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cooler cyclones. Even though these anticyclonic eddies resulted in lower levels of chlorophyll in comparison to the cyclonic eddies, the warmer waters at deeper depths may allow for a deeper mixed layer and higher concentration of diatoms which in turn result in higher rates of primary productivity. Furthermore, the prey populations could be distributed more within these eddies attracting these larger female sharks to forage in this mesopelagic zone. This diving pattern may follow a diel vertical migration but without more evidence on the biomass of their prey within this zone, these conclusions cannot be made only using this circumstantial evidence.
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formulate remediation strategies for pollution events. Eddy formations play a vital role in the fate and transport of solutes and particles in environmental flows such as in rivers, lakes, oceans, and the atmosphere. Upwelling in stratified coastal estuaries warrant the formation of dynamic eddies which distribute nutrients out from beneath the boundary layer to form plumes. Shallow waters, such as those along the coast, play a complex role in the transport of nutrients and pollutants due to the proximity of the upper-boundary driven by the wind and the lower-boundary near the bottom of the water body.
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Satellite Archival Transmitting tags (PSAT) to track the movement and diving behavior of two female white sharks (Carcharodon carcharias) within the eddies. The eddies were defined using sea surface height (SSH) and contours using the horizontal speed-based radius scale. This study found that the white sharks dove in both cyclones but favored the anticyclone which had three times more dives as the cyclonic eddies. Additionally, in the Gulf Stream eddies, the anticyclonic eddies were 57% more common and had more dives and deeper dives than the open ocean eddies and Gulf Stream cyclonic eddies.
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934:, are essential for the preservation of ecosystems, oil and other pollutants are also mixed in the current flow and can carry pollution far from its origin. Eddy formations circulate trash and other pollutants into concentrated areas which researchers are tracking to improve clean-up and pollution prevention. The distribution and motion of plastics caused by eddy formations in natural water bodies can be predicted using Lagrangian transport models. Mesoscale ocean eddies play crucial roles in transferring heat poleward, as well as maintaining heat gradients at different depths.
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These mesoscale eddies have shown to be beneficial in further creating ecosystem-based management for food web models to better understand the utilization of these eddies by both the apex predators and their prey. Gaube et al. (2018), used “Smart” Position or
Temperature Transmitting tags (SPOT) and
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Lift and drag properties of golf balls are customized by the manipulation of dimples along the surface of the ball, allowing for the golf ball to travel further and faster in the air. The data from turbulent-flow phenomena has been used to model different transitions in fluid flow regimes, which are
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is the study of blood flow in the circulatory system. Blood flow in straight sections of the arterial tree are typically laminar (high, directed wall stress), but branches and curvatures in the system cause turbulent flow. Turbulent flow in the arterial tree can cause a number of concerning effects,
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conducted a fluid dynamics experiment involving water and dye, where he adjusted the velocities of the fluids and observed the transition from laminar to turbulent flow, characterized by the formation of eddies and vortices. Turbulent flow is defined as the flow in which the system's inertial forces
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flow regime. The moving fluid creates a space devoid of downstream-flowing fluid on the downstream side of the object. Fluid behind the obstacle flows into the void creating a swirl of fluid on each edge of the obstacle, followed by a short reverse flow of fluid behind the obstacle flowing upstream,
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region. Moreover, further understanding this region in the open ocean and how the removal of fish in this region may impact this pelagic food web is crucial for the fish populations and apex predators that may rely on this food source in addition to making better ecosystem-based management plans.
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Within these anticyclonic eddies, the isotherm was displaced 50 meters downward allowing for the warmer water to penetrate deeper in the water column. This warmer water displacement may allow for the white sharks to make longer dives without the added energetic cost from thermal regulation in the
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phytoplankton, as well as, supported by areas of increased vertical nutrient fluxes and transportation of biological communities. This area of the
Atlantic is also thought to be an ocean desert, which creates an interesting paradox due to it hosting a variety of large pelagic fish populations and
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Modeling eddy development, as it relates to turbulence and fate transport phenomena, is vital in grasping an understanding of environmental systems. By understanding the transport of both particulate and dissolved solids in environmental flows, scientists and engineers will be able to efficiently
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The biomass in the mesopelagic zone is still understudied leading to the biomass of fish within this layer to potentially be underestimated. A more accurate measurement on this biomass may serve to benefit the commercial fishing industry providing them with additional fishing grounds within this
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McGillicuddy, D. J., Anderson, L. A., Bates, N. R., Bibby, T., Buesseler, K. O., Carlson, C. A., Davis, C. S., Ewart, C., Falkowski, P. G., Goldthwait, S. A., Hansell, D. A., Jenkins, W. J., Johnson, R., Kosnyrev, V. K., Ledwell, J. R., Li, Q. P., Siegel, D. A., & Steinberg, D. K. (2007).
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Because eddies may have a vigorous circulation associated with them, they are of concern to naval and commercial operations at sea. Further, because eddies transport anomalously warm or cold water as they move, they have an important influence on heat transport in certain parts of the ocean.
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The sub-tropical
Northern Atlantic is known to have both cyclonic and anticyclonic eddies that are associated with high surface chlorophyll and low surface chlorophyll, respectively. The presence of chlorophyll and higher levels of chlorophyll allows this region to support higher biomass of
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Gaube, P., Braun, C. D., Lawson, G. L., McGillicuddy, D. J., Penna, A. della, Skomal, G. B., Fischer, C., & Thorrold, S. R. (2018). Mesoscale eddies influence the movements of mature female white sharks in the Gulf Stream and
Sargasso Sea. Scientific Reports, 8(1).
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showing the thermal convection plume rising from an ordinary candle in still air. The plume is initially laminar, but transition to turbulence occurs in the upper third of the image. The image was made by Gary
Settles using a one-meter-diameter schlieren
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Gaube, P., McGillicuddy, D. J., Chelton, D. B., Behrenfeld, M. J., & Strutton, P. G. (2014). Regional variations in the influence of mesoscale eddies on near-surface chlorophyll. Journal of
Geophysical Research: Oceans, 119(12).
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Eddies are common in the ocean, and range in diameter from centimeters to hundreds of kilometers. The smallest scale eddies may last for a matter of seconds, while the larger features may persist for months to years.
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in the linear constitutive relation is required by tensorial algebra purposes when solving for two-equation turbulence models (or any other turbulence model that solves a transport equation for
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Chelton, D. B., Gaube, P., Schlax, M. G., Early, J. J., & Samelson, R. M. (2011). The influence of nonlinear mesoscale eddies on near-surface oceanic chlorophyll. Science, 334(6054).
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A diagram showing the velocity distribution of a fluid moving through a circular pipe, for laminar flow (left), time-averaged (center), and turbulent flow, instantaneous depiction (right)
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Mesoscale ocean eddies are characterized by currents that flow in a roughly circular motion around the center of the eddy. The sense of rotation of these currents may either be
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including atherosclerotic lesions, postsurgical neointimal hyperplasia, in-stent restenosis, vein bypass graft failure, transplant vasculopathy, and aortic valve calcification.
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Mesoscale eddies can be split into two categories: static eddies, caused by flow around an obstacle (see animation), and transient eddies, caused by baroclinic instability.
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Eddies that are between about 10 and 500 km (6 and 300 miles) in diameter and persist for periods of days to months are known in oceanography as mesoscale eddies.
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236:, a unit-less number used to determine when turbulent flow will occur. Conceptually, the Reynolds number is the ratio between inertial forces and viscous forces.
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Oceanic and atmospheric currents transfer particles, debris, and organisms all across the globe. While the transport of organisms, such as
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around a cylinder. This can occur around cylinders and spheres, for any fluid, cylinder size and fluid speed, provided that the flow has a
776:{\displaystyle \kappa ={\tfrac {1}{2}}{\bigl (}\langle u_{1}u_{1}\rangle +\langle u_{2}u_{2}\rangle +\langle u_{3}u_{3}\rangle {\bigr )}}
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of the fluid. A turbulent flow in a fluid is defined by the critical
Reynolds number, for a closed pipe this works out to approximately
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is an eddy which is an undulation that is a deviation from mean flow, but does not have the local closed streamlines of a vortex.
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toward the back of the obstacle. This phenomenon is naturally observed behind large emergent rocks in swift-flowing rivers.
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which produces such deviation. However, there are other types of eddies that are not simple vortices. For example, a
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1150:"Flow past a Cylinder on a Plane, with Application to Gulf Stream Separation and the Antarctic Circumpolar Current"
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An eddy is a movement of fluid that deviates from the general flow of the fluid. An example for an eddy is a
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606:{\displaystyle -\rho \langle u_{i}u_{j}\rangle =2\mu _{t}S_{i,j}-{\tfrac {2}{3}}\rho \kappa \delta _{i,j}}
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These are turbulence models in which the
Reynolds stresses, as obtained from a Reynolds averaging of the
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1202:"Effects of Disturbed Flow on Vascular Endothelium: Pathophysiological Basis and Clinical Perspectives"
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985:). These types of mesoscale eddies have been observed in many major ocean currents, including the
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When the ocean contains a sea surface height gradient this creates a jet or current, such as the
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Swirling of a fluid and the reverse current created when the fluid is in a turbulent flow regime
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Eddy/Wind interactions stimulate extraordinary mid-ocean plankton blooms. Science, 316(5827).
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1586:"Influence of a River Plume on Coastal Upwelling Dynamics: Importance of Stratification"
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used to thoroughly mix fluids and increase reaction rates within industrial processes.
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off the west
African coast, eddies create turbulent patterns called vortex streets.
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In terms of the critical Reynolds number, the critical velocity is represented as
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Roman, F.; Stipcich, G.; Armenio, V.; Inghilesi, R.; Corsini, S. (2010-06-01).
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325:{\displaystyle \mathrm {Re} ={\frac {2v\rho r}{\mu }}={\frac {\rho vd}{\mu }}}
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Reynolds Experiment (1883). Osborne Reynolds standing beside his apparatus.
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The general form for the Reynolds number flowing through a tube of radius
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1641:. Sixth International Symposium on Turbulence and Shear Flow Phenomena.
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is used to promote good fuel/air mixing in internal combustion engines.
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are dominant over the viscous forces. This phenomenon is described by
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Chen, Zhaoyun; Jiang, Yuwu; Wang, Jia; Gong, Wenping (2019-07-23).
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1365:"Linear eddy viscosity models -- CFD-Wiki, the free CFD reference"
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1561:"Ocean Mesoscale Eddies – Geophysical Fluid Dynamics Laboratory"
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Lightfoot, R. Byron Bird; Warren E. Stewart; Edwin N. (2002).
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California Institute of Technology Information Tech Services
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10.1175/1520-0485(2001)031<3274:FPACOA>2.0.CO;2
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10.1175/1520-0485(2001)031<3274:FPACOA>2.0.CO;2
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997:, and the Antarctic Circumpolar Current, amongst others.
873:{\displaystyle {\tfrac {2}{3}}\rho \kappa \delta _{i,j}}
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1315:. World Scientific Publishing Co. Pte. Ltd. pp.
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397:{\displaystyle \mathrm {Re} _{\text{c}}\approx 2000.}
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1511:Daily, Juliette; Hoffman, Matthew J. (2020-05-01).
60:. Unsourced material may be challenged and removed.
1635:"Large eddy simulation of mixing in coastal areas"
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2787:Deep-ocean Assessment and Reporting of Tsunamis
1680:Tansley, Claire E.; Marshall, David P. (2001).
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1498:National Oceanic and Atmospheric Administration
1148:Tansley, Claire E.; Marshall, David P. (2001).
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4164:List of atmospheric pressure records in Europe
1257:Encyclopedia Britannica eddy (fluid-mechanics)
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1292:: CS1 maint: multiple names: authors list (
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1272:(2. ed.). New York, NY : Wiley.
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3197:Tropical cyclones and climate change
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1781:https://doi.org/10.1002/2014JC010111
926:Fluid currents and pollution control
783:is the mean turbulent kinetic energy
58:adding citations to reliable sources
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4421:Mediterranean tropical-like cyclone
4414:North Indian Ocean tropical cyclone
4347:Mediterranean tropical-like cyclone
4230:East Asian-northwest Pacific storms
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4509:Upper tropospheric cyclonic vortex
4455:Australian region tropical cyclone
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2372:World Ocean Circulation Experiment
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1686:Journal of Physical Oceanography
1590:Journal of Physical Oceanography
1157:Journal of Physical Oceanography
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2703:Vine–Matthews–Morley hypothesis
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355:is the radius of the tube, and
184:Swirl and eddies in engineering
164:created when the fluid is in a
45:needs additional citations for
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4225:Continental North Asian storms
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215:Reynolds number and turbulence
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1:
1407:"Why are Golf Balls Dimpled?"
1345:hyperphysics.phy-astr.gsu.edu
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979:Antarctic Circumpolar Current
188:The propensity of a fluid to
4723:Tropical cyclones portal
3764:Great Sheffield Gale of 1962
3704:Moray Firth fishing disaster
3247:Ridiculously Resilient Ridge
2240:El Niño–Southern Oscillation
2210:Craik–Leibovich vortex force
1966:Luke's variational principle
1113:Computational fluid dynamics
1020:Influences on apex predators
829:Note that that inclusion of
484:Computational fluid dynamics
7:
4573:Mesoscale convective vortex
4555:Mesoscale convective system
4157:List of European windstorms
3574:Pacific Northwest windstorm
1390:"The Flight of a Golf Ball"
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144:in the range ~40 to ~1000.
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2305:Ocean dynamical thermostat
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1311:Elementary Fluid Mechanics
1218:10.1152/physrev.00047.2009
1103:River eddies in whitewater
69:"Eddy" fluid dynamics
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3633:
3593:
3586:
3546:
3517:
3478:
3471:
3462:
3453:
3395:
3357:
3325:
3314:
3305:
3260:
3214:
3205:
3139:
3050:
2889:
2863:
2840:Ocean acoustic tomography
2825:
2777:
2716:
2653:Mohorovičić discontinuity
2611:
2483:
2380:
2245:General circulation model
2175:
1881:Benjamin–Feir instability
1861:
1517:Marine Pollution Bulletin
3848:Boxing Day Storm of 1998
3841:Christmas Eve storm 1997
3177:Annular tropical cyclone
2970:Ocean surface topography
2345:Thermohaline circulation
2335:Subsurface ocean current
2275:Hydrothermal circulation
2108:Wave–current interaction
1886:Boussinesq approximation
1738:"Ocean Mesoscale Eddies"
641:{\displaystyle \mu _{t}}
479:Research and development
4637:Multiple-vortex tornado
4076:Friederike (David) 2018
4069:Eleanor (Burglind) 2018
3792:December 1981 windstorm
3750:North Sea flood of 1953
3663:Christmas Flood of 1717
3007:Sea surface temperature
2990:Outline of oceanography
2185:Atmospheric circulation
2123:shallow water equations
2113:Waves and shallow water
2006:Significant wave height
1611:10.1175/JPO-D-18-0215.1
1307:Kambe, Tsutomu (2007).
1130:, or dipole eddy pairs.
893:{\displaystyle \kappa }
811:{\displaystyle S_{i,j}}
490:Navier–Stokes equations
4578:Line echo wave pattern
4532:Mesoscale ocean eddies
4301:Southern Ocean cyclone
3389:Extratropical cyclones
3182:Bar (tropical cyclone)
3172:Central dense overcast
3002:Sea surface microlayer
2367:Wind generated current
964:
947:Mesoscale ocean eddies
894:
874:
812:
777:
642:
607:
469:
398:
326:
248:
224:
211:
145:
3950:Friedhelm/Bawbag 2011
3813:Burns' Day storm 1990
3697:Night of the Big Wind
3418:Post-tropical cyclone
3167:Rapid intensification
2835:Deep scattering layer
2817:World Geodetic System
2325:Princeton Ocean Model
2205:Coriolis–Stokes force
1855:Physical oceanography
1206:Physiological Reviews
954:
895:
875:
813:
778:
643:
608:
470:
399:
327:
242:
222:
209:
156:is the swirling of a
135:
4737:Tornadoes portal
4647:Anticyclonic tornado
4615:Low-topped supercell
4393:Cape Verde hurricane
3785:Gale of January 1976
2855:Underwater acoustics
2415:Perigean spring tide
2280:Langmuir circulation
1991:Rossby-gravity waves
1088:Kármán vortex street
917:Industrial processes
884:
833:
789:
654:
625:
499:
414:
370:
266:
244:Schlieren photograph
54:improve this article
4439:Southern Hemisphere
4377:Northern Hemisphere
4265:Southern Hemisphere
4220:Western Disturbance
4034:Thomas (Doris) 2017
3806:Great storm of 1987
3771:1968 Scotland storm
3711:Tay Bridge disaster
3690:Great Storm of 1824
3656:Great Storm of 1703
3626:European windstorms
3455:Northern Hemisphere
3273:South Atlantic High
3261:Southern Hemisphere
3237:North American High
3215:Northern Hemisphere
3017:Science On a Sphere
2623:Convergent boundary
2295:Modular Ocean Model
2255:Geostrophic current
1971:Mild-slope equation
1698:2001JPO....31.3274T
1602:2019JPO....49.2345C
1270:Transport phenomena
1169:2001JPO....31.3274T
1083:Reynolds experiment
938:Environmental flows
227:In 1883, scientist
201:transport phenomena
4386:Atlantic hurricane
4342:Lake Huron cyclone
3403:Anticyclonic storm
3278:South Pacific High
3242:North Pacific High
3157:High-pressure area
3147:Anticyclonic storm
2673:Seafloor spreading
2663:Outer trench swell
2628:Divergent boundary
2528:Continental margin
2513:Carbonate platform
2410:Lunitidal interval
1369:www.cfd-online.com
965:
890:
870:
846:
808:
773:
673:
638:
603:
579:
465:
394:
322:
249:
225:
212:
146:
4746:
4745:
4706:
4705:
4702:
4701:
4698:
4697:
4642:Satellite tornado
4517:
4516:
4482:
4481:
4478:
4477:
4402:Pacific hurricane
4318:
4317:
4314:
4313:
4259:
4258:
4203:
4202:
4173:
4172:
3718:Eyemouth disaster
3634:14th-18th century
3582:
3581:
3542:
3541:
3423:Low-pressure area
3301:
3300:
3293:Subtropical ridge
3252:Subtropical ridge
3162:Low-pressure area
3132:Centers of action
3090:
3089:
3082:Oceans portal
3042:World Ocean Atlas
3032:Underwater glider
2975:Ocean temperature
2638:Hydrothermal vent
2603:Submarine volcano
2538:Continental shelf
2518:Coastal geography
2508:Bathymetric chart
2390:Amphidromic point
2078:Wave nonlinearity
1936:Infragravity wave
1692:(11): 3274–3283.
1565:www.gfdl.noaa.gov
1494:"Ocean Pollution"
1430:Dimotakis, Paul.
1388:Arnold, Douglas.
1326:978-981-256-416-0
1163:(11): 3274–3283.
845:
672:
578:
460:
445:
424:
385:
361:dynamic viscosity
320:
299:
130:
129:
122:
104:
16:(Redirected from
4771:
4735:
4734:
4733:
4721:
4720:
4719:
4595:
4594:
4528:
4527:
4471:
4464:
4457:
4450:
4440:
4430:
4423:
4416:
4404:
4395:
4388:
4378:
4373:
4372:
4285:Black nor'easter
4270:
4269:
4266:
4185:Black Sea storms
4166:
4159:
4141:
4134:
4127:
4120:
4113:
4106:
4099:
4092:
4085:
4078:
4071:
4064:
4057:
4050:
4043:
4036:
4029:
4022:
4015:
4008:
4001:
3994:
3987:
3980:
3973:
3966:
3959:
3952:
3945:
3938:
3931:
3924:
3917:
3910:
3903:
3896:
3889:
3871:
3864:
3857:
3850:
3843:
3836:
3829:
3827:Braer Storm 1993
3822:
3815:
3808:
3801:
3794:
3787:
3780:
3773:
3766:
3759:
3752:
3745:
3738:
3720:
3713:
3706:
3699:
3692:
3676:
3665:
3658:
3651:
3644:
3628:
3618:
3611:
3604:
3595:
3594:
3591:
3590:
3535:
3528:
3510:
3503:
3496:
3489:
3476:
3475:
3469:
3468:
3465:
3460:
3459:
3456:
3382:
3375:
3368:
3359:
3358:
3332:
3331:
3328:
3323:
3322:
3319:
3312:
3311:
3268:South Polar High
3222:North Polar High
3212:
3211:
3117:
3110:
3103:
3094:
3093:
3080:
3079:
3068:
3067:
3058:
3057:
2997:Pelagic sediment
2935:Marine pollution
2729:Deep ocean water
2598:Submarine canyon
2533:Continental rise
2425:Rule of twelfths
2340:Sverdrup balance
2270:Humboldt Current
2195:Boundary current
2170:
2159:
1976:Radiation stress
1946:Iribarren number
1921:Equatorial waves
1876:Ballantine scale
1871:Airy wave theory
1848:
1841:
1834:
1825:
1824:
1818:
1811:
1805:
1798:
1783:
1776:
1770:
1764:
1758:
1757:
1755:
1754:
1734:
1728:
1727:
1709:
1677:
1671:
1670:
1630:
1624:
1623:
1613:
1596:(9): 2345–2363.
1581:
1575:
1574:
1572:
1571:
1557:
1551:
1550:
1532:
1508:
1502:
1501:
1490:
1484:
1483:
1481:
1480:
1463:
1457:
1456:
1454:
1453:
1447:
1441:. Archived from
1436:
1427:
1421:
1420:
1418:
1417:
1403:
1397:
1396:
1394:
1385:
1379:
1378:
1376:
1375:
1361:
1355:
1354:
1352:
1351:
1337:
1331:
1330:
1314:
1304:
1298:
1297:
1291:
1283:
1265:
1259:
1254:
1248:
1247:
1237:
1197:
1188:
1187:
1185:
1179:. Archived from
1154:
1145:
995:Kuroshio Current
899:
897:
896:
891:
879:
877:
876:
871:
869:
868:
847:
838:
817:
815:
814:
809:
807:
806:
782:
780:
779:
774:
772:
771:
762:
761:
752:
751:
733:
732:
723:
722:
704:
703:
694:
693:
681:
680:
674:
665:
647:
645:
644:
639:
637:
636:
612:
610:
609:
604:
602:
601:
580:
571:
565:
564:
549:
548:
530:
529:
520:
519:
474:
472:
471:
466:
461:
459:
451:
447:
446:
443:
441:
431:
426:
425:
422:
403:
401:
400:
395:
387:
386:
383:
381:
358:
354:
346:
338:
331:
329:
328:
323:
321:
316:
305:
300:
295:
281:
276:
258:
254:
229:Osborne Reynolds
160:and the reverse
125:
118:
114:
111:
105:
103:
62:
38:
30:
21:
18:Mesoscale eddies
4779:
4778:
4774:
4773:
4772:
4770:
4769:
4768:
4749:
4748:
4747:
4742:
4731:
4729:
4717:
4715:
4694:
4663:
4584:
4549:
4513:
4474:
4467:
4460:
4453:
4446:
4438:
4433:
4426:
4419:
4412:
4400:
4391:
4384:
4376:
4364:
4356:
4310:
4289:
4264:
4255:
4234:
4199:
4169:
4162:
4155:
4144:
4137:
4130:
4123:
4116:
4109:
4102:
4095:
4088:
4081:
4074:
4067:
4060:
4053:
4046:
4039:
4032:
4025:
4018:
4011:
4004:
3997:
3990:
3983:
3976:
3969:
3962:
3955:
3948:
3941:
3934:
3927:
3920:
3913:
3906:
3899:
3892:
3885:
3874:
3867:
3860:
3853:
3846:
3839:
3832:
3825:
3818:
3811:
3804:
3797:
3790:
3783:
3776:
3769:
3762:
3755:
3748:
3741:
3734:
3723:
3716:
3709:
3702:
3695:
3688:
3677:
3668:
3661:
3654:
3649:Burchardi flood
3647:
3642:Grote Mandrenke
3640:
3629:
3624:
3622:
3578:
3538:
3531:
3524:
3513:
3506:
3501:Great basin low
3499:
3492:
3487:Alberta clipper
3485:
3463:
3454:
3449:
3391:
3386:
3353:
3349:South Polar low
3344:North Polar low
3326:
3315:
3297:
3288:Australian High
3256:
3201:
3135:
3121:
3091:
3086:
3074:
3046:
2885:
2859:
2821:
2802:Sea-level curve
2773:
2712:
2698:Transform fault
2648:Mid-ocean ridge
2614:
2607:
2573:Oceanic plateau
2479:
2465:Tidal resonance
2435:Theory of tides
2376:
2285:Longshore drift
2235:Ekman transport
2171:
2165:
2164:
2163:
2162:
2161:
2160:
2151:
2103:Wave turbulence
2036:Trochoidal wave
1961:Longshore drift
1857:
1852:
1822:
1821:
1812:
1808:
1799:
1786:
1777:
1773:
1765:
1761:
1752:
1750:
1736:
1735:
1731:
1678:
1674:
1631:
1627:
1582:
1578:
1569:
1567:
1559:
1558:
1554:
1509:
1505:
1492:
1491:
1487:
1478:
1476:
1475:. 16 April 2016
1465:
1464:
1460:
1451:
1449:
1445:
1434:
1428:
1424:
1415:
1413:
1405:
1404:
1400:
1392:
1386:
1382:
1373:
1371:
1363:
1362:
1358:
1349:
1347:
1339:
1338:
1334:
1327:
1305:
1301:
1285:
1284:
1280:
1266:
1262:
1255:
1251:
1198:
1191:
1183:
1152:
1146:
1142:
1137:
1108:Wake turbulence
1077:Reynolds number
1047:
1022:
991:Agulhas Current
949:
940:
928:
919:
907:
885:
882:
881:
858:
854:
836:
834:
831:
830:
796:
792:
790:
787:
786:
767:
766:
757:
753:
747:
743:
728:
724:
718:
714:
699:
695:
689:
685:
676:
675:
663:
655:
652:
651:
632:
628:
626:
623:
622:
591:
587:
569:
554:
550:
544:
540:
525:
521:
515:
511:
500:
497:
496:
486:
481:
452:
442:
434:
433:
432:
430:
421:
417:
415:
412:
411:
382:
374:
373:
371:
368:
367:
356:
352:
344:
336:
306:
304:
282:
280:
269:
267:
264:
263:
256:
252:
234:Reynolds number
217:
197:fluid mechanics
186:
142:Reynolds number
126:
115:
109:
106:
63:
61:
51:
39:
28:
23:
22:
15:
12:
11:
5:
4777:
4767:
4766:
4761:
4759:Fluid dynamics
4744:
4743:
4741:
4740:
4726:
4711:
4708:
4707:
4704:
4703:
4700:
4699:
4696:
4695:
4693:
4692:
4687:
4682:
4677:
4671:
4669:
4665:
4664:
4662:
4661:
4656:
4651:
4650:
4649:
4644:
4639:
4629:
4624:
4623:
4622:
4617:
4612:
4601:
4599:
4592:
4586:
4585:
4583:
4582:
4581:
4580:
4570:
4565:
4559:
4557:
4551:
4550:
4548:
4547:
4542:
4536:
4534:
4525:
4519:
4518:
4515:
4514:
4512:
4511:
4506:
4501:
4496:
4490:
4488:
4484:
4483:
4480:
4479:
4476:
4475:
4473:
4472:
4465:
4458:
4451:
4443:
4441:
4435:
4434:
4432:
4431:
4424:
4417:
4410:
4405:
4398:
4397:
4396:
4381:
4379:
4370:
4358:
4357:
4355:
4354:
4349:
4344:
4339:
4334:
4328:
4326:
4320:
4319:
4316:
4315:
4312:
4311:
4309:
4308:
4303:
4297:
4295:
4291:
4290:
4288:
4287:
4282:
4276:
4274:
4267:
4261:
4260:
4257:
4256:
4254:
4253:
4248:
4242:
4240:
4236:
4235:
4233:
4232:
4227:
4222:
4217:
4211:
4209:
4205:
4204:
4201:
4200:
4198:
4197:
4192:
4187:
4181:
4179:
4175:
4174:
4171:
4170:
4168:
4167:
4160:
4152:
4150:
4146:
4145:
4143:
4142:
4135:
4128:
4121:
4114:
4107:
4100:
4093:
4086:
4079:
4072:
4065:
4058:
4051:
4044:
4037:
4030:
4023:
4016:
4009:
4006:Christina 2014
4002:
3995:
3988:
3981:
3974:
3967:
3960:
3953:
3946:
3939:
3932:
3925:
3918:
3911:
3904:
3897:
3890:
3882:
3880:
3876:
3875:
3873:
3872:
3865:
3858:
3851:
3844:
3837:
3830:
3823:
3816:
3809:
3802:
3795:
3788:
3781:
3778:Quimburga 1972
3774:
3767:
3760:
3753:
3746:
3739:
3731:
3729:
3725:
3724:
3722:
3721:
3714:
3707:
3700:
3693:
3685:
3683:
3679:
3678:
3671:
3669:
3667:
3666:
3659:
3652:
3645:
3637:
3635:
3631:
3630:
3621:
3620:
3613:
3606:
3598:
3588:
3584:
3583:
3580:
3579:
3577:
3576:
3571:
3566:
3561:
3556:
3550:
3548:
3544:
3543:
3540:
3539:
3537:
3536:
3529:
3526:Panhandle hook
3521:
3519:
3515:
3514:
3512:
3511:
3504:
3497:
3490:
3482:
3480:
3473:
3466:
3457:
3451:
3450:
3448:
3447:
3442:
3441:
3440:
3430:
3425:
3420:
3415:
3410:
3405:
3399:
3397:
3393:
3392:
3385:
3384:
3377:
3370:
3362:
3355:
3354:
3352:
3351:
3346:
3340:
3338:
3329:
3320:
3317:Synoptic scale
3309:
3303:
3302:
3299:
3298:
3296:
3295:
3290:
3285:
3280:
3275:
3270:
3264:
3262:
3258:
3257:
3255:
3254:
3249:
3244:
3239:
3234:
3229:
3224:
3218:
3216:
3209:
3203:
3202:
3200:
3199:
3194:
3189:
3184:
3179:
3174:
3169:
3164:
3159:
3154:
3149:
3143:
3141:
3137:
3136:
3130:of the world (
3120:
3119:
3112:
3105:
3097:
3088:
3087:
3085:
3084:
3072:
3062:
3051:
3048:
3047:
3045:
3044:
3039:
3034:
3029:
3024:
3022:Stratification
3019:
3014:
3009:
3004:
2999:
2994:
2993:
2992:
2982:
2977:
2972:
2967:
2962:
2957:
2952:
2947:
2942:
2937:
2932:
2927:
2922:
2914:
2912:Color of water
2909:
2907:Benthic lander
2904:
2899:
2893:
2891:
2887:
2886:
2884:
2883:
2878:
2873:
2867:
2865:
2861:
2860:
2858:
2857:
2852:
2847:
2842:
2837:
2831:
2829:
2823:
2822:
2820:
2819:
2814:
2812:Sea level rise
2809:
2807:Sea level drop
2804:
2799:
2794:
2789:
2783:
2781:
2775:
2774:
2772:
2771:
2766:
2761:
2756:
2751:
2746:
2741:
2736:
2731:
2726:
2720:
2718:
2714:
2713:
2711:
2710:
2705:
2700:
2695:
2690:
2685:
2680:
2675:
2670:
2665:
2660:
2655:
2650:
2645:
2643:Marine geology
2640:
2635:
2630:
2625:
2619:
2617:
2609:
2608:
2606:
2605:
2600:
2595:
2590:
2585:
2583:Passive margin
2580:
2578:Oceanic trench
2575:
2570:
2565:
2560:
2555:
2550:
2545:
2540:
2535:
2530:
2525:
2520:
2515:
2510:
2505:
2500:
2495:
2489:
2487:
2481:
2480:
2478:
2477:
2472:
2467:
2462:
2457:
2452:
2447:
2442:
2437:
2432:
2427:
2422:
2417:
2412:
2407:
2402:
2397:
2392:
2386:
2384:
2378:
2377:
2375:
2374:
2369:
2364:
2359:
2354:
2353:
2352:
2342:
2337:
2332:
2327:
2322:
2317:
2312:
2310:Ocean dynamics
2307:
2302:
2297:
2292:
2287:
2282:
2277:
2272:
2267:
2262:
2257:
2252:
2247:
2242:
2237:
2232:
2227:
2222:
2217:
2212:
2207:
2202:
2200:Coriolis force
2197:
2192:
2187:
2181:
2179:
2173:
2172:
2154:
2152:
2150:
2149:
2148:
2147:
2137:
2132:
2127:
2126:
2125:
2120:
2110:
2105:
2100:
2095:
2090:
2085:
2080:
2075:
2070:
2065:
2060:
2055:
2050:
2049:
2048:
2038:
2033:
2028:
2023:
2021:Stokes problem
2018:
2013:
2008:
2003:
1998:
1993:
1988:
1983:
1978:
1973:
1968:
1963:
1958:
1956:Kinematic wave
1953:
1948:
1943:
1938:
1933:
1928:
1923:
1918:
1913:
1908:
1903:
1898:
1893:
1888:
1883:
1878:
1873:
1867:
1865:
1859:
1858:
1851:
1850:
1843:
1836:
1828:
1820:
1819:
1806:
1784:
1771:
1759:
1729:
1672:
1645:(3): 327–341.
1625:
1576:
1552:
1503:
1485:
1458:
1422:
1398:
1380:
1356:
1332:
1325:
1299:
1278:
1260:
1249:
1212:(1): 327–387.
1189:
1186:on 2011-04-01.
1139:
1138:
1136:
1133:
1132:
1131:
1125:
1120:
1115:
1110:
1105:
1100:
1095:
1090:
1085:
1080:
1074:
1072:Irminger Rings
1069:
1064:
1062:Eddy diffusion
1059:
1053:
1046:
1043:
1027:apex predators
1021:
1018:
961:Canary Islands
948:
945:
939:
936:
927:
924:
918:
915:
906:
903:
902:
901:
889:
867:
864:
861:
857:
853:
850:
844:
841:
826:
825:
824:
823:
805:
802:
799:
795:
784:
770:
765:
760:
756:
750:
746:
742:
739:
736:
731:
727:
721:
717:
713:
710:
707:
702:
698:
692:
688:
684:
679:
671:
668:
662:
659:
649:
635:
631:
614:
613:
600:
597:
594:
590:
586:
583:
577:
574:
568:
563:
560:
557:
553:
547:
543:
539:
536:
533:
528:
524:
518:
514:
510:
507:
504:
485:
482:
480:
477:
476:
475:
464:
458:
455:
450:
440:
437:
429:
420:
405:
404:
393:
390:
380:
377:
343:of the fluid,
333:
332:
319:
315:
312:
309:
303:
298:
294:
291:
288:
285:
279:
275:
272:
216:
213:
185:
182:
150:fluid dynamics
128:
127:
42:
40:
33:
26:
9:
6:
4:
3:
2:
4776:
4765:
4762:
4760:
4757:
4756:
4754:
4739:
4738:
4727:
4725:
4724:
4713:
4712:
4709:
4691:
4688:
4686:
4683:
4681:
4678:
4676:
4673:
4672:
4670:
4666:
4660:
4657:
4655:
4652:
4648:
4645:
4643:
4640:
4638:
4635:
4634:
4633:
4630:
4628:
4625:
4621:
4618:
4616:
4613:
4611:
4608:
4607:
4606:
4603:
4602:
4600:
4596:
4593:
4591:
4587:
4579:
4576:
4575:
4574:
4571:
4569:
4566:
4564:
4561:
4560:
4558:
4556:
4552:
4546:
4543:
4541:
4540:Catalina eddy
4538:
4537:
4535:
4533:
4529:
4526:
4524:
4520:
4510:
4507:
4505:
4502:
4500:
4497:
4495:
4494:Cold-core low
4492:
4491:
4489:
4485:
4470:
4466:
4463:
4459:
4456:
4452:
4449:
4445:
4444:
4442:
4436:
4429:
4425:
4422:
4418:
4415:
4411:
4409:
4406:
4403:
4399:
4394:
4390:
4389:
4387:
4383:
4382:
4380:
4374:
4371:
4368:
4363:
4359:
4353:
4350:
4348:
4345:
4343:
4340:
4338:
4335:
4333:
4330:
4329:
4327:
4325:
4321:
4307:
4304:
4302:
4299:
4298:
4296:
4292:
4286:
4283:
4281:
4278:
4277:
4275:
4271:
4268:
4262:
4252:
4249:
4247:
4244:
4243:
4241:
4237:
4231:
4228:
4226:
4223:
4221:
4218:
4216:
4213:
4212:
4210:
4206:
4196:
4193:
4191:
4190:Icelandic Low
4188:
4186:
4183:
4182:
4180:
4176:
4165:
4161:
4158:
4154:
4153:
4151:
4147:
4140:
4136:
4133:
4129:
4126:
4122:
4119:
4115:
4112:
4108:
4105:
4101:
4098:
4094:
4091:
4087:
4084:
4080:
4077:
4073:
4070:
4066:
4063:
4059:
4056:
4052:
4049:
4045:
4042:
4038:
4035:
4031:
4028:
4024:
4021:
4017:
4014:
4010:
4007:
4003:
4000:
3996:
3993:
3989:
3986:
3982:
3979:
3975:
3972:
3968:
3965:
3961:
3958:
3954:
3951:
3947:
3944:
3940:
3937:
3933:
3930:
3926:
3923:
3919:
3916:
3912:
3909:
3905:
3902:
3898:
3895:
3891:
3888:
3884:
3883:
3881:
3877:
3870:
3866:
3863:
3859:
3856:
3852:
3849:
3845:
3842:
3838:
3835:
3831:
3828:
3824:
3821:
3817:
3814:
3810:
3807:
3803:
3800:
3796:
3793:
3789:
3786:
3782:
3779:
3775:
3772:
3768:
3765:
3761:
3758:
3754:
3751:
3747:
3744:
3740:
3737:
3733:
3732:
3730:
3726:
3719:
3715:
3712:
3708:
3705:
3701:
3698:
3694:
3691:
3687:
3686:
3684:
3680:
3675:
3664:
3660:
3657:
3653:
3650:
3646:
3643:
3639:
3638:
3636:
3632:
3627:
3619:
3614:
3612:
3607:
3605:
3600:
3599:
3596:
3592:
3589:
3585:
3575:
3572:
3570:
3567:
3565:
3562:
3560:
3557:
3555:
3552:
3551:
3549:
3545:
3534:
3533:November gale
3530:
3527:
3523:
3522:
3520:
3516:
3509:
3505:
3502:
3498:
3495:
3491:
3488:
3484:
3483:
3481:
3477:
3474:
3470:
3467:
3464:North America
3461:
3458:
3452:
3446:
3443:
3439:
3436:
3435:
3434:
3431:
3429:
3426:
3424:
3421:
3419:
3416:
3414:
3411:
3409:
3406:
3404:
3401:
3400:
3398:
3394:
3390:
3383:
3378:
3376:
3371:
3369:
3364:
3363:
3360:
3356:
3350:
3347:
3345:
3342:
3341:
3339:
3337:
3333:
3330:
3327:Surface-based
3324:
3321:
3318:
3313:
3310:
3308:
3304:
3294:
3291:
3289:
3286:
3284:
3283:Kalahari High
3281:
3279:
3276:
3274:
3271:
3269:
3266:
3265:
3263:
3259:
3253:
3250:
3248:
3245:
3243:
3240:
3238:
3235:
3233:
3230:
3228:
3227:Siberian High
3225:
3223:
3220:
3219:
3217:
3213:
3210:
3208:
3204:
3198:
3195:
3193:
3190:
3188:
3185:
3183:
3180:
3178:
3175:
3173:
3170:
3168:
3165:
3163:
3160:
3158:
3155:
3153:
3150:
3148:
3145:
3144:
3142:
3138:
3133:
3129:
3125:
3118:
3113:
3111:
3106:
3104:
3099:
3098:
3095:
3083:
3078:
3073:
3071:
3063:
3061:
3053:
3052:
3049:
3043:
3040:
3038:
3035:
3033:
3030:
3028:
3025:
3023:
3020:
3018:
3015:
3013:
3010:
3008:
3005:
3003:
3000:
2998:
2995:
2991:
2988:
2987:
2986:
2983:
2981:
2978:
2976:
2973:
2971:
2968:
2966:
2963:
2961:
2958:
2956:
2953:
2951:
2948:
2946:
2943:
2941:
2938:
2936:
2933:
2931:
2930:Marine energy
2928:
2926:
2923:
2921:
2920:
2915:
2913:
2910:
2908:
2905:
2903:
2900:
2898:
2897:Acidification
2895:
2894:
2892:
2888:
2882:
2879:
2877:
2874:
2872:
2869:
2868:
2866:
2862:
2856:
2853:
2851:
2850:SOFAR channel
2848:
2846:
2843:
2841:
2838:
2836:
2833:
2832:
2830:
2828:
2824:
2818:
2815:
2813:
2810:
2808:
2805:
2803:
2800:
2798:
2795:
2793:
2790:
2788:
2785:
2784:
2782:
2780:
2776:
2770:
2767:
2765:
2762:
2760:
2757:
2755:
2752:
2750:
2747:
2745:
2742:
2740:
2737:
2735:
2732:
2730:
2727:
2725:
2722:
2721:
2719:
2715:
2709:
2706:
2704:
2701:
2699:
2696:
2694:
2691:
2689:
2686:
2684:
2681:
2679:
2676:
2674:
2671:
2669:
2666:
2664:
2661:
2659:
2658:Oceanic crust
2656:
2654:
2651:
2649:
2646:
2644:
2641:
2639:
2636:
2634:
2633:Fracture zone
2631:
2629:
2626:
2624:
2621:
2620:
2618:
2616:
2610:
2604:
2601:
2599:
2596:
2594:
2591:
2589:
2586:
2584:
2581:
2579:
2576:
2574:
2571:
2569:
2568:Oceanic basin
2566:
2564:
2561:
2559:
2556:
2554:
2551:
2549:
2546:
2544:
2541:
2539:
2536:
2534:
2531:
2529:
2526:
2524:
2521:
2519:
2516:
2514:
2511:
2509:
2506:
2504:
2501:
2499:
2498:Abyssal plain
2496:
2494:
2491:
2490:
2488:
2486:
2482:
2476:
2473:
2471:
2468:
2466:
2463:
2461:
2458:
2456:
2453:
2451:
2448:
2446:
2443:
2441:
2438:
2436:
2433:
2431:
2428:
2426:
2423:
2421:
2418:
2416:
2413:
2411:
2408:
2406:
2405:Internal tide
2403:
2401:
2398:
2396:
2393:
2391:
2388:
2387:
2385:
2383:
2379:
2373:
2370:
2368:
2365:
2363:
2360:
2358:
2355:
2351:
2348:
2347:
2346:
2343:
2341:
2338:
2336:
2333:
2331:
2328:
2326:
2323:
2321:
2318:
2316:
2313:
2311:
2308:
2306:
2303:
2301:
2300:Ocean current
2298:
2296:
2293:
2291:
2288:
2286:
2283:
2281:
2278:
2276:
2273:
2271:
2268:
2266:
2263:
2261:
2258:
2256:
2253:
2251:
2248:
2246:
2243:
2241:
2238:
2236:
2233:
2231:
2228:
2226:
2223:
2221:
2218:
2216:
2213:
2211:
2208:
2206:
2203:
2201:
2198:
2196:
2193:
2191:
2188:
2186:
2183:
2182:
2180:
2178:
2174:
2169:
2158:
2146:
2143:
2142:
2141:
2138:
2136:
2133:
2131:
2128:
2124:
2121:
2119:
2116:
2115:
2114:
2111:
2109:
2106:
2104:
2101:
2099:
2098:Wave shoaling
2096:
2094:
2091:
2089:
2086:
2084:
2081:
2079:
2076:
2074:
2071:
2069:
2066:
2064:
2061:
2059:
2058:Ursell number
2056:
2054:
2051:
2047:
2044:
2043:
2042:
2039:
2037:
2034:
2032:
2029:
2027:
2024:
2022:
2019:
2017:
2014:
2012:
2009:
2007:
2004:
2002:
1999:
1997:
1994:
1992:
1989:
1987:
1984:
1982:
1979:
1977:
1974:
1972:
1969:
1967:
1964:
1962:
1959:
1957:
1954:
1952:
1949:
1947:
1944:
1942:
1941:Internal wave
1939:
1937:
1934:
1932:
1929:
1927:
1924:
1922:
1919:
1917:
1914:
1912:
1909:
1907:
1904:
1902:
1899:
1897:
1894:
1892:
1891:Breaking wave
1889:
1887:
1884:
1882:
1879:
1877:
1874:
1872:
1869:
1868:
1866:
1864:
1860:
1856:
1849:
1844:
1842:
1837:
1835:
1830:
1829:
1826:
1817:
1810:
1804:
1797:
1795:
1793:
1791:
1789:
1782:
1775:
1769:
1763:
1749:
1745:
1744:
1739:
1733:
1725:
1721:
1717:
1713:
1708:
1703:
1699:
1695:
1691:
1687:
1683:
1676:
1668:
1664:
1660:
1656:
1652:
1648:
1644:
1640:
1636:
1629:
1621:
1617:
1612:
1607:
1603:
1599:
1595:
1591:
1587:
1580:
1566:
1562:
1556:
1548:
1544:
1540:
1536:
1531:
1526:
1522:
1518:
1514:
1507:
1499:
1495:
1489:
1474:
1473:
1472:Science Daily
1468:
1462:
1448:on 2017-08-08
1444:
1440:
1433:
1426:
1412:
1408:
1402:
1391:
1384:
1370:
1366:
1360:
1346:
1342:
1336:
1328:
1322:
1318:
1313:
1312:
1303:
1295:
1289:
1281:
1279:0-471-41077-2
1275:
1271:
1264:
1258:
1253:
1245:
1241:
1236:
1231:
1227:
1223:
1219:
1215:
1211:
1207:
1203:
1196:
1194:
1182:
1178:
1174:
1170:
1166:
1162:
1158:
1151:
1144:
1140:
1129:
1126:
1124:
1121:
1119:
1116:
1114:
1111:
1109:
1106:
1104:
1101:
1099:
1096:
1094:
1091:
1089:
1086:
1084:
1081:
1078:
1075:
1073:
1070:
1068:
1065:
1063:
1060:
1057:
1054:
1052:
1049:
1048:
1042:
1038:
1034:
1030:
1028:
1017:
1013:
1011:
1007:
1003:
998:
996:
992:
988:
984:
980:
975:
972:
969:
962:
958:
953:
944:
935:
933:
932:phytoplankton
923:
914:
911:
887:
865:
862:
859:
855:
851:
848:
842:
839:
828:
827:
821:
818: is the
803:
800:
797:
793:
785:
758:
754:
748:
744:
737:
729:
725:
719:
715:
708:
700:
696:
690:
686:
669:
666:
660:
657:
650:
633:
629:
621:
620:
619:
618:
617:
598:
595:
592:
588:
584:
581:
575:
572:
566:
561:
558:
555:
551:
545:
541:
537:
534:
526:
522:
516:
512:
505:
502:
495:
494:
493:
491:
462:
456:
453:
448:
427:
418:
410:
409:
408:
391:
388:
366:
365:
364:
362:
350:
342:
317:
313:
310:
307:
301:
296:
292:
289:
286:
283:
277:
262:
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138:vortex street
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71: –
70:
66:
65:Find sources:
59:
55:
49:
48:
43:This article
41:
37:
32:
31:
19:
4728:
4714:
4627:Funnel cloud
4545:Haida Eddies
4504:Polar vortex
4062:Herwart 2017
4055:Ophelia 2017
3978:St Jude 2013
3957:Joachim 2011
3936:Xynthia 2010
3894:Jeanett 2002
3879:21st century
3799:Charley 1986
3736:Ulysses 1903
3728:20th century
3682:19th century
3559:Hatteras low
3554:Aleutian Low
3494:Colorado low
3428:Weather bomb
3128:anticyclones
3037:Water column
2985:Oceanography
2960:Observations
2955:Explorations
2925:Marginal sea
2918:
2876:OSTM/Jason-2
2708:Volcanic arc
2683:Slab suction
2400:Head of tide
2290:Loop Current
2230:Ekman spiral
2219:
2016:Stokes drift
1926:Gravity wave
1901:Cnoidal wave
1809:
1774:
1762:
1751:. Retrieved
1741:
1732:
1689:
1685:
1675:
1642:
1638:
1628:
1593:
1589:
1579:
1568:. Retrieved
1564:
1555:
1520:
1516:
1506:
1497:
1488:
1477:. Retrieved
1470:
1461:
1450:. Retrieved
1443:the original
1438:
1425:
1414:. Retrieved
1411:math.ucr.edu
1410:
1401:
1383:
1372:. Retrieved
1368:
1359:
1348:. Retrieved
1344:
1335:
1310:
1302:
1269:
1263:
1252:
1209:
1205:
1181:the original
1160:
1156:
1143:
1123:Hemodynamics
1118:Laminar flow
1067:Haida Eddies
1056:Eddy pumping
1039:
1035:
1031:
1023:
1014:
1010:Haida Eddies
1006:anticyclonic
999:
976:
973:
970:
966:
941:
929:
920:
910:Hemodynamics
908:
905:Hemodynamics
819:
615:
487:
406:
334:
250:
226:
194:
187:
171:
153:
147:
116:
107:
97:
90:
83:
76:
64:
52:Please help
47:verification
44:
4685:Steam devil
4605:Mesocyclone
4499:Cut-off low
4487:Upper level
4324:Subtropical
4294:Other areas
4239:Other areas
4215:Asiatic Low
4139:Ciarán 2023
4125:Larisa 2023
4118:Eunice 2022
4104:Aurore 2021
4097:Dennis 2020
4083:Adrian 2018
4048:Xavier 2017
4020:Niklas 2015
3971:Andrea 2012
3964:Dagmar 2011
3915:Kyrill 2007
3901:Gudrun 2005
3887:Oratia 2000
3869:Martin 1999
3862:Lothar 1999
3855:Anatol 1999
3757:Debbie 1961
3743:Iberia 1941
3508:Bighorn Low
3479:Lee Cyclone
3472:Continental
3232:Azores High
3207:Anticyclone
3027:Thermocline
2744:Mesopelagic
2717:Ocean zones
2688:Slab window
2553:Hydrography
2493:Abyssal fan
2460:Tidal range
2450:Tidal power
2445:Tidal force
2330:Rip current
2265:Gulf Stream
2225:Ekman layer
2215:Downwelling
2190:Baroclinity
2177:Circulation
2073:Wave height
2063:Wave action
2046:megatsunami
2026:Stokes wave
1986:Rossby wave
1951:Kelvin wave
1931:Green's law
987:Gulf Stream
822:strain rate
178:Rossby wave
4753:Categories
4690:Fire whirl
4680:Dust devil
4659:Waterspout
4620:Wall cloud
4332:Kona storm
4251:Kona storm
4132:Babet 2023
4111:Malik 2022
4090:Ciara 2020
3985:Xaver 2013
3943:Berit 2011
3929:Klaus 2009
3564:Nor'easter
3187:Superstorm
2965:Reanalysis
2864:Satellites
2845:Sofar bomb
2693:Subduction
2668:Ridge push
2563:Ocean bank
2543:Contourite
2470:Tide gauge
2455:Tidal race
2440:Tidal bore
2430:Slack tide
2395:Earth tide
2315:Ocean gyre
2135:Wind setup
2130:Wind fetch
2093:Wave setup
2088:Wave radar
2083:Wave power
1981:Rogue wave
1911:Dispersion
1753:2021-06-10
1570:2017-02-12
1523:: 111024.
1479:2017-02-12
1452:2017-03-06
1416:2017-02-12
1374:2017-02-12
1350:2017-02-12
1341:"Pressure"
1135:References
983:oxbow lake
80:newspapers
4654:Landspout
4610:Supercell
4590:Whirlwind
4523:Mesoscale
4306:Sudestada
4273:Australia
4195:Genoa low
4041:Zeus 2017
4027:Egon 2017
4013:Tini 2014
3999:Anne 2014
3992:Dirk 2013
3922:Emma 2008
3834:Lili 1996
3433:Sting jet
3192:Hypercane
2827:Acoustics
2779:Sea level
2678:Slab pull
2615:tectonics
2523:Cold seep
2485:Landforms
2362:Whirlpool
2357:Upwelling
2140:Wind wave
2068:Wave base
1996:Sea state
1916:Edge wave
1906:Cross sea
1724:130455873
1716:1520-0485
1667:123151803
1659:0142-727X
1620:0022-3670
1539:0025-326X
1288:cite book
1226:0031-9333
1098:Whirlwind
1093:Whirlpool
1008:(such as
888:κ
856:δ
852:κ
849:ρ
764:⟩
741:⟨
735:⟩
712:⟨
706:⟩
683:⟨
658:κ
630:μ
589:δ
585:κ
582:ρ
567:−
542:μ
532:⟩
509:⟨
506:ρ
503:−
454:ρ
449:μ
389:≈
318:μ
308:ρ
297:μ
290:ρ
166:turbulent
110:July 2013
4764:Vortices
4675:Gustnado
4568:Mesohigh
4563:Wake Low
4362:Tropical
4149:See also
3908:Per 2007
3569:Gulf low
3445:Rainband
3396:Concepts
3140:Concepts
3124:Cyclones
3060:Category
3012:Seawater
2739:Littoral
2734:Deep sea
2593:Seamount
2475:Tideline
2420:Rip tide
2350:shutdown
2320:Overflow
2053:Undertow
1896:Clapotis
1547:32319887
1244:21248169
1045:See also
1002:cyclonic
959:and the
341:velocity
4632:Tornado
4408:Typhoon
4367:Outline
4352:Thermal
3547:Oceanic
3413:Cyclone
3307:Cyclone
3070:Commons
2940:Mooring
2890:Related
2881:Jason-3
2871:Jason-1
2754:Pelagic
2749:Oceanic
2724:Benthic
2041:Tsunami
2011:Soliton
1694:Bibcode
1598:Bibcode
1235:3844671
1165:Bibcode
957:Madeira
359:is the
349:density
347:is its
339:is the
247:mirror.
162:current
94:scholar
4246:Arctic
3587:Europe
2759:Photic
2588:Seabed
2001:Seiche
1722:
1714:
1665:
1657:
1618:
1545:
1537:
1323:
1276:
1242:
1232:
1224:
1128:Modons
1051:Vortex
993:, the
989:, the
616:where
335:where
174:vortex
96:
89:
82:
75:
67:
4668:Minor
4598:Major
4178:Other
3518:Other
3408:Storm
3336:Polar
3152:Storm
2950:Ocean
2919:Alvin
2769:Swash
2613:Plate
2558:Knoll
2548:Guyot
2503:Atoll
2382:Tides
2145:model
2031:Swell
1863:Waves
1720:S2CID
1663:S2CID
1446:(PDF)
1435:(PDF)
1393:(PDF)
1184:(PDF)
1153:(PDF)
392:2000.
190:swirl
158:fluid
152:, an
101:JSTOR
87:books
4208:Asia
3438:List
3126:and
2917:DSV
2902:Argo
2764:Surf
2220:Eddy
1748:NOAA
1712:ISSN
1655:ISSN
1616:ISSN
1543:PMID
1535:ISSN
1321:ISBN
1294:link
1274:ISBN
1240:PMID
1222:ISSN
820:mean
199:and
154:eddy
73:news
1702:doi
1647:doi
1606:doi
1525:doi
1521:154
1317:240
1230:PMC
1214:doi
1173:doi
1004:or
259:):
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148:In
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436:R
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357:μ
353:r
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