Готові списки джерел за темами / Boundary currents

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Добірка наукової літератури з теми "Boundary currents"

Автор: Grafiati
Опубліковано: 25 січня 2025

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Статті в журналах з теми "Boundary currents"

1

Hogg, Nelson G., and William E. Johns. "Western boundary currents." Reviews of Geophysics 33, S2 (July 1995): 1311–34. http://dx.doi.org/10.1029/95rg00491.

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2

Ruju, Andrea, Pablo Higuera, Javier L. Lara, Inigo J. Losada, and Giovanni Coco. "RIP CURRENTS ON A BARRED BEACH." Coastal Engineering Proceedings 1, no. 33 (December 14, 2012): 38. http://dx.doi.org/10.9753/icce.v33.currents.38.

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This work presents the numerical study of rip current circulation on a barred beach. The numerical simulations have been carried out with the IH-FOAM model which is based on the three dimensional Reynolds Averaged Navier-Stokes equations. The new boundary conditions implemented in IH-FOAM have been used, including three dimensional wave generation as well as active wave absorption at the boundary. Applying the specific wave generation boundary conditions, the model is validated to simulate rip circulation on a barred beach. Moreover, this study addresses the identification of the forcing mechanisms and the three dimensional structure of the mean flow.
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3

Cessi, Paola, and Christopher L. Wolfe. "Adiabatic Eastern Boundary Currents." Journal of Physical Oceanography 43, no. 6 (June 1, 2013): 1127–49. http://dx.doi.org/10.1175/jpo-d-12-0211.1.

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Abstract The dynamics of the eastern boundary current of a high-resolution, idealized model of oceanic circulation are analyzed and interpreted in terms of residual mean theory. In this framework, it is clear that the eastern boundary current is adiabatic and inviscid. Nevertheless, the time-averaged potential vorticity is not conserved along averaged streamlines because of the divergence of Eliassen–Palm fluxes, associated with buoyancy and momentum eddy fluxes. In particular, eddy fluxes of buoyancy completely cancel the mean downwelling or upwelling, so that there is no net diapycnal residual transport. The eddy momentum flux acts like a drag on the mean velocity, opposing the acceleration from the eddy buoyancy flux: in the potential vorticity budget this results in a balance between the divergences of eddy relative vorticity and buoyancy fluxes, which leads to a baroclinic eastern boundary current whose horizontal scale is the Rossby deformation radius and whose vertical extent depends on the eddy buoyancy transport, the Coriolis parameter, and the mean surface buoyancy distribution.
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4

Ozdemir, Celalettin Emre, and Sahar Haddadian. "SEDIMENT TRANSPORT DUE TO CURRENT-SUPPORTED TURBIDITY CURRENTS OVER AN ERODIBLE BED." Coastal Engineering Proceedings, no. 36 (December 30, 2018): 33. http://dx.doi.org/10.9753/icce.v36.currents.33.

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Wave- and current-supported turbidity currents (WCSTCs), are one of the chief participants in shaping the marine geomorphology. What makes WCSTCs different from other turbidity currents is that boundary layer turbulence is required to suspend the sediments rather than the self-motion of the turbidity currents. In the presence of a mild slope, the gravitational acceleration drives the suspended sediments offshore (Sternberg et al., 1996; Wright et al., 2001). Depending on what dominates the boundary layer turbulence (BLT), we further define two major subclasses of WCSTCs: (i) wave-supported (WSTCs), and (ii) current-supported turbidity currents (CSTCs). Although significant advances have been made on the details of WSTCs (Ozdemir et al., 2011; Yu et al., 2014; Cheng et al., 2015), less is known about CSTCs. The objective of present study is to investigate the role of alongshore currents on CSTC dynamics over an erodible bottom boundary. The focus here is to identify the possible role of erosion on CSTC dynamics, and assess the coupling between current-induced BLT and suspended sediments for various bed erodibility parameters, i.e. critical shear stress, erosion coefficient, and settling velocity.
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5

Capodicasa, Erminia, Pietro Scandura, and Foti Enrico. "STEADY CURRENTS INDUCED BY SEA WAVES PROPAGATING OVER A SLOPING BOTTOM." Coastal Engineering Proceedings 1, no. 32 (January 30, 2011): 35. http://dx.doi.org/10.9753/icce.v32.currents.35.

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A numerical model aimed at computing the mean velocity generated by a sea wave propagating over a sloping bottom, offshore the breaker line, is presented. The model is based on the assumption that the fluid domain can be partitioned into two boundary layers and a core region where at a first order of approximation the flow can be regarded as irrotational. The irrotational flow is computed by using a theory based on the assumption of small amplitude waves which allows both fully absorbed waves and partially reflected waves at the coastline to be considered. The distribution of the mean velocity is controlled by the ratio between the thickness of the boundary layer and the wave amplitude. When this ratio is small, the mean velocities are rather constant along the depth and a second boundary layer develops close to the bottom. In the case of fully reflected waves such boundary layer separates and the mean vorticity can be convected far from the bottom.
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6

Sana, Ahmad, and Hitoshi Tanaka. "NUMERICAL MODELING OF A TURBULENT BOTTOM BOUNDARY LAYER UNDER SOLITARY WAVES ON A SMOOTH SURFACE." Coastal Engineering Proceedings, no. 36 (December 30, 2018): 26. http://dx.doi.org/10.9753/icce.v36.currents.26.

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A number of studies on bottom boundary layers under sinusoidal and cnoidal waves were carried out in the past owing to the role of bottom shear stress on coastal sediment movement. In recent years, the bottom boundary layers under long waves have attracted considerable attention due to the occurrence of huge tsunamis and corresponding sediment movement. In the present study two-equation turbulent models proposed by Menter(1994) have been applied to a bottom boundary layer under solitary waves. A comparison has been made for cross-stream velocity profile and other turbulence properties in x-direction.
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7

Cember, Richard P. "On deep western boundary currents." Journal of Geophysical Research: Oceans 103, no. C3 (March 15, 1998): 5397–417. http://dx.doi.org/10.1029/97jc02422.

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8

Csanady, G. T., and J. L. Pelegri. "Vorticity balance of boundary currents." Journal of Marine Research 53, no. 2 (March 1, 1995): 171–87. http://dx.doi.org/10.1357/0022240953213269.

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9

Adityawan, Mohammad Bagus, Hitoshi Tanaka, and Pengzhi Lin. "BED STRESS INVESTIGATION UNDER BREAKING SOLITARY WAVE RUNUP." Coastal Engineering Proceedings 1, no. 33 (October 25, 2012): 23. http://dx.doi.org/10.9753/icce.v33.currents.23.

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The bed stress under breaking solitary wave runup was investigated in this study using the Simultaneous Coupling Method (SCM). The SCM couples the shallow water equation (SWE) with k-w model. The depth averaged velocity from SWE is applied as the upper boundary condition in k-w model for bed stress assessment from the boundary layer. It was found that the boundary layer approach provides more accurate bed stress estimation than the empirical method, which leads to a more accurate prediction of runup and wave profile. The accumulation of bed stress in during solitary wave runup was evaluated. The bed stress on the direction leaving the shoreline will have more impact in the overall process. However, during a short period of run up process, bed stress toward the shoreline may have significant effect as well.
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10

Ma, Peifeng, and Ole Secher Madsen. "AN OPEN BOUNDARY CONDITION FOR APPLICATION IN NUMERICAL COASTAL MODELS." Coastal Engineering Proceedings 1, no. 32 (January 29, 2011): 30. http://dx.doi.org/10.9753/icce.v32.currents.30.

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Open boundaries (OBs) are usually unavoidable in numerical coastal circulation simulations. At OBs, appropriate open boundary conditions (OBCs) are required and a good OBC should be able to let outgoing waves freely pass to the exterior of a computational domain without creating reflections at the OBs. In the present study, a methodology has been developed to predict two parameters, phase speed c_r and decay time T_f, in a standard OBC formulation, so that the OBC is significantly improved compared to commonly used existing OBCs with specified c_r and T_f. For the conditions where wave period is unknown, the OBC with approximated c_r and T_f may be applied and a test reveals that this OBC is able to yield good results in typical coastal flow conditions. In addition, a Swing-Door Boundary Condition (SDBC) is proposed and tested for application at an offshore open boundary where both incoming and outgoing waves exist.
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Дисертації з теми "Boundary currents"

1

Cuny, Jerome. "Labrador Sea boundary currents /." Thesis, Connect to this title online; UW restricted, 2003. http://hdl.handle.net/1773/10959.

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2

Kuehl, Joseph J. "On the dynamics of oceanic gap-traversing boundary currents /." View online ; access limited to URI, 2009. http://digitalcommons.uri.edu/dissertations/AAI3401123.

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3

Chadwick, David Bartholomew. "Tidal exchange at the bay-ocean boundary /." Diss., Connect to a 24 p. preview or request complete full text in PDF format. Access restricted to UC campuses, 1997. http://wwwlib.umi.com/cr/ucsd/fullcit?p9823709.

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4

Chang, Kyung-Il. "The shelfward penetration of western boundary currents." Thesis, University of Southampton, 1993. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.239963.

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5

Le, Bras Isabela Astiz. "Dynamics of North Atlantic western boundary currents." Thesis, Massachusetts Institute of Technology, 2017. http://hdl.handle.net/1721.1/109056.

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Анотація:
Thesis: Ph. D., Joint Program in Physical Oceanography (Massachusetts Institute of Technology, Department of Earth, Atmospheric, and Planetary Sciences; and the Woods Hole Oceanographic Institution), 2017.
Cataloged from PDF version of thesis.
Includes bibliographical references (pages 163-174).
The Gulf Stream and Deep Western Boundary Current (DWBC) shape the distribution of heat and carbon in the North Atlantic, with consequences for global climate. This thesis employs a combination of theory, observations and models to probe the dynamics of these two western boundary currents. First, to diagnose the dynamical balance of the Gulf Stream, a depth-averaged vorticity budget framework is developed. This framework is applied to observations and a state estimate in the subtropical North Atlantic. Budget terms indicate a primary balance of vorticity between wind stress forcing and dissipation, and that the Gulf Stream has a significant inertial component. The next chapter weighs in on an ongoing debate over how the deep ocean is filled with water from high latitude sources. Measurements of the DWBC at Line W, on the continental slope southeast of New England, reveal water mass changes that are consistent with changes in the Labrador Sea, one of the sources of deep water thousands of kilometers upstream. Coherent patterns of change are also found along the path of the DWBC. These changes are consistent with an advective-diffusive model, which is used to quantify transit time distributions between the Labrador Sea and Line W. Advection and stirring are both found to play leading order roles in the propagation of water mass anomalies in the DWBC. The final study brings the two currents together in a quasi-geostrophic process model, focusing on the interaction between the Gulf Stream's northern recirculation gyre and the continental slope along which the DWBC travels. We demonstrate that the continental slope restricts the extent of the recirculation gyre and alters its forcing mechanisms. The recirculation gyre can also merge with the DWBC at depth, and its adjustment is associated with eddy fluxes that stir the DWBC with the interior. This thesis provides a quantitative description of the structure of the overturning circulation in the western North Atlantic, which is an important step towards understanding its role in the climate system.
by Isabela Astiz Le Bras.
Ph. D.
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6

Munday, David R. "On the flow separation of western boundary currents." Thesis, University of Reading, 2004. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.415521.

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7

Stahr, Frederick R. "Transport and bottom boundary layer observations of the North Atlantic deep western boundary current at the Blake Outer Ridge /." Thesis, Connect to this title online; UW restricted, 1998. http://hdl.handle.net/1773/10998.

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8

Parsadous, Ali. "Vertical sidewall boundary layers in combined waves and currents." Thesis, University College London (University of London), 1995. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.339101.

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9

Edberg, Richard. "Vortex Currents near the Boundary of a Two-Component Superconductor." Thesis, KTH, Fysik, 2017. http://urn.kb.se/resolve?urn=urn:nbn:se:kth:diva-209923.

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10

Ceballos, Lina Isabel. "North pacific gyre oscillation synchronizes climate fluctuations in the eastern and western boundary systems." Thesis, Atlanta, Ga. : Georgia Institute of Technology, 2008. http://hdl.handle.net/1853/26552.

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Анотація:
Thesis (M. S.)--Earth and Atmospheric Sciences, Georgia Institute of Technology, 2009.
Committee Chair: Di Lorenzo, Emanuele; Committee Member: Bracco, Annalisa; Committee Member: Webster, Peter J.. Part of the SMARTech Electronic Thesis and Dissertation Collection.
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Книги з теми "Boundary currents"

1

Hunt, Heather D. Boundary current experiment I & II, RAFOS float data report, 1994-1997. Woods Hole, Mass: Woods Hole Oceanographic Institution, 1998.

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2

Okkonen, Stephen R. Seasonality of boundary conditions for Cook Inlet, Alaska. Fairbanks, AK: Coastal Marine Institute, University of Alaska, Minerals Management Service, Dept. of the Interior, and the School of Fisheries & Ocean Sciences, 2009.

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3

Shen, J. Computational electromagnetics using boundary elements: Advances in modelling eddy currents. Southampton, UK: Computational Mechanics Publications, 1995.

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4

Cessi, Paola. On the role of topography and of boundary forcing in the ocean circulation. Woods Hole, Mass: Woods Hole Oceanographic Institution, 1987.

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5

Carlos N. Lopes da Costa. A numerical study of wind forcing in the eastern boundary current system off Portugal. Monterey, Calif: Naval Postgraduate School, 1989.

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6

United States. National Aeronautics and Space Administration., ed. Observations of the magnetopause current layer: Cases with no boundary layer and tests of recent models. [Washington, D.C.]: National Aeronautics and Space Administration, 1995.

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7

Fung, Shing F., and Theodore A. Fritz. The magnetospheric cusps: Structure and dynamics. Dordrecht: Springer, 2011.

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8

Shen, Jinxing. Computation of linear and nonlinear Eddi currents with the boundary element method. [s.l.]: [s.n.], 1994.

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9

Jessen, Paul F. Hydrographic and Acoustic Doppler Current Profiler (ADCP) data from the ONR Eastern Boundary Current Accelerated Research Iniative - June 9-16, 1992. Monterey, Calif: Naval Postgraduate School, 1993.

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10

United States. National Aeronautics and Space Administration., ed. Review of geography internship on convective wave project. [Greeley, Colo.]: Univ. of Northern Colorado, Geography Dept., 1990.

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Частини книг з теми "Boundary currents"

1

Atkinson, Larry P. "Western Boundary Currents." In Global Change – The IGBP Series, 121–69. Berlin, Heidelberg: Springer Berlin Heidelberg, 2010. http://dx.doi.org/10.1007/978-3-540-92735-8_3.

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2

Kamenkovich, V. M., M. N. Koshlyakov, and A. S. Monin. "Eddies of Western Boundary Currents." In Synoptic Eddies in the Ocean, 208–64. Dordrecht: Springer Netherlands, 1986. http://dx.doi.org/10.1007/978-94-009-4502-9_4.

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3

McCreary, Julian P., and Satish R. Shetye. "Sverdrup Flow and Boundary Currents." In Observations and Dynamics of Circulations in the North Indian Ocean, 299–312. Singapore: Springer Nature Singapore, 2023. http://dx.doi.org/10.1007/978-981-19-5864-9_11.

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4

Yamauchi, M., R. Lundin, L. Eliasson, S. Ohtani, and J. H. Clemmons. "Relationship between Large-, Meso-, and Small-Scale Field-Aligned Currents and their Current Carriers." In Polar Cap Boundary Phenomena, 173–88. Dordrecht: Springer Netherlands, 1998. http://dx.doi.org/10.1007/978-94-011-5214-3_14.

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5

Verweij, A. P. "Review on Boundary-Induced Coupling Currents." In Advances in Cryogenic Engineering Materials, 1059–68. Boston, MA: Springer US, 1998. http://dx.doi.org/10.1007/978-1-4757-9056-6_139.

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6

Krawczyk, A. "The Calculation of Transient Eddy Currents by Means of the Boundary Element Method." In Boundary Elements VIII, 905–17. Berlin, Heidelberg: Springer Berlin Heidelberg, 1986. http://dx.doi.org/10.1007/978-3-662-22335-2_36.

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7

Potemra, T. A. "Sources of Large-Scale Birkeland Currents." In Physical Signatures of Magnetospheric Boundary Layer Processes, 3–27. Dordrecht: Springer Netherlands, 1994. http://dx.doi.org/10.1007/978-94-011-1052-5_1.

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8

McAnally, W. H., and E. J. Hayter. "Estuarine Boundary Layers and Sediment Transport." In Residual Currents and Long-term Transport, 260–75. New York, NY: Springer New York, 1990. http://dx.doi.org/10.1007/978-1-4613-9061-9_19.

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9

Troshichev, O. A. "Low-latitude boundary layer and generation of field-aligned currents." In Earth's Low-Latitude Boundary Layer, 329–34. Washington, D. C.: American Geophysical Union, 2003. http://dx.doi.org/10.1029/133gm33.

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Pilipenko, Viacheslav A., Valeriy A. Martines-Bedenko, Mark J. Engebretson, Vladimir O. Papitashvili, and Patrick T. Newell. "High-latitude mapping of ULF activity, field-aligned currents, and DMSP-based dayside magnetospheric domains." In Earth's Low-Latitude Boundary Layer, 231–40. Washington, D. C.: American Geophysical Union, 2003. http://dx.doi.org/10.1029/133gm23.

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Тези доповідей конференцій з теми "Boundary currents"

1

Lin, Tzu-Ying, Yong-Xiao Chen, Jin-Fu Li, Chih-Yen Lo, Ding-Ming Kwai, and Yung-Fa Chou. "A Test Method for Finding Boundary Currents of 1T1R Memristor Memories." In 2016 IEEE 25th Asian Test Symposium (ATS). IEEE, 2016. http://dx.doi.org/10.1109/ats.2016.44.

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2

Pashchenko, Volodymyr. "The boundary elements modelling of eddy currents in the orthotropic composite." In 2014 International Conference on Mathematical Methods in Electromagnetic Theory (MMET). IEEE, 2014. http://dx.doi.org/10.1109/mmet.2014.6928729.

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3

Guth, K. "Grain Boundary Critical Currents in High-Tc Superconductors: A Magneto-Optical Study." In ADVANCES IN CRYOGENIC ENGINEERING: Transactions of the International Cryogenic Materials Conference - ICMC. AIP, 2004. http://dx.doi.org/10.1063/1.1774628.

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4

Wang, Jae Hwan, and Hyun Sik Yoon. "Large Eddy Simulation of Gravity Current Flow Past a Circular Cylinder Using Immersed Boundary Method." In ASME/JSME/KSME 2015 Joint Fluids Engineering Conference. American Society of Mechanical Engineers, 2015. http://dx.doi.org/10.1115/ajkfluids2015-07325.

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We investigated the flow of gravity currents past circular cylinders above the smooth bed. In order to simulate the gravity current interacting with cylinder, large eddy simulation (LES) coupled with a direct forcing/fictitious domain (DF/FD) method was employed. The hydrodynamic forces induced by the gravity current on a circular cylinder and the flow features were investigated according to a gap distance from location below the cylinder to the bed and Reynolds number. When the gravity current encounters the circular cylinder, the maximum drag force occurs regardless of gap distance. In addition, Von Karman vortex shedding emerges behind the circular cylinder for larger gap distance. In this regard, the results can be divided into impact, transient and quasi-steady stages based on the characteristics of the hydrodynamic forces varying with time, which is consistent with previous observations. Consequently, our numerical approach well simulated the flow of gravity currents past circular cylinders in good agreement with those of previous studies.
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5

Xiao, Mufei. "Reflection of Diffusion at Boundary Causes Anomalous Transient Photo-Currents in Amorphous Materials." In Frontiers in Optics. Washington, D.C.: OSA, 2005. http://dx.doi.org/10.1364/fio.2005.jtuc15.

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Thwaites, F. T., and A. J. Williams. "BASS measurements of currents, waves, stress, and turbulence in the North Sea bottom-boundary layer." In Proceedings of the IEEE Sixth Working Conference on Current Measurement (Cat. No.99CH36331). IEEE, 1999. http://dx.doi.org/10.1109/ccm.1999.755246.

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Jones, Oliver, Julio A. Zyserman, and Yushi Wu. "Influence of Apparent Roughness on Pipeline Design Conditions Under Combined Waves and Current." In ASME 2014 33rd International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2014. http://dx.doi.org/10.1115/omae2014-24030.

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The oscillatory nature of waves generates a thin boundary layer above the sea bed in which the fluid velocity decreases from its free stream value to zero at the bed. The wave boundary layer thickness is small compared to the current-alone boundary layer (which typically extends throughout the water depth) and, as such, is characterized by a zone of high shear velocity and associated high levels of turbulence. Strong turbulence intensities within the wave-induced boundary layer have an impact on the ambient current field, which experiences an increase in bottom resistance (the so-called ‘apparent roughness’) due to the presence of the turbulent boundary layer. For currents on the continental shelf, it is well known that the effect of wave-enhanced bottom friction (or “apparent roughness”) is important in controlling the near-bed current speed and turbulent mixing. It can thus be reasonably expected that accounting for this apparent roughness will influence the design basis for sub-marine pipelines that cross the continental shelf. In this paper, we implement — and then demonstrate — the effect of wave-related apparent roughness on currents with the aim of providing a more accurate design basis for pipelines on the continental shelf.
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Simons, Richard R., Tony J. Grass, and Mehrdad Mansour-Tehrani. "Bottom Shear Stresses in the Boundary Layers Under Waves and Currents Crossing at Right Angles." In 23rd International Conference on Coastal Engineering. New York, NY: American Society of Civil Engineers, 1993. http://dx.doi.org/10.1061/9780872629332.045.

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Wang, Kan, Yun-Sheng Xu, and Fu-Sheng Tang. "On-surface discretized boundary equation method based on field expressions in terms of magnetic currents." In 2009 3rd IEEE International Symposium on Microwave, Antenna, Propagation and EMC Technologies for Wireless Communications (MAPE). IEEE, 2009. http://dx.doi.org/10.1109/mape.2009.5355856.

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KRANENBURG, WOUTER, JAN RIBBERINK, and ROB UITTENBOGAARD. "NET CURRENTS IN THE WAVE BOUNDARY LAYER: BALANCE OF WAVE SHAPE AND FREE SURFACE EFFECTS." In The Proceedings of the Coastal Sediments 2011. World Scientific Publishing Company, 2011. http://dx.doi.org/10.1142/9789814355537_0113.

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Звіти організацій з теми "Boundary currents"

1

Cessi, Paola. Separation of Western Boundary Currents. Fort Belvoir, VA: Defense Technical Information Center, October 1992. http://dx.doi.org/10.21236/ada256516.

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2

Johns, William E. Dynamics of Boundary Currents and Marginal Seas. Fort Belvoir, VA: Defense Technical Information Center, September 1997. http://dx.doi.org/10.21236/ada628241.

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3

Johns, William E. Dynamics of Boundary Currents and Marginal Seas. Fort Belvoir, VA: Defense Technical Information Center, August 2002. http://dx.doi.org/10.21236/ada626445.

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4

Johns, William E. Dynamics of Boundary Currents and Marginal Seas: Windward Passage Experiment. Fort Belvoir, VA: Defense Technical Information Center, September 2006. http://dx.doi.org/10.21236/ada612623.

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5

Shi, Donglu. Transport critical currents and grain boundary coupling in high-{Tc} superconductors. Office of Scientific and Technical Information (OSTI), July 1991. http://dx.doi.org/10.2172/10144496.

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6

Joyce, Terrence M. Tracing the Pathway and Transport of Proto-NPIW Flowing Out of the Sea of Okhotsk into the Boundary Currents of the NW Pacific. Fort Belvoir, VA: Defense Technical Information Center, March 2001. http://dx.doi.org/10.21236/ada389289.

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7

Li, Honghai, Mitchell Brown, Lihwa Lin, Yan Ding, Tanya Beck, Alejandro Sanchez,, Weiming Wu, Christopher Reed, and Alan Zundel. Coastal Modeling System user's manual. Engineer Research and Development Center (U.S.), April 2024. http://dx.doi.org/10.21079/11681/48392.

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Анотація:
The Coastal Modeling System (CMS) is a suite of coupled 2D numerical models for simulating nearshore waves, currents, water levels, sediment transport, morphology change, and salinity and temperature. Developed by the Coastal Inlets Research Program of the US Army Corps of Engineers, the CMS provides coastal engineers and scientists a PC-based, easy-to-use, accurate, and efficient tool for understanding of coastal processes and for designing and managing of coastal inlets research, navigation projects, and sediment exchange between inlets and adjacent beaches. The present technical report acts as a user guide for the CMS, which contains comprehensive information on model theory, model setup, and model features. The detailed descriptions include creation of a new project, configuration of model grid, various types of boundary conditions, representation of coastal structures, numerical methods, and coupled simulations of waves, hydrodynamics, and sediment transport. Pre- and post-model data processing and CMS modeling procedures are also described through operation within a graphic user interface—the Surface- water Modeling System.
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8

Reusch, M. F. Free boundary skin current MHD (magnetohydrodynamic) equilibria. Office of Scientific and Technical Information (OSTI), February 1988. http://dx.doi.org/10.2172/5256723.

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9

Watts, D. R., Kathleen A. Donohue, and Arlene Guest. Western Boundary Current Systems Virtual Poster Session. Fort Belvoir, VA: Defense Technical Information Center, September 2001. http://dx.doi.org/10.21236/ada624673.

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10

Rhines, Peter B. Labrador Sea Boundary Current and Convection Dynamics. Fort Belvoir, VA: Defense Technical Information Center, September 2001. http://dx.doi.org/10.21236/ada625145.

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