Bibliografías temáticas / Currents dynamics

Literatura académica sobre el tema "Currents dynamics"

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Publicado: 14 de marzo de 2023

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Artículos de revistas sobre el tema "Currents dynamics"

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Luijendijk, Arjen, Johan Henrotte, Dirk Jan Walstra y Maarten Van Ormondt. "QUASI-3D MODELLING OF SURF ZONE DYNAMICS". Coastal Engineering Proceedings 1, n.º 32 (26 de enero de 2011): 52. http://dx.doi.org/10.9753/icce.v32.currents.52.

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A quasi-three-dimensional model (quasi-3D) has been developed through the implementation of an analytical 1DV flow model in existing depth-averaged shallow water equations. The model includes the effects of waves and wind on the vertical distribution of the horizontal velocities. Comparisons with data from both physical and field cases show that the quasi-3D approach is able to combine the effect of vertical structures with the efficiency of depth-averaged simulations. Inter-comparisons with three-dimensional simulations show that the quasi-3D approach can represent similar velocity profiles in the surf zone. Quasi-3D morphodynamic simulations show that the bed dynamics in the surf zone represent the relevant 3D effects in the surf zone much more than the depth-averaged computations. It was shown that the quasi-3D approach is computationally efficient as it only adds about 15-20% to the runtimes of a 2DH simulation which is minor compared to a run time increase of 250-800% when switching to a 3D simulation.
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Frank, Anna G., Sergey G. Bugrov y Vladimir S. Markov. "Hall currents in a current sheet: Structure and dynamics". Physics of Plasmas 15, n.º 9 (septiembre de 2008): 092102. http://dx.doi.org/10.1063/1.2972158.

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Dujardin, Romain. "Laminar currents and birational dynamics". Duke Mathematical Journal 131, n.º 2 (febrero de 2006): 219–47. http://dx.doi.org/10.1215/s0012-7094-06-13122-8.

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Ozdemir, Celalettin Emre y Sahar Haddadian. "SEDIMENT TRANSPORT DUE TO CURRENT-SUPPORTED TURBIDITY CURRENTS OVER AN ERODIBLE BED". Coastal Engineering Proceedings, n.º 36 (30 de diciembre de 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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Nasrollahpour, Reza, Mohamad Hidayat Jamal, Mehdi Ghomesi, Zulhilmi Ismail y Peiman Roushenas. "Density Currents Dynamics over Rough Beds". Applied Mechanics and Materials 735 (febrero de 2015): 159–62. http://dx.doi.org/10.4028/www.scientific.net/amm.735.159.

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Density currents are flows driven by density differences caused by suspended fine solid material, dissolved contents, temperature gradient or a combination of them. Reservoir sedimentation is often related to sediment transport by density currents. This sedimentation can block bottom outlets, reduce the capacity of reservoir and harms the dam power plants. The head is the leading edge of density currents. In this paper, the influences of artificially roughened beds on dynamics of the frontal region of density currents are investigated experimentally. Three rough beds using conic roughness elements and a smooth bed were tested. The observed trend is that as the surface roughness increases the head concentration and velocity decreases.
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Diller, Jeffrey. "Birational maps, positive currents, and dynamics." Michigan Mathematical Journal 46, n.º 2 (septiembre de 1999): 361–75. http://dx.doi.org/10.1307/mmj/1030132416.

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da Silveira, Ilson C. A., Glenn R. Flierl y Wendell S. Brown. "Dynamics of Separating Western Boundary Currents". Journal of Physical Oceanography 29, n.º 2 (febrero de 1999): 119–44. http://dx.doi.org/10.1175/1520-0485(1999)029<0119:doswbc>2.0.co;2.

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Cessi, Paola, R. Vance Condie y W. R. Young. "Dissipative dynamics of western boundary currents". Journal of Marine Research 48, n.º 4 (1 de noviembre de 1990): 677–700. http://dx.doi.org/10.1357/002224090784988719.

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Fan, Shuangshuang y Craig A. Woolsey. "Dynamics of underwater gliders in currents". Ocean Engineering 84 (julio de 2014): 249–58. http://dx.doi.org/10.1016/j.oceaneng.2014.03.024.

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Leonetti, Marc. "Dynamics of concentration-dependent ionic currents". Physical Review E 52, n.º 1 (1 de julio de 1995): R33—R35. http://dx.doi.org/10.1103/physreve.52.r33.

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Tesis sobre el tema "Currents dynamics"

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Sharifuzzaman, MD. "Dynamics of Crystalline Gravity Currents". Thesis, Griffith University, 2018. http://hdl.handle.net/10072/381374.

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Gravity currents, which are also known as density currents, are established when one fluid flows into another of different density, and the density difference between the two drives the flow. They are widespread and vital phenomena that occur within numerous natural systems (Lemckert and Imberger, 1993a, b; Lemckert et al., 2002; Yu et al., 2013; Zigic et al., 2002). While the majority of commonly occurring gravity currents have received significant attention by researchers, crystalline gravity currents have not been studied extensively yet, and there is very little fundamental knowledge about their behavior. Crystalline and particle-driven gravity currents are suspensions of dense particles that spread into an ambient fluid due to the difference between the density of suspension and that of the ambient fluid (Sparks et al., 1997; Simpson, 1997). Studies have been conducted in laboratories analyzing gravity currents mainly on lock exchange phenomenon (Huppert and Simpson, 1980; Hallworth et al. 1996; Lemckert et al., 2002; Rottman and Simpson, 1983; Shin et al., 2004) and continuous inflow phenomenon (Ellison and Turner, 1959; Garcia, 1993; Maxworthy, 1983; Middleton, 1966b; Zhang et al., 2008). In Lock exchange mechanism, two fluids of varying density are kept separate by a lock gate. The fluid with higher density is known as the lock fluid and it has significantly lower volume than the second fluid. When the lock gate is removed, gravity current forms because of the density difference between the fluids. During the evolution of the current, the particles continually deposit or dissolve, thus reducing the excess density of suspension and the driving buoyancy force (e. g. during the late stages of turbidity currents, Parker et al., 1986). While the non-dissolving kind (sediment-laden) is well studied by many researchers (Fragoso et al., 2013; Garcia, 1994; Hallworth et al., 1996; Kuenen, 1937; Parker et al., 1986; Simpson and Britter, 1979; Shin et al., 2004;), the crystalline gravity currents are not being looked at. The focus of this study was on these currents produced by lock release inflow of highly saline solution with suspended salt crystals to understand their behavior, and the impact they may have on the receiving environment. The results were then compared with those of unsaturated gravity currents under the same experimental conditions. Data were also extracted from the literature for sediment-laden lock release gravity currents under similar experimental conditions and compared with the findings of this study focusing on the self-similar phase. The outcomes of this experimental study showed that dynamics of crystalline gravity currents are entirely different from those of unsaturated and sediment-laden gravity currents. The temporal change in the driving buoyancy affects its characteristics. The research and outcomes of this study will assist in providing first-hand knowledge of the progress of gravity currents with initially suspended salt crystals in lock release condition into a receiving environment.
Thesis (Masters)
Master of Philosophy (MPhil)
School of Eng & Built Env
Science, Environment, Engineering and Technology
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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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Edwards, Deborah Anne. "Turbidity currents : dynamics, deposits and reversals". Thesis, University of Leeds, 1991. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.293760.

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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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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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Thorpe, Antony. "Sediment transport and bedform dynamics in rip currents". Thesis, University of Plymouth, 2016. http://hdl.handle.net/10026.1/6558.

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Simultaneous in-situ measurements of waves, currents, water depth, suspended sediment concentrations and bed profiles were made in a rip channel on Perranporth Beach, Cornwall, UK. Perranporth is a high energy beach (annual offshore Hs = 1.6 m) which is macro-tidal (mean spring range = 6.3 m) and the grain size is medium sand (D50 = 0.28 – 0.34 mm). It can be classified as a low tide bar – rip beach and exhibits a relatively flat inter-tidal zone with pronounced rhythmic low tide bar - rip morphology. Data were collected over two field campaigns, totalling 14 tidal cycles and including 27 occurrences of rip currents, in a range of offshore wave heights (Hs = 0.5 – 3 m). The in-situ measurements were supplemented with morphological beach surveys. Sediment samples were taken for grain size analysis. The rip current was found to be tidally modulated. The strongest rip flow (0.7 m/s) occurred at mid to low tide, when waves were breaking on the adjacent bar. Rip flow persisted when the bar had dried out at the lowest tidal elevations. The rip was observed to pulse at a very low frequency (VLF) with a period of 15 - 20 minutes, which was shown to be influenced by wave breaking on the adjacent bar. The rip was completely in-active at high tide. Bedforms were ubiquitous in the rip channel and occurred at all stages of the tide. Visual observations found bedforms to be orientated shore parallel. When the rip was active, mean bedform length and height was 1.45 m and 0.06 m respectively. The size and position of the bedforms in the nearshore suggested that they were best classified as megaripples. When the rip was not active, the mean bedform length and height was 1.09 m and 0.06 m respectively. In rip conditions, with typical mean offshore flow rates of > 0.3 m/s, the bedforms migrated in an offshore direction at a mean rate of 0.16 cm/min and a maximum rate of 4.6 cm/min. The associated mean bedform sediment transport rate was 0.0020 kg/m/s, with a maximum rate of 0.054 kg/m/s. In the rip, migration rates were correlated with offshore directed mean flow strength. In non-rip conditions, bedform migration was onshore directed with a mean rate of 0.09 cm/min and a maximum rate of = 2.2 cm/min. The associated mean bedform transport rate was 0.0015 kg/m/s, with a maximum rate of = 0.041 kg/m/s. The onshore bedform transport was correlated with incident wave skewness, and was weakly correlated with orbital velocity. Over a tidal cycle, the offshore directed bedform transport was only marginally larger in rip currents than when it was when onshore directed in non-rip conditions. Sediment suspension in the rip current was shown to be dependent on the presence of waves. Suspended sediment transport was dominated by the mean flux. The mean flux contributed > 70% of total suspended transport on 19 out of the 27 observed rip current occurrences. The net contribution of the oscillatory flux was small compared to the mean flux. Within the oscillatory component, a frequency domain partitioning routine showed that the VLF motion was an important mechanism for driving offshore directed sediment transport. This was balanced by onshore directed sediment transport at incident wave frequency of a similar magnitude. Depth integration showed that the mean total suspended sediment transport was in the range of 0.03 kg/m/s to 0.08 kg/m/s. At high tide, when the rip was inactive suspended sediment transport rates were minimal compared to when the rip was active. Bedform transport was (on average) 6% of the total suspended sediment transport in a rip current. The new results presented here show that rip currents make an important contribution to offshore directed sediment transport. The magnitudes of transport indicate that future improvements to morphology change models should include rip driven offshore sediment transport.
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Cordoba, Gustavo. "Dilute particle-laden currents : dynamics and deposit patterns". Thesis, University of Bristol, 2007. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.495639.

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A numerical model based on the full Navier-Stokes equations is developed to study the dynamics and deposit patterns of turbidity currents. The equation system is simplified using the dilute flow condition which allows one set of momentum equations. The model allows to simulate multiparticle flows in an ambient of pure or sea-water. The solution of the mathematical model is done extending the Characteristic-Based-Split (CBS) Finite Element algorithm to particle-laden flows. The algorithm is implemented by developing a computer program coded in Fortran 90. Additionally, a Box model based on mass balance is developed, which allows to account for the sedimentation, multiple particles and slope changes. Two dimensional and radial flows can be modelled using the proposed Box model just by changing the initial and boundary conditions. The confidence of both the Navier-Stokes based model and the mass-balance based Box model are successfully tested using laboratory experimental data.
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Barrass, Timothy Adam. "Dynamics and sedimentation from axisymmetric, polydisperse gravity currents". Thesis, University of Bristol, 2003. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.288282.

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Girton, James Bannister. "Dynamics of transport and variability in the Denmark Strait overflow /". Thesis, Connect to this title online; UW restricted, 2001. http://hdl.handle.net/1773/11023.

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Gregorio, Sandy O. "Investigation on the dynamics of gravity-driven coastal currents". Thesis, University of Warwick, 2011. http://wrap.warwick.ac.uk/47656/.

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Numerical simulations of buoyant, gravity-driven coastal plumes are summarized and compared to the inviscid geostrophic theory of Thomas & Linden (2007) and to laboratory studies for plumes owing along a vertical-wall coastline (those of Thomas & Linden (2007) and additional experiments performed at Warwick University). In addition, results of two new laboratory studies with different scales for plumes owing along a more realistic inclined-wall coastline are presented and compared to an extended theoretical model from the geostrophic theory of Thomas & Linden (2007). The theoretical and experimental results for plumes flowing along inclined-wall coastlines are compared to the inclined-wall experimental studies of Avicola & Huq (2002), Whitehead & Chapman (1986) and Lentz & Helfrich (2002), to the inclined-wall scaling theory of Lentz & Helfrich (2002), and to oceanic observations. The lengths, widths and velocities of the buoyant gravity currents are studied. Agreement between the laboratory and numerical experiments, and the geostrophic theories for both vertical-wall and inclined-wall studies is found to depend mainly on one non-dimensional parameter which characterizes the strength of horizontal viscous forces (the horizontal Ekman number). The best agreement between the experiments and the geostrophic theories is found for plumes with low viscous forces. At large values of the horizontal Ekman number, laboratory and numerical experiments depart more significantly from theory (e.g., in the plume propagation velocity). At very low values of the horizontal Ekman number (obtained in the large-scale inclined-wall experimental study only), departures between experiments and theory are observed as well. Agreement between experiments and theory is also found to depend on the steepness of the plumes isopycnal interface for the vertical-wall study, and on the ratio between the isopycnal and coastline slopes for the inclined-wall study.
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Meuleners, Michael Joseph. "A numerical study of the mesoscale eddy dynamics of the Leeuwin Current system /". Connect to this title, 2005. http://theses.library.uwa.edu.au/adt-WU2007.0134.

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Libros sobre el tema "Currents dynamics"

1

Turbidity currents: Dynamics, deposits, and reversals. Berlin: Springer-Verlag, 1993.

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Edwards, Deborah Anne, ed. Turbidity Currents: Dynamics, Deposits and Reversals. Berlin/Heidelberg: Springer-Verlag, 1993. http://dx.doi.org/10.1007/bfb0019704.

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Baringer, Molly O'Neil. Mixing and dynamics of the Mediterranean outflow. [Wood Hole, Mass: Woods Hole Oceanographic Institution, Massachusetts Institute of Technology, 1994.

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Signell, Richard Peter. Tidal dynamics and dispersion around coastal headlands: Doctoral dissertation. Woods Hole, Mass: Woods Hole Oceanographic Institution, 1989.

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International Conference on Tidal Dynamics and Environment (2002 Hangzhou, China). Tidal dynamics and environment. Lawrence, Kansas: Coastal Education and Research Foundation, 2004.

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E, Simpson John. Gravity currents: In the environment and the laboratory. Chichester, West Sussex, England: E. Horwood, 1987.

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Gravity currents in the environment and the laboratory. 2a ed. Cambridge, U.K: Cambridge University Press, 1997.

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Center, Goddard Space Flight, ed. The magnetospheric constellation mission: Dynamic Response and Coupling Observatory (DRACO). [Greenbelt, Md.]: NASA, Goddard Space Flight Center, 2002.

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

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Edwards, Christopher A. Dynamics of nonlinear cross-equatorial flow in the deep ocean. Woods Hole, Mass: Massachusetts Institute of Technology, Woods Hole Oceanographic Institution, Joint Program in Oceanography/Applied Ocean Science and Engineering, 1996.

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Capítulos de libros sobre el tema "Currents dynamics"

1

Urrutia, J. M. y R. L. Stenzel. "Laboratory Work on Transient Currents and Its Application to Auroral Arc Currents". En Auroral Plasma Dynamics, 129–32. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm080p0129.

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Hadjsaid, Nouredine, Ion Trisstiu y Lucian Toma. "Short-Circuit Currents Calculation". En Handbook of Electrical Power System Dynamics, 229–90. Hoboken, NJ, USA: John Wiley & Sons, Inc., 2013. http://dx.doi.org/10.1002/9781118516072.ch5.

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Loss, Daniel y Dmitrii L. Maslov. "Persistent Currents and Luttinger Liquids". En Quantum Dynamics of Submicron Structures, 199–210. Dordrecht: Springer Netherlands, 1995. http://dx.doi.org/10.1007/978-94-011-0019-9_16.

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Boyd, John P. "Stratified Models of Mean Currents". En Dynamics of the Equatorial Ocean, 223–48. Berlin, Heidelberg: Springer Berlin Heidelberg, 2017. http://dx.doi.org/10.1007/978-3-662-55476-0_10.

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Zhang, Ling y Robert L. Carovillano. "Plasma Convection and Currents in the Auroral Zone". En Auroral Plasma Dynamics, 89–96. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm080p0089.

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Weidenmüller, Hans A. "Persistent Currents and the Coulomb Interaction". En Quantum Dynamics of Submicron Structures, 183–97. Dordrecht: Springer Netherlands, 1995. http://dx.doi.org/10.1007/978-94-011-0019-9_15.

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Wendler, L. "Persistent Currents in a Few Electron Ring". En Quantum Dynamics of Submicron Structures, 241–44. Dordrecht: Springer Netherlands, 1995. http://dx.doi.org/10.1007/978-94-011-0019-9_19.

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Han, Seon Mi y Haym Benaroya. "Environmental Loading-Waves and Currents". En Nonlinear and Stochastic Dynamics of Compliant Offshore Structures, 95–110. Dordrecht: Springer Netherlands, 2002. http://dx.doi.org/10.1007/978-94-015-9912-2_4.

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Xu, R. L. "Particle Dynamics and Currents in the Magnetotail". En Plasma and the Universe, 257–77. Dordrecht: Springer Netherlands, 1988. http://dx.doi.org/10.1007/978-94-009-3021-6_17.

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Güdde, Jens, Marcus Rohleder, Torsten Meier, Stephan W. Koch y Ulrich Höfer. "Coherently Controlled Electrical Currents at Surfaces". En Dynamics at Solid State Surfaces and Interfaces, 579–91. Weinheim, Germany: Wiley-VCH Verlag GmbH & Co. KGaA, 2010. http://dx.doi.org/10.1002/9783527633418.ch24.

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Actas de conferencias sobre el tema "Currents dynamics"

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Koelling, Stefan. "Electromagnetic currents from chiral EFT". En 6th International Workshop on Chiral Dynamics. Trieste, Italy: Sissa Medialab, 2010. http://dx.doi.org/10.22323/1.086.0108.

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Reniers, Ad, Graham Symonds y Ed Thornton. "Modelling of Rip Currents during RDEX". En Fourth Conference on Coastal Dynamics. Reston, VA: American Society of Civil Engineers, 2001. http://dx.doi.org/10.1061/40566(260)50.

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Osipov, Dmitry S., Dmitry V. Kovalenko y Nadezda N. Dolgikh. "Calculation of currents resonance at higher harmonics in power supply systems based on wavelet packet transform". En 2017 Dynamics of Systems, Mechanisms and Machines (Dynamics). IEEE, 2017. http://dx.doi.org/10.1109/dynamics.2017.8239492.

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Dally, William R. "Modeling Nearshore Currents on Reef-Fronted Beaches". En Fourth Conference on Coastal Dynamics. Reston, VA: American Society of Civil Engineers, 2001. http://dx.doi.org/10.1061/40566(260)57.

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Ranasinghe, Roshan Suminda, Shinji Sato y Yoshimitsu Tajima. "12. MODELING OF WAVES & CURRENTS AROUND POROUS SUBMERGED BREAKWATERS". En Coastal Dynamics 2009 - Impacts of Human Activities on Dynamic Coastal Processes. WORLD SCIENTIFIC, 2009. http://dx.doi.org/10.1142/9789814282475_0015.

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Girshin, S. S., V. N. Goryunov, E. A. Kuznetsov, A. Ya Bigun, E. V. Petrova y A. A. Bubenchikov. "Comparative analysis of insulation-covered and bare conductors of overhead lines with variation of load currents considering weather conditions". En 2016 Dynamics of Systems, Mechanisms and Machines (Dynamics). IEEE, 2016. http://dx.doi.org/10.1109/dynamics.2016.7819012.

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Avdeeva, Ksenia V. "Experimental Research of Stray Currents Influence of DC Railway Transport to Grounding Grid". En 2019 Dynamics of Systems, Mechanisms and Machines (Dynamics). IEEE, 2019. http://dx.doi.org/10.1109/dynamics47113.2019.8944418.

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Lyubimov, V. V. y S. V. Podkletnova. "Damping of Microsatellite Angular Velocity by Means of Magnetic Moments of Foucault Currents". En 2019 Dynamics of Systems, Mechanisms and Machines (Dynamics). IEEE, 2019. http://dx.doi.org/10.1109/dynamics47113.2019.8944456.

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Simons, Richard R. y Ruairi D. MacIver. "Regular, Bichromatic and Random Waves on Co-Linear Currents". En Fourth Conference on Coastal Dynamics. Reston, VA: American Society of Civil Engineers, 2001. http://dx.doi.org/10.1061/40566(260)14.

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Kit, Eliezer y Alexander Perlin. "Computation of Wave Induced Currents Using ``Apparent'' Roughness Concept". En Fourth Conference on Coastal Dynamics. Reston, VA: American Society of Civil Engineers, 2001. http://dx.doi.org/10.1061/40566(260)16.

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Informes sobre el tema "Currents dynamics"

1

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

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

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3

Williamson, C. H. Structure Dynamics, Vortex Dynamics and Fluid Loading on Structures in Waves and Currents. Fort Belvoir, VA: Defense Technical Information Center, agosto de 2003. http://dx.doi.org/10.21236/ada416599.

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

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5

Bialek, J. M. y D. W. Weissenburger. Coupling of mechanical dynamics and induced currents in a cantilever beam. Office of Scientific and Technical Information (OSTI), enero de 1985. http://dx.doi.org/10.2172/6089020.

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6

Poulain, Pierre-Marie. Dynamics of Localized Currents and Eddy Variability in the Adriatic (DOLCEVITA). Fort Belvoir, VA: Defense Technical Information Center, septiembre de 2003. http://dx.doi.org/10.21236/ada629114.

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7

Weissenburger, D. W. y J. M. Bialek. The coupling of mechanical dynamics and induced currents in plates and surfaces. Office of Scientific and Technical Information (OSTI), octubre de 1986. http://dx.doi.org/10.2172/6765195.

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8

Melville, W. K. y Eric Terrill. Airborne Measurements of Whitecap Kinematics and Dynamics in the High-Wind Regime: Source Functions for Marine Aerosols, Surface Currents and Turbulence. Fort Belvoir, VA: Defense Technical Information Center, septiembre de 2003. http://dx.doi.org/10.21236/ada630299.

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9

Evtushenko, Pavel. Large dynamic range beam diagnostics and beam dynamics studies for high current electron LINACs. Office of Scientific and Technical Information (OSTI), octubre de 2016. http://dx.doi.org/10.2172/1467456.

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10

Oltman-Shay, Joan y Uday Putrevu. Nearshore Wave and Current Dynamics. Fort Belvoir, VA: Defense Technical Information Center, septiembre de 1997. http://dx.doi.org/10.21236/ada629340.

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