the present research to adjust the model according to each case study. In the three different cases of simulation, using these exceptional coefficients, the model simulates the main tidal characteristics of the tidal flow within the Strait. According to the results of the numerical simulation process, tidal currents are more intensive close to the eastern coast of the Strait of Messina near to Punta Pezzo. This area is far from any ferry route between Italy and Sicily. The best location to deploy tidal turbines for the energy extraction process is therefore recommended to be within these surroundings. Finally, a physical (laboratory) model is used to simulate the flow regime within the Strait of Messina. The Particle Image Velocimetry (PIV) technique was applied in the flow-table tank at the University of Edinburgh. The physical model simulates the flow behaviour within the Strait of Messina to a satisfactory degree. The cyclonic and anti-cyclonic motions observed at the southern extremity of the Strait are also very well simulated. The results of the present study assure confidence in the use of tidal currents within the Strait of Messina as a renewable energy resource. The safety of the environment must be ensured by following environmental guidelines, respecting the energy extraction limits and by applying an effective monitoring programme. The later is strongly recommended to be an adaptive one in which higher environmental authorities are able to watch, revise and control the environmental team within the project. These authorities are also able to postpone the project in case of any severe environmental case. The simulation processes emphasize the effect of morphometry and topography in enhancing tidal currents in the Strait of Messina. Moreover, numerical simulation assures that the complex morphometry and bathymetry, in addition to the open boundaries of the Strait of Messina, are challenging issues for modellers in order to mimic the real tidal current resource in the case of the Strait of Messina. The study also strongly recommends applying a more effective numerical model than TFD to assess the tidal hydrodynamical environment before and after any proposed energy extraction process. This will certainly, with the EIA of the marine ecosystem, help to make a right decision about the proposed project in order to achieve the goal of using clean and clear renewable energy resources while maintaining both natural and hydrodynamical environments to the most possible safest degree.
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Evans, Paul Stephen. "Hydrodynamic characteristics of macrotidal straits and implications for tidal stream turbine deployment." Thesis, Cardiff University, 2014. http://orca.cf.ac.uk/70531/.

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National efforts to reduce energy dependency on fossil fuels have prompted examination of macrotidal nearshore zones around the UK for potential tidal stream resource development. Although a number of prospective tidal energy sites have been identified, the local hydrodynamics of these sites are often poorly understood. Tidal-energy developers rely on detailed characterisation of tidal energy sites prior to device field trials and installation. Although first-order appraisals may make macrotidal tidal straits appear attractive for development, detailed, site-specific hydrodynamic and bathymetric surveys are important for determining site suitability for tidal stream turbine (TST) installation. Understanding the ways in which coastal features affect tidal velocities at potential TST development sites will improve identification and analysis of physical constraints on tidal-energy development. Ramsey Sound (Pembrokeshire, Wales, UK) will soon host Wales’ first TST demonstration project. However, the local hydrodynamics of the sound have been underexamined. Ramsey Sound experiences a marked tidal asymmetry, with local bathymetric features that affect flow fields which are spatially heterogeneous in three dimensions. Using Ramsey Sound as a case study, this thesis has three objectives: (1) to examine the wake created by submerged objects through field- and laboratory-based measurements, (2) to experimentally investigate the effect of submergence on wake development and decay downstream of a conical island, and (3) to develop a TST suitability tool, which examines the effects of velocity, water depth and bed slope on power availability within a macrotidal coastal area. Laboratory experiments have shown that submergence level is an important parameter controlling wake structure and extent, and that changes in submergence level affect both the 3-D flow structure in the near wake and the 2-D far wake of islands. Analysis of physical and hydrodynamic characteristics in Ramsey Sound, including tidal velocities across the swept area of the pilot TST, vertical shear in the stream flow, estimated power output, water depth and bed slope, suggests that the spatial and temporal variability in the flow field may render much of Ramsey Sound unsuitable for tidal power extraction. Although the resource potential depends on velocity and bathymetric conditions that are fundamentally local, many prospective tidal energy sites are subject to similar physical and hydrodynamic constraints. Results of this study can help inform site selection in these complicated, highly dynamic macrotidal environments.
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Edwards, Thomas Edward James. "Plasticity of γ-TiAl alloys". Thesis, University of Cambridge, 2018. https://www.repository.cam.ac.uk/handle/1810/275867.

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Gamma titanium aluminide alloys are emerging as a lightweight replacement to nickel superalloys, with current application in turbine stages of aero-engines, as well as in high performance automobiles and potentially the nuclear industry. The lack of toughness of its two constitutive intermetallic phases, γ-TiAl and α2-Ti3Al, prevents a conventional damage tolerant approach to fatigue lifing. To gain confidence in the use of γ-TiAl alloys and extend the temperature-stress envelope of applicability, the present work aims to achieve an understanding of the development of plasticity and flaw formation during cyclic loading. The general plasticity of a γ-TiAl alloy, Ti-45Al-2Nb-2Mn(at.%)-0.8vol.%TiB2, in compression was investigated by mapping the development of localised strain at the specimen surface. Methods were developed to produce speckle patterns for high resolution digital image correlation that were stable at test temperatures of 700 °C in air, in order to study the extent of plasticity generated by differing deformation mechanisms at application-relevant temperatures, with nano-scale resolution. At the colony scale (i.e. single stacks of co-planar α2-Ti3Al and γ-TiAl lamellae, where each stack is formed from a single high temperature disordered α-TiAl grain), macroscopic deformation bands were observed to develop at only a few percent strain. Within such bands, which propagated across many colonies of differing lamellar orientations, considerable lattice curvature and localised slip and twin operation occurred. This correlated with colony boundary failure in such bands. Twinning of the γ-TiAl phase parallel to the lamellar interfaces, longitudinal twinning, has rarely been studied, despite generalised twinning in equiaxed γ-TiAl grains being known to cause boundary decohesion. Here, the occurrence of longitudinal twinning in both microcompression and polycrystalline testpieces was investigated up to 700 °C by electron backscatter diffraction. The strength of constraint by surrounding lamellar domains was found to be the determining factor in the increased prominence of twinning at 700 °C, and hence determined whether twinning shear-induced flaws formed at colony boundaries. Using the high temperature digital image correlation strain mapping and electron backscatter diffraction techniques developed, along with transmission electron microscopy, the onset of plasticity at temperatures up to 700 °C was studied in both micro-scale and macro-scale test specimens for different lamellar thicknesses. Testpieces were loaded below the macroscopic yield stress in both monotonic and high cycle fatigue regimes, to 107 cycles, at a tensile stress ratio of R = 0.1. Longitudinal plasticity occurred in most colonies with soft mode lamellar orientations, and was located just 30 - 50 nm from lamellar interfaces. Lamellar refinement caused an increased number of slip bands to develop. In most cases, plastic strains decreased to zero by the colony boundary and strain transfer across such boundaries in high cycle fatigue was rare. At room temperature, the maximum applied stress was found to influence the number of slip bands more than the number of loading cycles.
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Kingston, Kristopher William. "Shear stresses under waves and currents." Thesis, University of British Columbia, 1985. http://hdl.handle.net/2429/25097.

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This study set out to investigate the shear stress behaviour at the bed under combined wave and current action. The intention of the study was to make experimental measurements to determine how wave and current shear stresses combine, so that theoretical models describing the combined flow condition could be proposed. Two types of experiment were conducted, and theoretical models for the combined flow were assessed. One set of experiments attempted to use a shear plate to make direct measurements of the combined flow shear stress, and of the shear stresses for the component waves and steady currents. This approach failed because the large correction terms introduced by the non-uniform wave pressure field could not be accurately estimated. The second set of experiments used a laser doppler anemometer to make detailed velocity profile measurements over flat sediment beds. The onset of sediment motion was used as a criterion to carefully control the experiments. It is assumed that the threshold of sediment motion represents a specific shear stress intensity at the bed for sediments of narrow size ranges. As the shear stresses can be determined from the velocity fields under waves and currents, their additive nature under combined flow conditions could be investigated. For each sediment size range, it is shown that the same maximum velocity very near the bed can be used to specify the threshold of sediment motion condition for all flow types, be they under waves, currents, or combined waves and currents. It is also shown that the near-bed velocity under a laboratory wave can be predicted accurately from second order wave theory and that the velocity under a current can be predicted from combining Manning's relation with the universal log velocity law. It is further shown that the near-bed velocity under a combined wave and current can be described by the vectorial addition of the maximum component wave velocity and the average component current velocity. The shear stress for the onset of motion is calculated for the steady current using Manning's relation, for the wave by combining the oscillatory shear stress formula with Kamphuis's rough turbulent friction factor relation, and for the combined wave and current by the simple vectorial addition of the component shear stresses, and is shown to be comparable with Shields's threshold criterion for nearly all conditions tested.<br>Applied Science, Faculty of<br>Civil Engineering, Department of<br>Graduate
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Serrano, Pierre. "Modélisation multi-échelles du comportement mécanique des alliages TiAl pour la prévision de leur tenue en fatigue." Thesis, Toulouse 3, 2020. http://thesesups.ups-tlse.fr/4952/.

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Les alliages à base d'aluminures de titane (TiAl) sont des matériaux légers introduits dans la dernière génération de turboréacteurs pour l'aéronautique civil sous la forme d'aube de turbine basse pression. Ces alliages disposent notamment d'excellentes propriétés mécaniques à haute température et d'une résistance spécifique élevée. Leur utilisation reste cependant délicate du fait de leur faible ductilité et ténacité à température ambiante. Afin de trouver de nouvelles applications à ces matériaux, les deux principaux défis pour les futures générations d'alliage sont l'augmentation de la température d'utilisation et l'amélioration des propriétés en fatigue thermomécanique. Dans cette optique, le présent travail consiste à établir un lien entre la microstructure des alliages TiAl et leur tenue en fatigue. Pour cela, des travaux expérimentaux et numériques sont réalisés à différentes échelles d'intérêt sur les quatre microstructures dites génériques de ces matériaux. Dans un premier volet expérimental, un lien entre microstructure et comportement mécanique cyclique est établi via la réalisation d'essais mécaniques à l'échelle macroscopique (i.e. réponse contrainte-déformation), et d'essais micromécaniques qui permettent d'étudier la répartition de la déformation dans la microstructure. Dans un deuxième volet numérique, un modèle de plasticité cristalline permettant de tenir compte des spécificités des microstructures à structure lamellaire des alliages TiAl est défini. Les comportements mécaniques cycliques des quatre microstructures génériques sont ensuite modélisés via la réalisation de calculs éléments finis sur microstructures virtuelles et homogénéisation numérique. Enfin, cette modélisation est utilisée afin de réaliser une analyse aux Indicateurs de Tenue en Fatigue (ITF). Cette analyse permet de comparer les tenues en fatigue des différentes microstructures et d'identifier les éléments microstructuraux qui pilotent la durée de vie en fatigue pour différents régimes de sollicitation. Les résultats obtenus permettent alors d'effectuer un retour vers la métallurgie en indiquant les zones à renforcer pour améliorer les propriétés en fatigue de futurs alliages<br>Technological advances in aircraft engine design require the use of lightweight materials at increasingly high temperatures. Therefore, intermetallics titanium aluminide alloys based on $\gamma$-TiAl have been introduced in the most recent civil turbo-engines as low pressure turbine blades. To extend the use of this material to other application technologies, new alloys are being developed with enhanced mechanical properties. Particularly, material development teams focus on increasing the working temperature and the fatigue strength. The aim of this work is to study the link between TiAl alloys microstructures and their fatigue strengths. Both experimental and numerical aspects are studied at various scales of interest. To begin with, the cyclic deformation of TiAl generic microstructures is studied experimentally by performing standard testing (i.e. stress-strain response) and micro-scale testing. Then, a crystal plasticity model that can be used to take into account the specific behavior of lamellar colonies is defined. The mechanical behavior of TiAl alloys is thereafter modeled by means of finite element computation on statistically representative microstructures and computational homogenization. Lastly, a Fatigue Indicator Parameters (FIP) analysis is performed to identify the various fatigue hot spot within TiAl microstructures. The results are used to suggest microstructure designs that could improve the fatigue strength of TiAl alloys next generation
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Sung, Yu-Lin, and 宋雨霖. "A Study of Tidal Current in Taiwan Strait." Thesis, 2012. http://ndltd.ncl.edu.tw/handle/96228052516803285099.

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碩士<br>國立臺灣海洋大學<br>海洋環境資訊學系<br>100<br>The Taiwan Strait (TS) is a 180×600 km shelf channel located between Taiwan and China. We analyzed five ADCP acoustic Doppler current profilers (ADCPs), four were deployed along the central part of the TS distributed uniform from Taichung to Wuchung and one was deployed in the Peng-Hu Channel (PHC). The data period is 1999-2001. In the general phase, tidal motions are dominated by barotropic component in TS due to shallow bathymetry and weak stratification. In this study, using in-suit data accompanying with OTPS (OSU Tidal Prediction Software), we found that the barotropic diurnal/semidiurnal tidal motions almost flowed along the topography trend of the strait. The current magnitudes of barotropic diurnal tides were 0.1~ 0.13 m/s in the central part of the TS and PHC. The current magnitudes of barotropic semidiurnal tides eastward decrease in the central part of TS, and the maximum magnitude of semidiurnal barotropic tidal current were observed in the PHC(~ 0.9 m/s), much stronger than that in the central TS. Also, the magnitudes of barotropic tidal currents were enhanced by the rising and nearshore narrow channel in the TS. Meanwhile, the baroclinic diurnal/semidiurnal tidal motions were not significant in the general phase, in TS, and the magnitudes were 30~50% and 20~35% of the magnitudes of the barotropic diurnal/semidiurnal tidal motions, respectively. The baroclinic tides were dominated by first-mode baroclinic tidal motions. The depth-integrated kinetic energy (KE) of the baroclinic tides revealed nearly spring-neap circle. However, KE of baroclinic tides were not only effected by the circle, other external events such as typhoon and eddy in the South Chain Sea could also enhance the KE of the baroclinic tides in the central part in TS. Meanwhile, the time lag (> 50hours) of the KE between the barotropic and baroclinic tides implied that internal tides were remotely generated in the Luzon Strait and subsequently proceeded to TS via South China Sea. Compiling typhoon track、Sea Surface Temperature (SST) and Sea Level Anomaly (SLA), we conclude that the internal tides could be intensified in the presence of horizontal fronts in the northern South Chinese Sea (SCS). The fronts could be produced by the typhoon-induced cold wake or cold eddy. As our observation, the strong mode-1 semidiurnal baroclinic tides were intensified, with a maximum velocity of ~0.27 m/s. The maximum depth-integrated kinetic energy of semidiurnal internal tides after the time of the thermal fronts impact were 1.5~2 times of those in the time of spring tide. And the enhancement of internal tides were the most remarkable in the west of strait (Mainland China side).
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Tsai, Wei-Lin, and 蔡維琳. "Major constituents of tidal currents north of Taiwan Strait." Thesis, 2010. http://ndltd.ncl.edu.tw/handle/21095076407010512259.

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碩士<br>臺灣大學<br>海洋研究所<br>98<br>The volume transport from Taiwan Strait to East China Sea is 50 times more than that from Yangtze River, and the sediments and nutrients from Taiwan Strait to East China Sea is one third of the total. It has a great influence on the water mass exchanging and ecology of Taiwan coast and East China Sea. The research focuses on the major constituents of tidal currents and the volume transport (VT) of the northern Taiwan Strait. Because the of data density previous studies is low in time and space in this region, lacking of long-term and a cross section of the strait actual measurement data, we installed a shipboard ADCP on the TaiMa Ferry that navigates between Keelung and Matsu to measure and to gather along track current velocity data. We obtain 160~280 data sets in different grids after screening sixteen months, and then use Harmonic Analysis to find out along-track tidal amplitude and phase of M2, S2, K1, O1 constituents. The result from Harmonic Analysis showed that M2 is the major constituent and its energy is more than S2, K1 and O1 in our study area. Owing to the low and discontinuous sampling frequency on the fixed station, we can’t distinguish constituents that have similar period and low energy. For example, the relation between Harmonic Analysis result and OSU tidal model (TPXO) result of M2 reach 0.9 shows that most tidal current can be filtered. On the other hand, S2 is affected by M2, K1 and O1 still can’t be filtered correctly due to longer period and lower energy. To have 20% or less error on tidal current constituents, it requires data length of 3, 5 and 3 years for M2, S2 and K1 tides. Use two different methods that TPXO and Harmonic Analysis to remove tidal contribution show 1~3 Sv VT through TWS and VT difference value of to- and return-cruises may be -1~1 Sv. The cause of the difference of VT between to- and return-cruises maybe the influence of wind, but it also implies the inaccuracy of remove tidal contribution. In addition, the northeast of the TS is located at the edge of the Keelung Valley and the east side of TS has a hollow and large variation on topography. This research also suggests the existence of baroclinic tide in these two regions, the associated tidal current amplitudes differ about 5~10 cm/s between upper and lower water level. It means that the result of Harmonic Analysis can never match the result of barotropic tidal model of TPXO.
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Books on the topic "Tidal Strait"

1

Foster, Michael Whitfield. The rise and fall of Cook Strait: A look at the dynamics of New Zealand's unusual tidal system. Michael Foster, 2007.

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Macías, D. The Strait of Gibraltar: A field laboratory to analyze biological response to physical forcing. Nova Science Publishers, 2010.

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Burau, Jon R. Tidal and residual currents measured by an accoustic doppler current profiler at the west end of Carquinez Strait, San Francisco Bay, California, March to November 1988. U.S. Geological Survey, 1993.

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Canada, Service hydrographique du, and Canadian Hydrographic Service, eds. Current atlas : Juan de Fuca Strait to Strait of Georgia =: Atlas des courants : Juan de Fuca strait à strait of Georgia. Canadian Hydrographic Service = Service hydrographique du Canada, 1999.

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M, Bolton, and Canadian Hydrographic Service, eds. Current atlas: Juan de Fuca Strait to Strait of Georgia = Atlas des courants : Juan de Fuca Strait à Strait of Georgia. Canadian Hydrographic Service, Dept. of Fisheries and Ocean, 1999.

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Fisheries, Canadian Minister of. Current Atlas: Juan de Fuca Strait to Strait of Georgia. Canadian Hydrographic Office, 1999.

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Canada. Ministry of Fisheries and Oceans. Canadian Hydrographic Service., ed. Current atlas =: Atlas des courants : Juan de Fuca Strait to Strait of Georgia. Canadian Hydrographic Service, 1999.

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The Currents in Belle Isle Strait: From investigations of the tidal and current survey in the seasons of 1894 and 1906. Dept. of Marine and Fisheries, 1994.

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Canada. Dept. of Marine and Fisheries., ed. The Currents in the Gulf of St. Lawrence: Including the Anticosti region, Belle Isle and Cabot Straits; condensed from the reports of the survey of tides and currents for the seasons of 1894, 1895 and 1896. Government Printing Bureau, 1986.

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H, Armstrong Baxter, and Geological Survey (U.S.), eds. Low strain level acoustic emission due to seismic waves and tidal/thermoelastic strains observed at the San Francisco Presidio, California. U.S. Geological Survey, 1993.

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Book chapters on the topic "Tidal Strait"

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Bignami, F., and E. Salusti. "Tidal Currents and Transient Phenomena in the Strait of Messina: a Review." In The Physical Oceanography of Sea Straits. Springer Netherlands, 1990. http://dx.doi.org/10.1007/978-94-009-0677-8_4.

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García-Lafuente, Jesús, Simone Sammartino, José C. Sánchez-Garrido, and Cristina Naranjo. "Asymmetric Baroclinic Response to Tidal Forcing Along the Main Sill of the Strait of Gibraltar Inferred from Mooring Observations." In The Ocean in Motion. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-71934-4_14.

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Migné, Aline, and Dominique Davoult. "Macrobenthic metabolism as carbon and nitrogen fluxes in a coastal area exposed to strong tidal currents (Dover Strait, eastern English Channel)." In Recruitment, Colonization and Physical-Chemical Forcing in Marine Biological Systems. Springer Netherlands, 1998. http://dx.doi.org/10.1007/978-94-017-2864-5_25.

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Sentchev, Alexei, Max Yaremchuk, and Maxime Thiébaut. "Monitoring Strong Tidal Currents in Straits and Nearshore Regions." In The Ocean in Motion. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-71934-4_33.

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Yamauchi, T. "Case 9: Earthquake occurrence and temporal variations in Earth tidal strain amplitudes." In Evaluation of Proposed Earthquake Precursors. American Geophysical Union, 1991. http://dx.doi.org/10.1029/sp032p0061.

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Iino, Y., M. Itoh, M. Omote, Y. Yamaguchi, and T. Ban. "Effects of High Temperature Gas Environments(H2, Pure Air, Ar, Vacuum) on Slow Strain Rate Tensile Properties at 700°C of TiAl Alloy." In The Mechanical Behavior of Materials X. Trans Tech Publications Ltd., 2007. http://dx.doi.org/10.4028/0-87849-440-5.1007.

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"tidal strait(s)." In Dictionary Geotechnical Engineering/Wörterbuch GeoTechnik. Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-41714-6_201240.

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Shnukal, Anna, and Guy Ramsay. "Tidal Flows: an overview of Torres Strait Islander–Asian contact." In Navigating Boundaries: The Asian diaspora in Torres Strait. ANU eView, 2017. http://dx.doi.org/10.22459/nb.11.2017.02.

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Arnold, R. J. "An Improved Open Boundary Condition for A Tidal Model of Bass Strait." In North-Holland Mathematics Studies. Elsevier, 1987. http://dx.doi.org/10.1016/s0304-0208(08)70033-1.

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Ganju, Neil K., and David H. Schoellhamer. "Chapter 24 Lateral variability of the estuarine turbidity maximum in a tidal strait." In Sediment and Ecohydraulics - INTERCOH 2005. Elsevier, 2008. http://dx.doi.org/10.1016/s1568-2692(08)80026-5.

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Conference papers on the topic "Tidal Strait"

1

SATO, SATOSHI, NOBORU MATSUURA, ISAO ABE, TAKASHI SASAKI, and RYUUICHI HORII. "TIDAL CURRENT FORECASTING SYSTEM IN THE KANMON STRAIT." In Proceedings of the 8th International Symposium on Flow Modeling and Turbulence Measurements. WORLD SCIENTIFIC, 2002. http://dx.doi.org/10.1142/9789812777591_0057.

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Wen-Jye, JUANG, LIN Ming-Chung, and CHIANG Chung-Chiuan. "Visualization of Tidal Oscillation in the Taiwan Strait." In Proceedings of the 2nd International Conference. WORLD SCIENTIFIC, 2004. http://dx.doi.org/10.1142/9789812703040_0010.

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Li, Ye, Jonathan A. Colby, Neil Kelley, Robert Thresher, Bonnie Jonkman, and Scott Hughes. "Inflow Measurement in a Tidal Strait for Deploying Tidal Current Turbines: Lessons, Opportunities and Challenges." In ASME 2010 29th International Conference on Ocean, Offshore and Arctic Engineering. ASMEDC, 2010. http://dx.doi.org/10.1115/omae2010-20911.

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Tidal energy has received increasing attention over the past decade. This increasing focus on capturing the energy from tidal currents has brought about the development of many designs for tidal current turbines. Several of these turbines are progressing rapidly from design to prototype and pre-commercial stages. As these systems near commercial development, it becomes increasingly important that their performance be validated through laboratory tests (e.g., towing tank tests) and sea tests. Several different turbine configurations have been tested recently. The test results show significant differences in turbine performance between laboratory tests, numerical simulations, and sea tests. Although the mean velocity of the current is highly predictable, evidence suggests a critical factor in these differences is the unsteady inflow. To understand the physics and the effect of the inflow on turbine performance and reliability, Verdant Power (Verdant) and the National Renewable Energy Laboratory (NREL) have engaged in a partnership to address the engineering challenges facing marine current turbines. As part of this effort, Verdant deployed Acoustic Doppler Current Profiler (ADCP) equipment to collect data from a kinetic hydropower system (KHPS) installation at the Roosevelt Island Tidal Energy (RITE) project in the East River in New York City. The ADCP collected data for a little more than one year, and this data is critical for properly defining the operating environment needed for marine systems. This paper summarizes the Verdant-NREL effort to study inflow data provided by the fixed, bottom-mounted ADCP instrumentation and how the data is processed using numerical tools. It briefly reviews previous marine turbine tests and inflow measurements, provides background information from the RITE project, and describes the test turbine design and instrumentation setup. This paper also provides an analysis of the measured time domain data and a detailed discussion of shear profiling, turbulence intensity, and time-dependent fluctuations of the inflow. The paper concludes with suggestions for future work. The analysis provided in this paper will benefit future turbine operation studies. In addition, this study, as well as future studies in this topic area, will be beneficial to environmental policy makers and fishing communities.
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Chen, Lei, Paul A. J. Bonar, and Thomas A. A. Adcock. "Design of a Tidal Turbine Array for the Bohai Strait, China." In ASME 2018 37th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2018. http://dx.doi.org/10.1115/omae2018-77169.

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In this paper, we consider array design strategies to maximise the power available to turbines placed in the Bohai Strait, which is considered to be one of China’s most promising candidate sites for tidal stream power. The discontinuous Galerkin version of the open-source hydrodynamic model ADCIRC is used to simulate flow through the strait and tidal turbines are introduced using a sub-grid scale actuator disc model. New design algorithms based on key theoretical results are used to build large arrays, which are then compared in terms of both the collective power output and the power produced per turbine. The results of the analysis are used to draw general conclusions about the optimal design of tidal turbine arrays.
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Fujiwara, Takamichi, Takaharu Hamada, and Yusaku Kyozuka. "A Feasibility Study on Generation of Electricity by the Tidal Current in Kanmon Strait." In ASME 2003 22nd International Conference on Offshore Mechanics and Arctic Engineering. ASMEDC, 2003. http://dx.doi.org/10.1115/omae2003-37353.

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Promotion of the utilization of natural energy is urgent as a countermeasure to global warming. There are several kinds of energy resources in the ocean: waves, thermal differences, tidal levels and tidal currents. A feasibility study on tidal current power generation in Kanmon Strait, Japan is introduced in this report. A variable mesh version of the Marine Environmental Committee ocean model is used to reproduce the tidal current and to learn the distribution of tidal kinetic energy. Based on the simulation results, the optimal location for installation of a power plant is determined. The electric power created by a propeller type generator with a 10m diameter is also calculated as the average annual consumption of a household and availability of the power generation by the tidal current in Kanmon Strait is discussed.
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Kyozuka, Yusaku. "Observation of Waves in Naru Strait, Goto, Nagasaki, a Tidal Current Test Site." In ASME 2019 38th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2019. http://dx.doi.org/10.1115/omae2019-96652.

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Abstract Waves are primarily important for the tidal current power generation as they relate not only to the wave load acting on the tidal turbine but also to the installation/maintenance cost of the device through the workable day rate at the sea. Generally, the tidal current power site is in a narrow strait, and the wave characteristics are strongly dependent on the place. Also, there are few data itself. So, we conducted the wave observation in Naru Strait, Goto City, Nagasaki, where the tidal current power project by the Ministry of Environment is in progress. An AWAC (Acoustic Wave and Current Meter) was deployed on the sea bottom of 20m depth in Naru Strait on 18 May and recovered on 12 November, 2017. The wave data obtained for about 6 months were analyzed as wave spectra and mean directions by the records of surface elevation together with tidal current velocity. In particular, the changes of wave amplitude by the tidal current and the storms including typhoon passing are presented.
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Li, Huajun, Guoxiang Wu, Bingchen Liang, and Fan Fei. "Numerical assessment of tidal stream energy resource in Langyatai strait." In OCEANS 2012 - YEOSU. IEEE, 2012. http://dx.doi.org/10.1109/oceans-yeosu.2012.6263629.

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Coiro, D. P., G. Troise, T. Ciuffardi, and G. Sannino. "Tidal current energy resource assessment: The Strait of Messina test case." In 2013 International Conference on Clean Electrical Power (ICCEP). IEEE, 2013. http://dx.doi.org/10.1109/iccep.2013.6586992.

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Wu, He, Huaming Yu, Liang Kuang, Jie Ding, and Lu Wang. "Initial analysis and assessment of tidal current energy resource in the Qiongzhou Strait." In OCEANS 2014 - TAIPEI. IEEE, 2014. http://dx.doi.org/10.1109/oceans-taipei.2014.6964510.

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Hee-Su Lee, Jong-Chun Park, Dai-Hyun Choi, Se-min Jeong, Shigeru Tabeta, and Shinichiro Hirabayashi. "Numerical simulation of tidal currents around Korea/Japan strait and application to speed trial." In OCEANS 2010 IEEE - Sydney. IEEE, 2010. http://dx.doi.org/10.1109/oceanssyd.2010.5604024.

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Reports on the topic "Tidal Strait"

1

Amos, C. L., J. T. Judge, and J. V. Barrie. Storm-enhanced tidal sand transport - Hecate Strait, British Columbia, Canada. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1993. http://dx.doi.org/10.4095/183934.

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Straneo, Fiammetta, and Luc Rainville. The Competition of Tidal Mixing and Freshwater Forcing in Shaping the Outflow from Hudson Strait. Defense Technical Information Center, 2008. http://dx.doi.org/10.21236/ada534117.

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Hsiung, L. In-Situ TEM Observations of Strain-Induced Interface Instability in TiAl/Ti3Al Laminate Composite. Office of Scientific and Technical Information (OSTI), 2003. http://dx.doi.org/10.2172/15007359.

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Jay, David A. Internal Circulation in Tidal Channels and Straits and Associated AASERT Internal Circulation in Tidal Channels and Straits: a Comparison of Observed and Numerical Turbulence Estimates. Defense Technical Information Center, 1997. http://dx.doi.org/10.21236/ada628935.

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Tidal and residual currents measured by an acoustic doppler current profiler at the west end of Carquinez Strait, San Francisco Bay, California, March to November 1988. US Geological Survey, 1993. http://dx.doi.org/10.3133/wri924064.

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