Relevant bibliographies by topics / Eddies

Academic literature on the topic 'Eddies'

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Published: 4 June 2021
Last updated: 29 July 2024

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Journal articles on the topic "Eddies"

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Wu, Xiaoci, Pengchao Jin, Yang Zhang, and Wei Yu. "Changing Humboldt Squid Abundance and Distribution at Different Stages of Oceanic Mesoscale Eddies." Journal of Marine Science and Engineering 12, no. 4 (April 7, 2024): 626. http://dx.doi.org/10.3390/jmse12040626.

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Humboldt squid, Dosidicus gigas, is one of the main economic cephalopod species off Peruvian waters, and their abundance and distribution are regulated by localized oceanic mesoscale dynamical processes. To this end, the present study employs normalization and frequency distribution methods, combining mesoscale eddy, oceanic environment, and D. gigas fishery data. This is the first exploration into the different stages of mesoscale eddies during their evolution off Peruvian waters and their influence on the regional marine environment, as well as the abundance and distribution of D. gigas resources. The results indicate that across the four stages of eddies, namely formation, intensification, mature, and aged, their kinetic energy and structure follow a pattern of “growth–equilibration–decay”. The abundance of D. gigas within the eddy’s covered zone undergoes an initial increase, followed by a decrease during the evolution of the four stages, peaking during the eddy’s mature stage. The abundance of D. gigas was higher in the anticyclonic eddies than that in the cyclonic eddies under different stages. The environmental factors conducive to D. gigas in eddies exhibited similar changes to D. gigas abundance throughout the eddy’s different stages. Our research emphasizes that anticyclonic eddies, during their evolution, exerted a more significant impact on the abundance and distribution of D. gigas in the Peruvian waters compared with cyclonic eddies. The eddy-induced changes in water temperature and productivity caused by the eddies may be the primary drivers of this impact.
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Early, Jeffrey J., R. M. Samelson, and Dudley B. Chelton. "The Evolution and Propagation of Quasigeostrophic Ocean Eddies*." Journal of Physical Oceanography 41, no. 8 (August 1, 2011): 1535–55. http://dx.doi.org/10.1175/2011jpo4601.1.

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Abstract The long-term evolution of initially Gaussian eddies is studied in a reduced-gravity shallow-water model using both linear and nonlinear quasigeostrophic theory in an attempt to understand westward-propagating mesoscale eddies observed and tracked by satellite altimetry. By examining both isolated eddies and a large basin seeded with eddies with statistical characteristics consistent with those of observed eddies, it is shown that long-term eddy coherence and the zonal wavenumber–frequency power spectral density are best matched by the nonlinear model. Individual characteristics of the eddies including amplitude decay, horizontal length scale decay, and zonal and meridional propagation speed of a previously unrecognized quasi-stable state are examined. The results show that the meridional deflections from purely westward flow (poleward for cyclones and equatorward for anticyclones) are consistent with satellite observations. Examination of the fluid transport properties of the eddies shows that an inner core of the eddy, defined by the zero relative vorticity contour, contains only fluid from the eddy origin, whereas a surrounding outer ring contains a mixture of ambient fluid from throughout the eddy’s lifetime.
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Liu, Jiaxin, Jue Ning, and Xu Chen. "Evolution of Different Types of Eddies Originating from Different Baroclinic Instability Types." Remote Sensing 15, no. 24 (December 14, 2023): 5730. http://dx.doi.org/10.3390/rs15245730.

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This paper investigates the evolution of global eddies and various types of eddies originating from baroclinic instability (BCI) by utilizing satellite altimetry, Argo profiles, and climatology datasets. The structure of global eddies with regard to potential temperature anomalies experiences downward propagation and spreading from the periods of eddy growth to stabilization. However, from the eddy’s stabilization to the decay period, the process of spreading primarily occurs horizontally, and this process is usually accompanied by weakening. By comparing the evolution of eddies in three typical regions dominated by distinct types of BCI, we found that the basic properties of eddies related to different BCI types evolve similarly; however, there are notable differences in their vertical structures and evolution. Eddies associated with Phillips + Charney_s-type, Charney_s-type, and Eady-type BCIs exhibit dual-core, single-core, and dual-core structures, respectively. In particular, the intrusion of the Okhotsk cold water mass into the Northwest Pacific region forms cold-core anticyclonic eddies, resulting in AEs that are significantly distinct from the rest of the ocean. The evolution of surface-layer cores closely resembles that of the global eddies, while the decay of subsurface and bottom-layer cores is comparably sluggish. Additionally, we examine the impact of local oceanic stratification conditions on eddy decay and determine that stronger vertical gradients result in more vigorous eddy decay, accounting for the concentration of eddies at depths where vertical gradients are weaker during their evolution.
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Avnur, Ron, and Joseph M. Hellerstein. "Eddies." ACM SIGMOD Record 29, no. 2 (June 2000): 261–72. http://dx.doi.org/10.1145/335191.335420.

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Yuan, Quanmu, and Jianyu Hu. "Spatiotemporal Characteristics and Volume Transport of Lagrangian Eddies in the Northwest Pacific." Remote Sensing 15, no. 17 (September 4, 2023): 4355. http://dx.doi.org/10.3390/rs15174355.

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Mesoscale eddies play a crucial role in the transport of mass, heat, salt and nutrients, exerting significant influence on ocean circulation patterns, biogeochemical processes and the global climate system. Based on Lagrangian-Averaged Vorticity Deviation (LAVD) method, this study applies 27 years (1993–2019) of geostrophic current velocity data to detect Rotationally Coherent Lagrangian Vortices (RCLVs) in the Northwest Pacific (NWP; 10°N–30°N, 115°E–155°E), with the spatiotemporal characteristics of Eulerian Sea Surface Height Eddies (SSH eddies) and RCLVs being compared. A higher number of SSH eddies and RCLVs can be observed in spring and winter, and their inter-annual variations are similar. SSH eddies show higher generation number and larger radius in the Subtropical Countercurrent region, while RCLVs occur more favorably in the ocean basin. The propagation speed distributions of both eddy types are nearly identical and decrease with increasing latitude. Due to the material coherent transport maintained by RCLVs within a finite time interval, the coherent cores of RCLVs are considerably smaller in scale as compared to those of SSH eddies. The average zonal transports induced by SSH eddies and RCLVs are estimated to be −0.82 Sv and −0.51 Sv (1 Sv = 106 m3/s), respectively. For non-overlapping SSH eddies with RCLVs, approximately 80% of the water within the eddy leaks out during the eddy’s lifespan. In the case of overlapping SSH eddies, the ratio of coherent water inside the eddy decreases with increasing radius, and the leakage rate is around 58%. Finally, an examination of 36 shedding RCLVs events from the Kuroshio near the Luzon Strait, which induce an average zonal transport of −0.14 Sv, reveals that 54% of the water within the shedding RCLVs originates from the Kuroshio.
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Lai, Yeping, Hao Zhou, Jing Yang, Yuming Zeng, and Biyang Wen. "Submesoscale Eddies in the Taiwan Strait Observed by High-Frequency Radars: Detection Algorithms and Eddy Properties." Journal of Atmospheric and Oceanic Technology 34, no. 4 (April 2017): 939–53. http://dx.doi.org/10.1175/jtech-d-16-0160.1.

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AbstractThis study compared the efficiencies of two widely used automatic eddy detection algorithms—that is, the winding-angle (WA) method and the vector geometry (VG) method—and investigated the submesoscale eddy properties using surface current observations derived from high-frequency radars (HFRs) in the Taiwan Strait. The results showed that the WA method using the streamline and the VG method based on the streamfunction field have almost the same capacity for identifying eddies, but the former is more competent than the latter in capturing the eddy size. The two algorithms simultaneously identified 1080 submesoscale eddies, with the centers and boundaries determined only by the WA method, and they were further used to investigate the eddy properties. In general, no significant difference was observed between the cyclonic and anticyclonic eddies in terms of radius, life span, and kinematics, as well as the evolution during their life cycles. The typical radius of the eddy in this region was 3–18 km. And a strong correlation was observed between the life span and the radius. The spatial distribution of the eddies indicated that topography played a significant role in the generation of the eddies. And the trajectories of the eddies suggested that all the eddies in this area mostly tended to move southeastward. Statistically, three different stages of the eddy’s life span could be identified by the significant growth and decay of the radius and the mean kinetic energy. This study shows the great capability of HFRs in oceanography research and applications, especially for observing the submesocale dynamics.
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Huang, Xiaorong, and Guihua Wang. "Response of a Mesoscale Dipole Eddy to the Passage of a Tropical Cyclone: A Case Study Using Satellite Observations and Numerical Modeling." Remote Sensing 14, no. 12 (June 15, 2022): 2865. http://dx.doi.org/10.3390/rs14122865.

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Mesoscale eddies occurring in the world’s oceans typically exist in pairs known as mesoscale dipole eddies or simply dipole eddies. Tropical cyclones (hereafter TCs) that move over the world’s oceans often encounter and interact with these dipole eddies. Through this interaction, TCs induce significant perturbations in the mesoscale eddies. However, the specific influences that the passage of a TC on a dipole eddy have not been addressed. In this paper, a case study of the dipole eddy’s response to the passage of a TC is conducted by using satellite observations and numerical simulation. The passage of a TC induces a long-duration response in the dipole eddy. First, the cyclonic ocean eddy component (COE) of the dipole is amplified, and the anticyclonic ocean eddy component (AOE) is weakened or even destroyed during the interaction. The amplification of the COE and weakening of the AOE primarily manifests as a change in their amplitudes and radii and as the adjustment of their vertical structure. The dipole eddy’s response to the interaction with a TC manifests as an upwelling anomaly and the injection of positive relative vorticity. Following the passage of the TC, the COE gradually stabilizes, and AOE slowly recovers after the disturbance energy from the interaction dissipates, which facilitates the reestablishment of the dipole eddy. The dipole reaches an equilibrium state through a quasi-geostrophic adjustment process. As a consequence, the overall effect of the interaction of the dipole with the TC leads to an asymmetric signature on the dipole eddy. The eddy–eddy interaction in a dipole may allow it to stabilize in a shorter time relative to that of a solitary eddy.
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Monin, A. S., and G. M. Zhikharev. "Ocean eddies." Uspekhi Fizicheskih Nauk 160, no. 5 (1990): 1. http://dx.doi.org/10.3367/ufnr.0160.199005a.0001.

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Monin, A. S., and G. M. Zhikharev. "Ocean eddies." Soviet Physics Uspekhi 33, no. 5 (May 31, 1990): 313–39. http://dx.doi.org/10.1070/pu1990v033n05abeh002569.

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Eldevik, Tor, and Kristian B. Dysthe. "Spiral Eddies." Journal of Physical Oceanography 32, no. 3 (March 2002): 851–69. http://dx.doi.org/10.1175/1520-0485(2002)032<0851:se>2.0.co;2.

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Dissertations / Theses on the topic "Eddies"

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Abernathey, Ryan (Ryan Patrick). "Mixing by ocean eddies." Thesis, Massachusetts Institute of Technology, 2012. http://hdl.handle.net/1721.1/70772.

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Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 2012.
Cataloged from PDF version of thesis.
Includes bibliographical references (p. 163-175).
Mesoscale eddies mix and transport tracers such as heat and potential vorticity laterally in the ocean. While this transport plays an important role in the climate system, especially in the Southern Ocean, we lack a, comprehensive understanding of what sets mixing rates. This thesis seeks to advance this understanding through three related studies. First, mixing rates are diagnosed from an eddy-resolving state estimate of the Southern Ocean, revealing a meridional cross-section of effective diffusivity shaped by the interplay between eddy propagation and mean flow. Effective diffusivity diagnostics are then applied to quantify surface mixing rates globally, using a, kinematic model with velocities derived from satellite observations; the diagnosed mixing rates show a rich spatial structure, with especially strong mixing in the tropics and western-boundary-current regions. Finally, an idealized numerical model of the Southern Ocean is analyzed, focusing on the response to changes in win( stress. The sensitivity of the meridional overturning circulation to the wind changes demonstrates the importance of properly capturing eddy mixing rates for large-scale climate problems.
by Ryan Abernathey.
Ph.D.
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Cenedese, Claudia. "Baroclinic eddies over topography." Thesis, University of Cambridge, 1999. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.624104.

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Athanasiadis, Panos J. "Teleconnections and transient eddies." Thesis, University of Reading, 2007. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.493965.

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The subject of this thesis is the dynamics of teleconnections and mid-latitude stationary eddies, key components of the structure and variability of the extratropical general circulation. Deepening our understanding of their dynamics is of particular importance in the context of predicting and explaining possible climate changes.
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Haines, K. "Long-lived eddies in planetary atmospheres." Thesis, Imperial College London, 1987. http://hdl.handle.net/10044/1/38343.

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An, Byoung Woong. "Modelling outflows, coastal currents and eddies." Thesis, University College London (University of London), 2004. http://discovery.ucl.ac.uk/1446475/.

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Several types of flows driven by outflows on the continental shelf are examined mathematically and numerically. Within a quasigeostrophic framework, a variety of vertical structures and topographies are used. Features are explained in terms of potential vorticity conservation. The combined effects of topography and anomalous vorticity of the outflow are studied. First, shelf-like topography is considered. The role of topographic wave radiation is studied using the linearised barotropic potential vorticity equation for a weak outflow with zero vorticity. Contour dynamics is used for stronger outflows with relative vorticity. Next, the effects of anomalous vorticity in driving such coastal currents are studied using 11/2-layer model and its interaction with topography. Simulations show that the strong tendency for the development of anticyclonic eddy near topographic change. Two-layer outflows and their interaction with topography are examined. Purely buoyancy driven outflows are considered in which only one of two layers enters the flow domain. Purely barotropic outflows are also considered. Simulations show the development of eddies by interaction with topography in the lower fluid. The effect of topography whose gradient lies perpendicular to the coastline on coastal currents and eddies is investigated. The formation of dipole eddies is found to be a robust feature when the coastal current interacts with the topography depending on the sign of the topographic gradient. The stability of a two-layer converging/diverging coastal jet associated with piecewise constant potential vorticity is studied numerically. Baroclinic instability is demonstrated. The origin of the instability appears first at the coast, and may explain the meandering and eddying associated with detaching western boundary currents. The final study revisits the barotropic outflow problem. Owing to boundary layer separation at the exit, the outflow may consist of a dipolar structure. The interaction of this dipole with shelf-like topography is studied numerically.
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Burns, Helen. "Diabatic eddies in idealised channel models." Thesis, University of Southampton, 2018. https://eprints.soton.ac.uk/424757/.

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The Southern Ocean is a unique and climatically important region where mesoscale eddies are of first order importance. The circulation of the Southern Ocean controls the amount of carbon stored in the ocean and is an integral part of the worlds global overturning circulation. It is therefore of great importance to understand the dynamics of the Southern Ocean and the possible response of the overturning circulation to changing forcing i.e. climate change. Because of the role eddies play in setting that circulation, the dynamics are still not fully understood. This thesis explores one poorly understood aspect of the Southern Ocean; dia- batic eddies. Using the Massachusetts Institute of Technology General Circulation Model (MITgcm) to set up an idealised channel we close the northern boundary which causes the Southern Ocean overturning to collapse. This is to be expected as the circulation is part of the global overturning and must be connected to the rest of the world’s ocean. We use Transformed Eulerian Mean (TEM) theory to suggest this collapse is achieved via diabatic eddies altering the effective surface buoyancy forcing. We then alter the northern boundary condition to show that diabatic eddies can be related to the northern boundary stratification. However the response of the diabatic eddies is also dependent on the surface forcing, partic- ularly the sense of the forcing: changing from fixed-fluxes to surface restoring can have dramatic effects. Surface restoring alters the dynamics of the mixed layer, eddy compensation and saturation. This suggests that when exploring Southern Ocean dynamics in regional models, the effect of the imposed boundary conditions must always be considered. Our results suggest if the background stratification is altered we may see a very different circulation in the Southern Ocean, but to what extent would also depend on the response of the atmosphere and hence the surface forcing.
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Hall, C. "Cyclonic Eddies in the Cape Basin." Master's thesis, University of Cape Town, 2008. http://hdl.handle.net/11427/6586.

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A great deal of attention has been paid to the inter-ocean exchange of thermohalineproperties in the Agulhas Retroflection region. Recent observations have shown thatthe highly energetic field of the southern half of the Cape Basin consists of bothcyclonic and anticyclonic eddies. These eddies interact with each other, resulting inthe vigorous stirring of these water mass. Investigations have shown that the cycloniceddies tend to be smaller and outnumber the anticyclonic rings. Nonetheless, verylittle is known of their characteristics and the nature in which they are formed. Usingremote sensing data, confirmed with hydrographic data, this study determines thelocation, frequency and seasonality of cyclonic eddy formation; their size, trajectoriesand lifespan; physical components and associations with Agulhas Rings.Cyclonic eddies were seen to split, merge and link with other cyclonic eddies, withsplitting events creating child cyclonic eddies. The 105 parent and 157 child cycloniceddies identified during this study show that an average of II parent and 17 childcyclonic eddies were formed annually. 31.58 % follow an overall west-southwestdirection, with 27.37 % translocating west north-westward. Poleward translocationspeeds average at 0.3 kIn/day, whereas translocation speeds obtained from alldirectional components averages at 2.153 kIn/day for parent and 2.975 km/day forchild cyclonic eddies. Parent cyclonic eddies lived for approximately 254 days,whereas child cyclonic eddies survived for a mean of 188 days. Of note was asignificant variation of lifespan between parent and child cyclonic eddies formed inboth the north and south of the study area. 77 % of northern and 93 % of southerncyclonic eddies were formed directly adjacent to positive sea level anomalies orAgulhas Rings, resulting in an total overall association of 82.93 % parent and 89.63 %child cyclonic eddies. Cyclonic eddy groups were seen to merge at a rate of 16.38parent and 14 child cyclonic eddies per year, whereas topography appeared to affectthe demise of 17.00 % of the investigated cyclonic eddies.Therefore this study may form a basis for further investigations into the influenceCape Basin cyclonic eddies have on the meridional transfer of heat, salt, nutrients,oxygen and carbon concentrations in the South-East Atlantic Ocean. A more in-depthstudy using model outputs and targeted in situ hydrographical data would againenhance cyclonic eddy knowledge.
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Ring, Michael J. 1979. "The role of eddies in buoyancy flux." Thesis, Massachusetts Institute of Technology, 2001. http://hdl.handle.net/1721.1/114316.

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Thesis: S.B., Massachusetts Institute of Technology, Department of Earth, Atmospheric, and Planetary Sciences, 2001.
Thesis: S.B., Massachusetts Institute of Technology, Department of Physics, 2001.
Cataloged from PDF version of thesis.
Includes bibliographical references (page 35).
This thesis explores the role of eddies in determining the stratification of the ocean through a laboratory experiment. The experiment uses a dual-tank apparatus, with a smaller tank sitting inside the larger tank. Both tanks sit on a rotating turntable, which simulates the rotation of Earth. During the experiment, salty water is pumped from the outer tank through small holes in the base of the inner tank, which is initially filled with fresh water. The evolution of the dense fluid in the inner tank is observed, with particular regard to the number of eddies that form. These observations are checked against theoretical predictions, derived from analysis of buoyancy flux, for the number of eddies expected to form.
by Michael J. Ring.
S.B.
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Lewis, Stephen Richard. "Long-lived eddies in the atmosphere of Jupiter." Thesis, University of Oxford, 1988. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.329956.

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Miltenberger, Alexander Reid. "The effects of ocean eddies on tropical cyclones." Thesis, Massachusetts Institute of Technology, 2012. http://hdl.handle.net/1721.1/78538.

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Thesis (S.M.)--Joint Program in Oceanography/Applied Ocean Science and Engineering (Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences; and the Woods Hole Oceanographic Institution), 2012.
Cataloged from PDF version of thesis.
Includes bibliographical references (p. 40-41).
The purpose of this study is to understand the interactions of tropical cyclones with ocean eddies. In particular we examine the influence of a cold-core eddy on the cold wake formed during the passage of Typhoon Fanapi (2010). The three-dimensional version of the numerical Price-Weller-Pinkel (PWP) vertical mixing model has previously been used to simulate and study the cold wakes of Atlantic hurricanes. The model has not been used in comparison with observations of typhoons in the Western Pacific Ocean. In 2010 several typhoons were studied during the Impact of Typhoons on the Ocean in the Pacific (ITOP) field campaign and Fanapi was particularly well observed. We use these observations and the 3DPWP to understand the ocean cold wake generated by Fanapi. The cold wake of Fanapi was advected by a cyclonic eddy that was south of the typhoon track. The 3DPWP model outputs with and without an eddy are compared with observations made during the field campaign. These observations are compared to model outputs with eddies in a series of positions right and left of the storm track in order to study effects of mesoscale eddies on ocean vertical mixing in the cold wake of typhoons.
by Alexander Reid Miltenberger.
S.M.
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Books on the topic "Eddies"

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Drvenkar, Zoran. Eddies erste Lügengeschichte. Hamburg, Germany: Oetinger, 2000.

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Drvenkar, Zoran, and Barbara Scholz. Eddies zweite Lügengeschichte. Hamburg, Germany: Oetinger, 2002.

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E, Taslim Mohammad, Hung Shi Chang, and United States. National Aeronautics and Space Administration. Scientific and Technical Information Branch., eds. Numerical study of large-eddy breakup and its effect on the drag characteristics of boundary layers. Tucson, Ariz: University of Arizona, 1985.

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E, Taslim Mohammad, Hung Shi Chang, and United States. National Aeronautics and Space Administration. Scientific and Technical Information Branch., eds. Numerical study of large-eddy breakup and its effect on the drag characteristics of boundary layers. Tucson, Ariz: University of Arizona, 1985.

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Foiaş, Ciprian. On the interaction of small and large eddies in two dimensional turbulent flows. Hampton, Va: National Aeronautics and Space Administration, Langley Research Center, 1987.

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Kamenkovich, V. M., M. N. Koshlyakov, and A. S. Monin, eds. Synoptic Eddies in the Ocean. Dordrecht: Springer Netherlands, 1986. http://dx.doi.org/10.1007/978-94-009-4502-9.

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Kamenkovich, V. M. Sinopticheskie vikhri v okeane. 2nd ed. Leningrad: Gidrometeoizdat, 1987.

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Joseph, Gutowski William, and United States. National Aeronautics and Space Administration., eds. The impact of greenhouse climate change on the energetics and hydrologic processes of mid-latitude transient eddies. [Washington, D.C: National Aeronautics and Space Administration, 1991.

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Morozov, E. G., and V. G. Kort. Vikhri i vnutrennie volny v okeane. Moskva: Mezhduvedomstvennyĭ geofizicheskiĭ kom-t pri Prezidiume Akademii nauk SSSR, 1988.

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N, Fedorov K., ed. Vnutritermoklinnye vikhri v okeane. Moskva: Akademii͡a︡ nauk SSSR, In-t okeanologii im. P.P. Shirshova, 1986.

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Book chapters on the topic "Eddies"

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Tolmazin, David. "Countercurrents and eddies." In Elements of Dynamic Oceanography, 115–27. Dordrecht: Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-4856-3_6.

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Gangopadhyay, Avijit. "Turbulence and Eddies." In Introduction to Ocean Circulation and Modeling, 201–22. Boca Raton: CRC Press, 2022. http://dx.doi.org/10.1201/9780429347221-9.

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Robinson, Ian S. "Mesoscale ocean features: Eddies." In Discovering the Ocean from Space, 69–114. Berlin, Heidelberg: Springer Berlin Heidelberg, 2010. http://dx.doi.org/10.1007/978-3-540-68322-3_3.

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Kamenkovich, V. M., M. N. Koshlyakov, and A. S. Monin. "Theory of Ocean Eddies." In Synoptic Eddies in the Ocean, 131–207. Dordrecht: Springer Netherlands, 1986. http://dx.doi.org/10.1007/978-94-009-4502-9_3.

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Zohar, Y., and C. M. Ho. "Small Eddies in Large Vortices." In Separated Flows and Jets, 665–70. Berlin, Heidelberg: Springer Berlin Heidelberg, 1991. http://dx.doi.org/10.1007/978-3-642-84447-8_82.

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Langlois, William E., and Michel O. Deville. "Stokes Flow and Corner Eddies." In Slow Viscous Flow, 293–305. Cham: Springer International Publishing, 2013. http://dx.doi.org/10.1007/978-3-319-03835-3_12.

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Berman, Neil S. "Large Eddies and Polymer Strings." In Structure of Turbulence and Drag Reduction, 275–81. Berlin, Heidelberg: Springer Berlin Heidelberg, 1990. http://dx.doi.org/10.1007/978-3-642-50971-1_24.

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Pennell, Summer Melody. "Moments of Active Reflection: Eddies." In Queering Critical Literacy and Numeracy for Social Justice, 73–88. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-11584-5_5.

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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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Kamenkovich, V. M., M. N. Koshlyakov, and A. S. Monin. "Eddies in the Open Ocean." In Synoptic Eddies in the Ocean, 265–376. Dordrecht: Springer Netherlands, 1986. http://dx.doi.org/10.1007/978-94-009-4502-9_5.

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Conference papers on the topic "Eddies"

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Avnur, Ron, and Joseph M. Hellerstein. "Eddies." In the 2000 ACM SIGMOD international conference. New York, New York, USA: ACM Press, 2000. http://dx.doi.org/10.1145/342009.335420.

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BRADLEY, SG, and S. VON HÜNERBEIN. "SOUND SCATTERING BY LARGE EDDIES." In Spring Conference Acoustics 2002. Institute of Acoustics, 2023. http://dx.doi.org/10.25144/18255.

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S, Akash, Charu Harshini K, and Amsaveni A. "Eddies Detection Using Hyperspectral Imaging." In 2024 1st International Conference on Trends in Engineering Systems and Technologies (ICTEST). IEEE, 2024. http://dx.doi.org/10.1109/ictest60614.2024.10576125.

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Cooper, Cortis K., James B. Stear, Sergei Frolov, Lee Gordon, Darryl Symonds, and Michael J. Vogel. "The Case Against Severe Cold Eddies." In Offshore Technology Conference. Offshore Technology Conference, 2008. http://dx.doi.org/10.4043/19618-ms.

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Belonenko, Tatyana. "WHAT�ARE�THEY:�EDDIES�OR�WAVES?" In SGEM2012 12th International Multidisciplinary Scientific GeoConference and EXPO. Stef92 Technology, 2012. http://dx.doi.org/10.5593/sgem2012/s06.v2017.

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Moschos, Evangelos, Olivier Schwander, Alexandre Stegner, and Patrick Gallinari. "Deep-SST-Eddies: A Deep Learning Framework to Detect Oceanic Eddies in Sea Surface Temperature Images." In ICASSP 2020 - 2020 IEEE International Conference on Acoustics, Speech and Signal Processing (ICASSP). IEEE, 2020. http://dx.doi.org/10.1109/icassp40776.2020.9053909.

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He, W., M. Tanahashi, and T. Miyauchi. "Fine Scale Structure of High Reynolds Number Taylor-Couette Flow." In ASME/JSME 2007 5th Joint Fluids Engineering Conference. ASMEDC, 2007. http://dx.doi.org/10.1115/fedsm2007-37172.

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Abstract:
Direct numerical simulation (DNS) has been conducted to investigate turbulence transition process and fine scale structures in Taylor-Couette flow. Fourier-Chebyshev spectral methods have been used for spatial discretization and DNS are conducted up to Re = 12000. With the increase of Reynolds number, fine scale eddies are formed in a stepwise fashion. In relatively weak turbulent Taylor-Couette flow, fine scale eddies elongated in the azimuthal direction appear near the outflow and inflow boundaries between Taylor vortices. These fine scale eddies in the outflow and inflow boundaries are inclined at about −45/135 degree with respect to the azimuthal direction. With the increase of Reynolds number, the number of fine scale eddies increases and fine scale eddies appear in whole flow fields. The Taylor vortices in high Reynolds number organize lots of fine scale eddies. In high Reynolds number Taylor-Couette flow, fine scale eddies parallel to the axial direction are formed in sweep regions between large scale Taylor vortices. The most expected diameter and maximum azimuthal velocity of coherent fine scale eddies are 8 times of Kolmogorov scale and 1.7 times of Kolmogorov velocity respectively for high Reynolds Taylor-Couette flow. This scaling law coincides with that in other turbulent flow fields.
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Li, Li, and Robert A. Dalrymple. "The Horizontal Eddies in the Offshore Zone." In 26th International Conference on Coastal Engineering. Reston, VA: American Society of Civil Engineers, 1999. http://dx.doi.org/10.1061/9780784404119.012.

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Paes, Rosa Cristhyna, Gutemberg Franca, Victor Daher, Angelo Sartori, and Nelson Ebecken. "Methodology for eddies recognition from satellite images." In IGARSS 2010 - 2010 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2010. http://dx.doi.org/10.1109/igarss.2010.5653695.

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Liu, W. Timothy, and Xiaosu Xie. "Wind/stress feedback to mesoscale ocean eddies." In 2017 IEEE International Geoscience and Remote Sensing Symposium (IGARSS). IEEE, 2017. http://dx.doi.org/10.1109/igarss.2017.8127413.

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Reports on the topic "Eddies"

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Cushman-Roisin, Benoit. Mesoscale Eddies and Fronts. Fort Belvoir, VA: Defense Technical Information Center, January 1991. http://dx.doi.org/10.21236/ada231933.

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Lopez, Jose M., Jorge E. Corredor, Julio M. Morell, Jorge E. Capella, and Fernando Gilbes. Characterization of Caribbean Meso-Scale Eddies. Fort Belvoir, VA: Defense Technical Information Center, September 2006. http://dx.doi.org/10.21236/ada611897.

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Muller, Peter. Stochastic Forcing of Quasi-Geostrophic Eddies. Fort Belvoir, VA: Defense Technical Information Center, February 1996. http://dx.doi.org/10.21236/ada327549.

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Lopez, Jose M., Jorge E. Corredor, Julio M. Morell, Jorge E. Capella, and Fernando Gilbes. Characterization of Caribbean Meso-Scale Eddies. Fort Belvoir, VA: Defense Technical Information Center, September 2003. http://dx.doi.org/10.21236/ada629466.

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Lopez, Jose M., Jorge E. Corredor, Julio M. Morell, Jorge E. Capella, and Fernando Gilbes. Characterization of Caribbean Meso-Scale Eddies. Fort Belvoir, VA: Defense Technical Information Center, September 2007. http://dx.doi.org/10.21236/ada550732.

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Aspliden, C. I., L. L. Wendell, K. S. Clem, and G. L. Gower. Boundary layer eddies at the Goodnoe Hills site. Office of Scientific and Technical Information (OSTI), May 1991. http://dx.doi.org/10.2172/5562018.

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Blackwelder, Ron F. Some Ideas on the Control of Near-Wall Eddies. Fort Belvoir, VA: Defense Technical Information Center, January 1989. http://dx.doi.org/10.21236/ada207819.

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Barth, John A. Mapping Jets and Eddies in an Eastern Boundary Current. Fort Belvoir, VA: Defense Technical Information Center, August 1997. http://dx.doi.org/10.21236/ada328754.

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Huyer, Adriana, P. M. Kosro, Jack A. Barth, and Robert L. Smith. Mapping Jets and Eddies in an Eastern Boundary Current. Fort Belvoir, VA: Defense Technical Information Center, September 1997. http://dx.doi.org/10.21236/ada627847.

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Huyer, Adriana, P. Michael Kosro, Jack A. Barth, and Robert L. Smith. Mapping Jets and Eddies in an Eastern Boundary Current. Fort Belvoir, VA: Defense Technical Information Center, April 1998. http://dx.doi.org/10.21236/ada342961.

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