Bibliographies thématiques / Boundary currents

Sommaire

  1. Articles de revues
  2. Thèses
  3. Livres
  4. Chapitres de livres
  5. Actes de conférences
  6. Rapports d'organisations

Littérature scientifique sur le sujet « Boundary currents »

Auteur : Grafiati
Publié le 25 janvier 2025

Créez une référence correcte selon les styles APA, MLA, Chicago, Harvard et plusieurs autres

Choisissez une source :

Consultez les listes thématiques d’articles de revues, de livres, de thèses, de rapports de conférences et d’autres sources académiques sur le sujet « Boundary currents ».

À côté de chaque source dans la liste de références il y a un bouton « Ajouter à la bibliographie ». Cliquez sur ce bouton, et nous générerons automatiquement la référence bibliographique pour la source choisie selon votre style de citation préféré : APA, MLA, Harvard, Vancouver, Chicago, etc.

Vous pouvez aussi télécharger le texte intégral de la publication scolaire au format pdf et consulter son résumé en ligne lorsque ces informations sont inclues dans les métadonnées.

Articles de revues sur le sujet "Boundary currents"

1

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

Texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
2

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

Texte intégral
Résumé :
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.
Styles APA, Harvard, Vancouver, ISO, etc.
3

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

Texte intégral
Résumé :
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.
Styles APA, Harvard, Vancouver, ISO, etc.
4

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

Texte intégral
Résumé :
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.
Styles APA, Harvard, Vancouver, ISO, etc.
5

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

Texte intégral
Résumé :
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.
Styles APA, Harvard, Vancouver, ISO, etc.
6

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

Texte intégral
Résumé :
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.
Styles APA, Harvard, Vancouver, ISO, etc.
7

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

Texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
8

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

Texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
9

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

Texte intégral
Résumé :
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.
Styles APA, Harvard, Vancouver, ISO, etc.
10

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

Texte intégral
Résumé :
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.
Styles APA, Harvard, Vancouver, ISO, etc.
Plus de sources

Thèses sur le sujet "Boundary currents"

1

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

Texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
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.

Texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
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.

Texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
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.

Texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
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.

Texte intégral
Résumé :
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.
Styles APA, Harvard, Vancouver, ISO, etc.
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.

Texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
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.

Texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
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.

Texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
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.

Texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
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.

Texte intégral
Résumé :
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.
Styles APA, Harvard, Vancouver, ISO, etc.
Plus de sources

Livres sur le sujet "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.

Trouver le texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
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.

Trouver le texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
3

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

Trouver le texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
4

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

Trouver le texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
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.

Trouver le texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
6

United States. National Aeronautics and Space Administration., dir. 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.

Trouver le texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
7

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

Trouver le texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
8

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

Trouver le texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
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.

Trouver le texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
10

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

Trouver le texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
Plus de sources

Chapitres de livres sur le sujet "Boundary currents"

1

Atkinson, Larry P. « Western Boundary Currents ». Dans 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.

Texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
2

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

Texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
3

McCreary, Julian P., et Satish R. Shetye. « Sverdrup Flow and Boundary Currents ». Dans 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.

Texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
4

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

Texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
5

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

Texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
6

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

Texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
7

Potemra, T. A. « Sources of Large-Scale Birkeland Currents ». Dans 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.

Texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
8

McAnally, W. H., et E. J. Hayter. « Estuarine Boundary Layers and Sediment Transport ». Dans 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.

Texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
9

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

Texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
10

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

Texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.

Actes de conférences sur le sujet "Boundary currents"

1

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

Texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
2

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

Texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
3

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

Texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
4

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

Texte intégral
Résumé :
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.
Styles APA, Harvard, Vancouver, ISO, etc.
5

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

Texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
6

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

Texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
7

Jones, Oliver, Julio A. Zyserman et Yushi Wu. « Influence of Apparent Roughness on Pipeline Design Conditions Under Combined Waves and Current ». Dans 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.

Texte intégral
Résumé :
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.
Styles APA, Harvard, Vancouver, ISO, etc.
8

Simons, Richard R., Tony J. Grass et Mehrdad Mansour-Tehrani. « Bottom Shear Stresses in the Boundary Layers Under Waves and Currents Crossing at Right Angles ». Dans 23rd International Conference on Coastal Engineering. New York, NY : American Society of Civil Engineers, 1993. http://dx.doi.org/10.1061/9780872629332.045.

Texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
9

Wang, Kan, Yun-Sheng Xu et Fu-Sheng Tang. « On-surface discretized boundary equation method based on field expressions in terms of magnetic currents ». Dans 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.

Texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
10

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

Texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.

Rapports d'organisations sur le sujet "Boundary currents"

1

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

Texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
2

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

Texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
3

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

Texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
4

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

Texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
5

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

Texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
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, mars 2001. http://dx.doi.org/10.21236/ada389289.

Texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
7

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

Texte intégral
Résumé :
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.
Styles APA, Harvard, Vancouver, ISO, etc.
8

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

Texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
9

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

Texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
10

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

Texte intégral
Styles APA, Harvard, Vancouver, ISO, etc.
Vous pouvez également être intéressé par les bibliographies sur le sujet « Boundary currents » pour d’autres types de sources :
Articles de revues Thèses Livres
Nous offrons des réductions sur tous les plans premium pour les auteurs dont les œuvres sont incluses dans des sélections littéraires thématiques. Contactez-nous pour obtenir un code promo unique!

Vers la bibliographie