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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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1001:). Oceanic eddies are also usually made of water masses that are different from those outside the eddy. That is, the water within an eddy usually has different temperature and salinity characteristics to the water outside the eddy. There is a direct link between the water mass properties of an eddy and its rotation. Warm eddies rotate anti-cyclonically, while cold eddies rotate cyclonically.
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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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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
765:{\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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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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595:{\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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1191:"Effects of Disturbed Flow on Vascular Endothelium: Pathophysiological Basis and Clinical Perspectives"
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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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1575:"Influence of a River Plume on Coastal Upwelling Dynamics: Importance of Stratification"
1456:"Ocean currents push phytoplankton, and pollution, around the globe faster than thought"
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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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314:{\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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is used to promote good fuel/air mixing in internal combustion engines.
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1068:- a dimensionless constant used to predict the onset of turbulent flow
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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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1354:"Linear eddy viscosity models -- CFD-Wiki, the free CFD reference"
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1550:"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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986:, and the Antarctic Circumpolar Current, amongst others.
862:{\displaystyle {\tfrac {2}{3}}\rho \kappa \delta _{i,j}}
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1304:. World Scientific Publishing Co. Pte. Ltd. pp.
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386:{\displaystyle \mathrm {Re} _{\text{c}}\approx 2000.}
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1500:Daily, Juliette; Hoffman, Matthew J. (2020-05-01).
49:. Unsourced material may be challenged and removed.
1624:"Large eddy simulation of mixing in coastal areas"
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2786:North West Shelf Operational Oceanographic System
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2776:Deep-ocean Assessment and Reporting of Tsunamis
1669:Tansley, Claire E.; Marshall, David P. (2001).
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1487:National Oceanic and Atmospheric Administration
1137:Tansley, Claire E.; Marshall, David P. (2001).
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4153:List of atmospheric pressure records in Europe
1246:Encyclopedia Britannica eddy (fluid-mechanics)
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1281:: CS1 maint: multiple names: authors list (
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1421:"The Mixing Transition in Turbulent Flows"
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109:Learn how and when to remove this message
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1805:https://doi.org/10.1126/science.1136256
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1261:(2. ed.). New York, NY : Wiley.
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3186:Tropical cyclones and climate change
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1770:https://doi.org/10.1002/2014JC010111
915:Fluid currents and pollution control
772:is the mean turbulent kinetic energy
47:adding citations to reliable sources
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4410:Mediterranean tropical-like cyclone
4403:North Indian Ocean tropical cyclone
4336:Mediterranean tropical-like cyclone
4219:East Asian-northwest Pacific storms
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4444:Australian region tropical cyclone
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1146:Journal of Physical Oceanography
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344:is the radius of the tube, and
173:Swirl and eddies in engineering
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34:needs additional citations for
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4214:Continental North Asian storms
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204:Reynolds number and turbulence
1:
1396:"Why are Golf Balls Dimpled?"
1334:hyperphysics.phy-astr.gsu.edu
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968:Antarctic Circumpolar Current
177:The propensity of a fluid to
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3753:Great Sheffield Gale of 1962
3693:Moray Firth fishing disaster
3236:Ridiculously Resilient Ridge
2229:El Niño–Southern Oscillation
2199:Craik–Leibovich vortex force
1955:Luke's variational principle
1102:Computational fluid dynamics
1009:Influences on apex predators
818:Note that that inclusion of
473:Computational fluid dynamics
7:
4562:Mesoscale convective vortex
4544:Mesoscale convective system
4146:List of European windstorms
3563:Pacific Northwest windstorm
1379:"The Flight of a Golf Ball"
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133:in the range ~40 to ~1000.
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2294:Ocean dynamical thermostat
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1300:Elementary Fluid Mechanics
1207:10.1152/physrev.00047.2009
1092:River eddies in whitewater
58:"Eddy" fluid dynamics
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3575:
3535:
3506:
3467:
3460:
3451:
3442:
3384:
3346:
3314:
3303:
3294:
3249:
3203:
3194:
3128:
3039:
2878:
2852:
2829:Ocean acoustic tomography
2814:
2766:
2705:
2642:Mohorovičić discontinuity
2600:
2472:
2369:
2234:General circulation model
2164:
1870:Benjamin–Feir instability
1850:
1506:Marine Pollution Bulletin
3837:Boxing Day Storm of 1998
3830:Christmas Eve storm 1997
3166:Annular tropical cyclone
2959:Ocean surface topography
2334:Thermohaline circulation
2324:Subsurface ocean current
2264:Hydrothermal circulation
2097:Wave–current interaction
1875:Boussinesq approximation
1727:"Ocean Mesoscale Eddies"
630:{\displaystyle \mu _{t}}
468:Research and development
4626:Multiple-vortex tornado
4065:Friederike (David) 2018
4058:Eleanor (Burglind) 2018
3781:December 1981 windstorm
3739:North Sea flood of 1953
3652:Christmas Flood of 1717
2996:Sea surface temperature
2979:Outline of oceanography
2174:Atmospheric circulation
2112:shallow water equations
2102:Waves and shallow water
1995:Significant wave height
1600:10.1175/JPO-D-18-0215.1
1296:Kambe, Tsutomu (2007).
1119:, or dipole eddy pairs.
882:{\displaystyle \kappa }
800:{\displaystyle S_{i,j}}
479:Navier–Stokes equations
4567:Line echo wave pattern
4521:Mesoscale ocean eddies
4290:Southern Ocean cyclone
3378:Extratropical cyclones
3171:Bar (tropical cyclone)
3161:Central dense overcast
2991:Sea surface microlayer
2356:Wind generated current
953:
936:Mesoscale ocean eddies
883:
863:
801:
766:
631:
596:
458:
387:
315:
237:
213:
200:
134:
3939:Friedhelm/Bawbag 2011
3802:Burns' Day storm 1990
3686:Night of the Big Wind
3407:Post-tropical cyclone
3156:Rapid intensification
2824:Deep scattering layer
2806:World Geodetic System
2314:Princeton Ocean Model
2194:Coriolis–Stokes force
1844:Physical oceanography
1195:Physiological Reviews
943:
884:
864:
802:
767:
632:
597:
459:
388:
316:
231:
211:
198:
145:is the swirling of a
124:
4726:Tornadoes portal
4636:Anticyclonic tornado
4604:Low-topped supercell
4382:Cape Verde hurricane
3774:Gale of January 1976
2844:Underwater acoustics
2404:Perigean spring tide
2269:Langmuir circulation
1980:Rossby-gravity waves
1077:Kármán vortex street
906:Industrial processes
873:
822:
778:
643:
614:
488:
403:
359:
255:
233:Schlieren photograph
43:improve this article
4428:Southern Hemisphere
4366:Northern Hemisphere
4254:Southern Hemisphere
4209:Western Disturbance
4023:Thomas (Doris) 2017
3795:Great storm of 1987
3760:1968 Scotland storm
3700:Tay Bridge disaster
3679:Great Storm of 1824
3645:Great Storm of 1703
3615:European windstorms
3444:Northern Hemisphere
3262:South Atlantic High
3250:Southern Hemisphere
3226:North American High
3204:Northern Hemisphere
3006:Science On a Sphere
2612:Convergent boundary
2284:Modular Ocean Model
2244:Geostrophic current
1960:Mild-slope equation
1687:2001JPO....31.3274T
1591:2019JPO....49.2345C
1259:Transport phenomena
1158:2001JPO....31.3274T
1072:Reynolds experiment
927:Environmental flows
216:In 1883, scientist
190:transport phenomena
4375:Atlantic hurricane
4331:Lake Huron cyclone
3392:Anticyclonic storm
3267:South Pacific High
3231:North Pacific High
3146:High-pressure area
3136:Anticyclonic storm
2662:Seafloor spreading
2652:Outer trench swell
2617:Divergent boundary
2517:Continental margin
2502:Carbonate platform
2399:Lunitidal interval
1358:www.cfd-online.com
954:
879:
859:
835:
797:
762:
662:
627:
592:
568:
454:
383:
311:
238:
214:
201:
135:
4735:
4734:
4695:
4694:
4691:
4690:
4687:
4686:
4631:Satellite tornado
4506:
4505:
4471:
4470:
4467:
4466:
4391:Pacific hurricane
4307:
4306:
4303:
4302:
4248:
4247:
4192:
4191:
4162:
4161:
3707:Eyemouth disaster
3623:14th-18th century
3571:
3570:
3531:
3530:
3412:Low-pressure area
3290:
3289:
3282:Subtropical ridge
3241:Subtropical ridge
3151:Low-pressure area
3121:Centers of action
3079:
3078:
3071:Oceans portal
3031:World Ocean Atlas
3021:Underwater glider
2964:Ocean temperature
2627:Hydrothermal vent
2592:Submarine volcano
2527:Continental shelf
2507:Coastal geography
2497:Bathymetric chart
2379:Amphidromic point
2067:Wave nonlinearity
1925:Infragravity wave
1681:(11): 3274–3283.
1554:www.gfdl.noaa.gov
1483:"Ocean Pollution"
1419:Dimotakis, Paul.
1377:Arnold, Douglas.
1315:978-981-256-416-0
1152:(11): 3274–3283.
834:
661:
567:
449:
434:
413:
374:
350:dynamic viscosity
309:
288:
119:
118:
111:
93:
4760:
4724:
4723:
4722:
4710:
4709:
4708:
4584:
4583:
4517:
4516:
4460:
4453:
4446:
4439:
4429:
4419:
4412:
4405:
4393:
4384:
4377:
4367:
4362:
4361:
4274:Black nor'easter
4259:
4258:
4255:
4174:Black Sea storms
4155:
4148:
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:
3878:
3860:
3853:
3846:
3839:
3832:
3825:
3818:
3816:Braer Storm 1993
3811:
3804:
3797:
3790:
3783:
3776:
3769:
3762:
3755:
3748:
3741:
3734:
3727:
3709:
3702:
3695:
3688:
3681:
3665:
3654:
3647:
3640:
3633:
3617:
3607:
3600:
3593:
3584:
3583:
3580:
3579:
3524:
3517:
3499:
3492:
3485:
3478:
3465:
3464:
3458:
3457:
3454:
3449:
3448:
3445:
3371:
3364:
3357:
3348:
3347:
3321:
3320:
3317:
3312:
3311:
3308:
3301:
3300:
3257:South Polar High
3211:North Polar High
3201:
3200:
3106:
3099:
3092:
3083:
3082:
3069:
3068:
3057:
3056:
3047:
3046:
2986:Pelagic sediment
2924:Marine pollution
2718:Deep ocean water
2587:Submarine canyon
2522:Continental rise
2414:Rule of twelfths
2329:Sverdrup balance
2259:Humboldt Current
2184:Boundary current
2159:
2148:
1965:Radiation stress
1935:Iribarren number
1910:Equatorial waves
1865:Ballantine scale
1860:Airy wave theory
1837:
1830:
1823:
1814:
1813:
1807:
1800:
1794:
1787:
1772:
1765:
1759:
1753:
1747:
1746:
1744:
1743:
1723:
1717:
1716:
1698:
1666:
1660:
1659:
1619:
1613:
1612:
1602:
1585:(9): 2345–2363.
1570:
1564:
1563:
1561:
1560:
1546:
1540:
1539:
1521:
1497:
1491:
1490:
1479:
1473:
1472:
1470:
1469:
1452:
1446:
1445:
1443:
1442:
1436:
1430:. Archived from
1425:
1416:
1410:
1409:
1407:
1406:
1392:
1386:
1385:
1383:
1374:
1368:
1367:
1365:
1364:
1350:
1344:
1343:
1341:
1340:
1326:
1320:
1319:
1303:
1293:
1287:
1286:
1280:
1272:
1254:
1248:
1243:
1237:
1236:
1226:
1186:
1177:
1176:
1174:
1168:. Archived from
1143:
1134:
984:Kuroshio Current
888:
886:
885:
880:
868:
866:
865:
860:
858:
857:
836:
827:
806:
804:
803:
798:
796:
795:
771:
769:
768:
763:
761:
760:
751:
750:
741:
740:
722:
721:
712:
711:
693:
692:
683:
682:
670:
669:
663:
654:
636:
634:
633:
628:
626:
625:
601:
599:
598:
593:
591:
590:
569:
560:
554:
553:
538:
537:
519:
518:
509:
508:
463:
461:
460:
455:
450:
448:
440:
436:
435:
432:
430:
420:
415:
414:
411:
392:
390:
389:
384:
376:
375:
372:
370:
347:
343:
335:
327:
320:
318:
317:
312:
310:
305:
294:
289:
284:
270:
265:
247:
243:
218:Osborne Reynolds
149:and the reverse
114:
107:
103:
100:
94:
92:
51:
27:
19:
4768:
4767:
4763:
4762:
4761:
4759:
4758:
4757:
4738:
4737:
4736:
4731:
4720:
4718:
4706:
4704:
4683:
4652:
4573:
4538:
4502:
4463:
4456:
4449:
4442:
4435:
4427:
4422:
4415:
4408:
4401:
4389:
4380:
4373:
4365:
4353:
4345:
4299:
4278:
4253:
4244:
4223:
4188:
4158:
4151:
4144:
4133:
4126:
4119:
4112:
4105:
4098:
4091:
4084:
4077:
4070:
4063:
4056:
4049:
4042:
4035:
4028:
4021:
4014:
4007:
4000:
3993:
3986:
3979:
3972:
3965:
3958:
3951:
3944:
3937:
3930:
3923:
3916:
3909:
3902:
3895:
3888:
3881:
3874:
3863:
3856:
3849:
3842:
3835:
3828:
3821:
3814:
3807:
3800:
3793:
3786:
3779:
3772:
3765:
3758:
3751:
3744:
3737:
3730:
3723:
3712:
3705:
3698:
3691:
3684:
3677:
3666:
3657:
3650:
3643:
3638:Burchardi flood
3636:
3631:Grote Mandrenke
3629:
3618:
3613:
3611:
3567:
3527:
3520:
3513:
3502:
3495:
3490:Great basin low
3488:
3481:
3476:Alberta clipper
3474:
3452:
3443:
3438:
3380:
3375:
3342:
3338:South Polar low
3333:North Polar low
3315:
3304:
3286:
3277:Australian High
3245:
3190:
3124:
3110:
3080:
3075:
3063:
3035:
2874:
2848:
2810:
2791:Sea-level curve
2762:
2701:
2687:Transform fault
2637:Mid-ocean ridge
2603:
2596:
2562:Oceanic plateau
2468:
2454:Tidal resonance
2424:Theory of tides
2365:
2274:Longshore drift
2224:Ekman transport
2160:
2154:
2153:
2152:
2151:
2150:
2149:
2140:
2092:Wave turbulence
2025:Trochoidal wave
1950:Longshore drift
1846:
1841:
1811:
1810:
1801:
1797:
1788:
1775:
1766:
1762:
1754:
1750:
1741:
1739:
1725:
1724:
1720:
1667:
1663:
1620:
1616:
1571:
1567:
1558:
1556:
1548:
1547:
1543:
1498:
1494:
1481:
1480:
1476:
1467:
1465:
1464:. 16 April 2016
1454:
1453:
1449:
1440:
1438:
1434:
1423:
1417:
1413:
1404:
1402:
1394:
1393:
1389:
1381:
1375:
1371:
1362:
1360:
1352:
1351:
1347:
1338:
1336:
1328:
1327:
1323:
1316:
1294:
1290:
1274:
1273:
1269:
1255:
1251:
1244:
1240:
1187:
1180:
1172:
1141:
1135:
1131:
1126:
1097:Wake turbulence
1066:Reynolds number
1036:
1011:
980:Agulhas Current
938:
929:
917:
908:
896:
874:
871:
870:
847:
843:
825:
823:
820:
819:
785:
781:
779:
776:
775:
756:
755:
746:
742:
736:
732:
717:
713:
707:
703:
688:
684:
678:
674:
665:
664:
652:
644:
641:
640:
621:
617:
615:
612:
611:
580:
576:
558:
543:
539:
533:
529:
514:
510:
504:
500:
489:
486:
485:
475:
470:
441:
431:
423:
422:
421:
419:
410:
406:
404:
401:
400:
371:
363:
362:
360:
357:
356:
345:
341:
333:
325:
295:
293:
271:
269:
258:
256:
253:
252:
245:
241:
223:Reynolds number
206:
186:fluid mechanics
175:
131:Reynolds number
115:
104:
98:
95:
52:
50:
40:
28:
17:
12:
11:
5:
4766:
4756:
4755:
4750:
4748:Fluid dynamics
4733:
4732:
4730:
4729:
4715:
4700:
4697:
4696:
4693:
4692:
4689:
4688:
4685:
4684:
4682:
4681:
4676:
4671:
4666:
4660:
4658:
4654:
4653:
4651:
4650:
4645:
4640:
4639:
4638:
4633:
4628:
4618:
4613:
4612:
4611:
4606:
4601:
4590:
4588:
4581:
4575:
4574:
4572:
4571:
4570:
4569:
4559:
4554:
4548:
4546:
4540:
4539:
4537:
4536:
4531:
4525:
4523:
4514:
4508:
4507:
4504:
4503:
4501:
4500:
4495:
4490:
4485:
4479:
4477:
4473:
4472:
4469:
4468:
4465:
4464:
4462:
4461:
4454:
4447:
4440:
4432:
4430:
4424:
4423:
4421:
4420:
4413:
4406:
4399:
4394:
4387:
4386:
4385:
4370:
4368:
4359:
4347:
4346:
4344:
4343:
4338:
4333:
4328:
4323:
4317:
4315:
4309:
4308:
4305:
4304:
4301:
4300:
4298:
4297:
4292:
4286:
4284:
4280:
4279:
4277:
4276:
4271:
4265:
4263:
4256:
4250:
4249:
4246:
4245:
4243:
4242:
4237:
4231:
4229:
4225:
4224:
4222:
4221:
4216:
4211:
4206:
4200:
4198:
4194:
4193:
4190:
4189:
4187:
4186:
4181:
4176:
4170:
4168:
4164:
4163:
4160:
4159:
4157:
4156:
4149:
4141:
4139:
4135:
4134:
4132:
4131:
4124:
4117:
4110:
4103:
4096:
4089:
4082:
4075:
4068:
4061:
4054:
4047:
4040:
4033:
4026:
4019:
4012:
4005:
3998:
3995:Christina 2014
3991:
3984:
3977:
3970:
3963:
3956:
3949:
3942:
3935:
3928:
3921:
3914:
3907:
3900:
3893:
3886:
3879:
3871:
3869:
3865:
3864:
3862:
3861:
3854:
3847:
3840:
3833:
3826:
3819:
3812:
3805:
3798:
3791:
3784:
3777:
3770:
3767:Quimburga 1972
3763:
3756:
3749:
3742:
3735:
3728:
3720:
3718:
3714:
3713:
3711:
3710:
3703:
3696:
3689:
3682:
3674:
3672:
3668:
3667:
3660:
3658:
3656:
3655:
3648:
3641:
3634:
3626:
3624:
3620:
3619:
3610:
3609:
3602:
3595:
3587:
3577:
3573:
3572:
3569:
3568:
3566:
3565:
3560:
3555:
3550:
3545:
3539:
3537:
3533:
3532:
3529:
3528:
3526:
3525:
3518:
3515:Panhandle hook
3510:
3508:
3504:
3503:
3501:
3500:
3493:
3486:
3479:
3471:
3469:
3462:
3455:
3446:
3440:
3439:
3437:
3436:
3431:
3430:
3429:
3419:
3414:
3409:
3404:
3399:
3394:
3388:
3386:
3382:
3381:
3374:
3373:
3366:
3359:
3351:
3344:
3343:
3341:
3340:
3335:
3329:
3327:
3318:
3309:
3306:Synoptic scale
3298:
3292:
3291:
3288:
3287:
3285:
3284:
3279:
3274:
3269:
3264:
3259:
3253:
3251:
3247:
3246:
3244:
3243:
3238:
3233:
3228:
3223:
3218:
3213:
3207:
3205:
3198:
3192:
3191:
3189:
3188:
3183:
3178:
3173:
3168:
3163:
3158:
3153:
3148:
3143:
3138:
3132:
3130:
3126:
3125:
3119:of the world (
3109:
3108:
3101:
3094:
3086:
3077:
3076:
3074:
3073:
3061:
3051:
3040:
3037:
3036:
3034:
3033:
3028:
3023:
3018:
3013:
3011:Stratification
3008:
3003:
2998:
2993:
2988:
2983:
2982:
2981:
2971:
2966:
2961:
2956:
2951:
2946:
2941:
2936:
2931:
2926:
2921:
2916:
2911:
2903:
2901:Color of water
2898:
2896:Benthic lander
2893:
2888:
2882:
2880:
2876:
2875:
2873:
2872:
2867:
2862:
2856:
2854:
2850:
2849:
2847:
2846:
2841:
2836:
2831:
2826:
2820:
2818:
2812:
2811:
2809:
2808:
2803:
2801:Sea level rise
2798:
2796:Sea level drop
2793:
2788:
2783:
2778:
2772:
2770:
2764:
2763:
2761:
2760:
2755:
2750:
2745:
2740:
2735:
2730:
2725:
2720:
2715:
2709:
2707:
2703:
2702:
2700:
2699:
2694:
2689:
2684:
2679:
2674:
2669:
2664:
2659:
2654:
2649:
2644:
2639:
2634:
2632:Marine geology
2629:
2624:
2619:
2614:
2608:
2606:
2598:
2597:
2595:
2594:
2589:
2584:
2579:
2574:
2572:Passive margin
2569:
2567:Oceanic trench
2564:
2559:
2554:
2549:
2544:
2539:
2534:
2529:
2524:
2519:
2514:
2509:
2504:
2499:
2494:
2489:
2484:
2478:
2476:
2470:
2469:
2467:
2466:
2461:
2456:
2451:
2446:
2441:
2436:
2431:
2426:
2421:
2416:
2411:
2406:
2401:
2396:
2391:
2386:
2381:
2375:
2373:
2367:
2366:
2364:
2363:
2358:
2353:
2348:
2343:
2342:
2341:
2331:
2326:
2321:
2316:
2311:
2306:
2301:
2299:Ocean dynamics
2296:
2291:
2286:
2281:
2276:
2271:
2266:
2261:
2256:
2251:
2246:
2241:
2236:
2231:
2226:
2221:
2216:
2211:
2206:
2201:
2196:
2191:
2189:Coriolis force
2186:
2181:
2176:
2170:
2168:
2162:
2161:
2143:
2141:
2139:
2138:
2137:
2136:
2126:
2121:
2116:
2115:
2114:
2109:
2099:
2094:
2089:
2084:
2079:
2074:
2069:
2064:
2059:
2054:
2049:
2044:
2039:
2038:
2037:
2027:
2022:
2017:
2012:
2010:Stokes problem
2007:
2002:
1997:
1992:
1987:
1982:
1977:
1972:
1967:
1962:
1957:
1952:
1947:
1945:Kinematic wave
1942:
1937:
1932:
1927:
1922:
1917:
1912:
1907:
1902:
1897:
1892:
1887:
1882:
1877:
1872:
1867:
1862:
1856:
1854:
1848:
1847:
1840:
1839:
1832:
1825:
1817:
1809:
1808:
1795:
1773:
1760:
1748:
1718:
1661:
1634:(3): 327–341.
1614:
1565:
1541:
1492:
1474:
1447:
1411:
1387:
1369:
1345:
1321:
1314:
1288:
1267:
1249:
1238:
1201:(1): 327–387.
1178:
1175:on 2011-04-01.
1128:
1127:
1125:
1122:
1121:
1120:
1114:
1109:
1104:
1099:
1094:
1089:
1084:
1079:
1074:
1069:
1063:
1061:Irminger Rings
1058:
1053:
1051:Eddy diffusion
1048:
1042:
1035:
1032:
1016:apex predators
1010:
1007:
950:Canary Islands
937:
934:
928:
925:
916:
913:
907:
904:
895:
892:
891:
890:
878:
856:
853:
850:
846:
842:
839:
833:
830:
815:
814:
813:
812:
794:
791:
788:
784:
773:
759:
754:
749:
745:
739:
735:
731:
728:
725:
720:
716:
710:
706:
702:
699:
696:
691:
687:
681:
677:
673:
668:
660:
657:
651:
648:
638:
624:
620:
603:
602:
589:
586:
583:
579:
575:
572:
566:
563:
557:
552:
549:
546:
542:
536:
532:
528:
525:
522:
517:
513:
507:
503:
499:
496:
493:
474:
471:
469:
466:
465:
464:
453:
447:
444:
439:
429:
426:
418:
409:
394:
393:
382:
379:
369:
366:
332:of the fluid,
322:
321:
308:
304:
301:
298:
292:
287:
283:
280:
277:
274:
268:
264:
261:
205:
202:
174:
171:
139:fluid dynamics
117:
116:
31:
29:
22:
15:
9:
6:
4:
3:
2:
4765:
4754:
4751:
4749:
4746:
4745:
4743:
4728:
4727:
4716:
4714:
4713:
4702:
4701:
4698:
4680:
4677:
4675:
4672:
4670:
4667:
4665:
4662:
4661:
4659:
4655:
4649:
4646:
4644:
4641:
4637:
4634:
4632:
4629:
4627:
4624:
4623:
4622:
4619:
4617:
4614:
4610:
4607:
4605:
4602:
4600:
4597:
4596:
4595:
4592:
4591:
4589:
4585:
4582:
4580:
4576:
4568:
4565:
4564:
4563:
4560:
4558:
4555:
4553:
4550:
4549:
4547:
4545:
4541:
4535:
4532:
4530:
4529:Catalina eddy
4527:
4526:
4524:
4522:
4518:
4515:
4513:
4509:
4499:
4496:
4494:
4491:
4489:
4486:
4484:
4483:Cold-core low
4481:
4480:
4478:
4474:
4459:
4455:
4452:
4448:
4445:
4441:
4438:
4434:
4433:
4431:
4425:
4418:
4414:
4411:
4407:
4404:
4400:
4398:
4395:
4392:
4388:
4383:
4379:
4378:
4376:
4372:
4371:
4369:
4363:
4360:
4357:
4352:
4348:
4342:
4339:
4337:
4334:
4332:
4329:
4327:
4324:
4322:
4319:
4318:
4316:
4314:
4310:
4296:
4293:
4291:
4288:
4287:
4285:
4281:
4275:
4272:
4270:
4267:
4266:
4264:
4260:
4257:
4251:
4241:
4238:
4236:
4233:
4232:
4230:
4226:
4220:
4217:
4215:
4212:
4210:
4207:
4205:
4202:
4201:
4199:
4195:
4185:
4182:
4180:
4179:Icelandic Low
4177:
4175:
4172:
4171:
4169:
4165:
4154:
4150:
4147:
4143:
4142:
4140:
4136:
4129:
4125:
4122:
4118:
4115:
4111:
4108:
4104:
4101:
4097:
4094:
4090:
4087:
4083:
4080:
4076:
4073:
4069:
4066:
4062:
4059:
4055:
4052:
4048:
4045:
4041:
4038:
4034:
4031:
4027:
4024:
4020:
4017:
4013:
4010:
4006:
4003:
3999:
3996:
3992:
3989:
3985:
3982:
3978:
3975:
3971:
3968:
3964:
3961:
3957:
3954:
3950:
3947:
3943:
3940:
3936:
3933:
3929:
3926:
3922:
3919:
3915:
3912:
3908:
3905:
3901:
3898:
3894:
3891:
3887:
3884:
3880:
3877:
3873:
3872:
3870:
3866:
3859:
3855:
3852:
3848:
3845:
3841:
3838:
3834:
3831:
3827:
3824:
3820:
3817:
3813:
3810:
3806:
3803:
3799:
3796:
3792:
3789:
3785:
3782:
3778:
3775:
3771:
3768:
3764:
3761:
3757:
3754:
3750:
3747:
3743:
3740:
3736:
3733:
3729:
3726:
3722:
3721:
3719:
3715:
3708:
3704:
3701:
3697:
3694:
3690:
3687:
3683:
3680:
3676:
3675:
3673:
3669:
3664:
3653:
3649:
3646:
3642:
3639:
3635:
3632:
3628:
3627:
3625:
3621:
3616:
3608:
3603:
3601:
3596:
3594:
3589:
3588:
3585:
3581:
3578:
3574:
3564:
3561:
3559:
3556:
3554:
3551:
3549:
3546:
3544:
3541:
3540:
3538:
3534:
3523:
3522:November gale
3519:
3516:
3512:
3511:
3509:
3505:
3498:
3494:
3491:
3487:
3484:
3480:
3477:
3473:
3472:
3470:
3466:
3463:
3459:
3456:
3453:North America
3450:
3447:
3441:
3435:
3432:
3428:
3425:
3424:
3423:
3420:
3418:
3415:
3413:
3410:
3408:
3405:
3403:
3400:
3398:
3395:
3393:
3390:
3389:
3387:
3383:
3379:
3372:
3367:
3365:
3360:
3358:
3353:
3352:
3349:
3345:
3339:
3336:
3334:
3331:
3330:
3328:
3326:
3322:
3319:
3316:Surface-based
3313:
3310:
3307:
3302:
3299:
3297:
3293:
3283:
3280:
3278:
3275:
3273:
3272:Kalahari High
3270:
3268:
3265:
3263:
3260:
3258:
3255:
3254:
3252:
3248:
3242:
3239:
3237:
3234:
3232:
3229:
3227:
3224:
3222:
3219:
3217:
3216:Siberian High
3214:
3212:
3209:
3208:
3206:
3202:
3199:
3197:
3193:
3187:
3184:
3182:
3179:
3177:
3174:
3172:
3169:
3167:
3164:
3162:
3159:
3157:
3154:
3152:
3149:
3147:
3144:
3142:
3139:
3137:
3134:
3133:
3131:
3127:
3122:
3118:
3114:
3107:
3102:
3100:
3095:
3093:
3088:
3087:
3084:
3072:
3067:
3062:
3060:
3052:
3050:
3042:
3041:
3038:
3032:
3029:
3027:
3024:
3022:
3019:
3017:
3014:
3012:
3009:
3007:
3004:
3002:
2999:
2997:
2994:
2992:
2989:
2987:
2984:
2980:
2977:
2976:
2975:
2972:
2970:
2967:
2965:
2962:
2960:
2957:
2955:
2952:
2950:
2947:
2945:
2942:
2940:
2937:
2935:
2932:
2930:
2927:
2925:
2922:
2920:
2919:Marine energy
2917:
2915:
2912:
2910:
2909:
2904:
2902:
2899:
2897:
2894:
2892:
2889:
2887:
2886:Acidification
2884:
2883:
2881:
2877:
2871:
2868:
2866:
2863:
2861:
2858:
2857:
2855:
2851:
2845:
2842:
2840:
2839:SOFAR channel
2837:
2835:
2832:
2830:
2827:
2825:
2822:
2821:
2819:
2817:
2813:
2807:
2804:
2802:
2799:
2797:
2794:
2792:
2789:
2787:
2784:
2782:
2779:
2777:
2774:
2773:
2771:
2769:
2765:
2759:
2756:
2754:
2751:
2749:
2746:
2744:
2741:
2739:
2736:
2734:
2731:
2729:
2726:
2724:
2721:
2719:
2716:
2714:
2711:
2710:
2708:
2704:
2698:
2695:
2693:
2690:
2688:
2685:
2683:
2680:
2678:
2675:
2673:
2670:
2668:
2665:
2663:
2660:
2658:
2655:
2653:
2650:
2648:
2647:Oceanic crust
2645:
2643:
2640:
2638:
2635:
2633:
2630:
2628:
2625:
2623:
2622:Fracture zone
2620:
2618:
2615:
2613:
2610:
2609:
2607:
2605:
2599:
2593:
2590:
2588:
2585:
2583:
2580:
2578:
2575:
2573:
2570:
2568:
2565:
2563:
2560:
2558:
2557:Oceanic basin
2555:
2553:
2550:
2548:
2545:
2543:
2540:
2538:
2535:
2533:
2530:
2528:
2525:
2523:
2520:
2518:
2515:
2513:
2510:
2508:
2505:
2503:
2500:
2498:
2495:
2493:
2490:
2488:
2487:Abyssal plain
2485:
2483:
2480:
2479:
2477:
2475:
2471:
2465:
2462:
2460:
2457:
2455:
2452:
2450:
2447:
2445:
2442:
2440:
2437:
2435:
2432:
2430:
2427:
2425:
2422:
2420:
2417:
2415:
2412:
2410:
2407:
2405:
2402:
2400:
2397:
2395:
2394:Internal tide
2392:
2390:
2387:
2385:
2382:
2380:
2377:
2376:
2374:
2372:
2368:
2362:
2359:
2357:
2354:
2352:
2349:
2347:
2344:
2340:
2337:
2336:
2335:
2332:
2330:
2327:
2325:
2322:
2320:
2317:
2315:
2312:
2310:
2307:
2305:
2302:
2300:
2297:
2295:
2292:
2290:
2289:Ocean current
2287:
2285:
2282:
2280:
2277:
2275:
2272:
2270:
2267:
2265:
2262:
2260:
2257:
2255:
2252:
2250:
2247:
2245:
2242:
2240:
2237:
2235:
2232:
2230:
2227:
2225:
2222:
2220:
2217:
2215:
2212:
2210:
2207:
2205:
2202:
2200:
2197:
2195:
2192:
2190:
2187:
2185:
2182:
2180:
2177:
2175:
2172:
2171:
2169:
2167:
2163:
2158:
2147:
2135:
2132:
2131:
2130:
2127:
2125:
2122:
2120:
2117:
2113:
2110:
2108:
2105:
2104:
2103:
2100:
2098:
2095:
2093:
2090:
2088:
2087:Wave shoaling
2085:
2083:
2080:
2078:
2075:
2073:
2070:
2068:
2065:
2063:
2060:
2058:
2055:
2053:
2050:
2048:
2047:Ursell number
2045:
2043:
2040:
2036:
2033:
2032:
2031:
2028:
2026:
2023:
2021:
2018:
2016:
2013:
2011:
2008:
2006:
2003:
2001:
1998:
1996:
1993:
1991:
1988:
1986:
1983:
1981:
1978:
1976:
1973:
1971:
1968:
1966:
1963:
1961:
1958:
1956:
1953:
1951:
1948:
1946:
1943:
1941:
1938:
1936:
1933:
1931:
1930:Internal wave
1928:
1926:
1923:
1921:
1918:
1916:
1913:
1911:
1908:
1906:
1903:
1901:
1898:
1896:
1893:
1891:
1888:
1886:
1883:
1881:
1880:Breaking wave
1878:
1876:
1873:
1871:
1868:
1866:
1863:
1861:
1858:
1857:
1855:
1853:
1849:
1845:
1838:
1833:
1831:
1826:
1824:
1819:
1818:
1815:
1806:
1799:
1793:
1786:
1784:
1782:
1780:
1778:
1771:
1764:
1758:
1752:
1738:
1734:
1733:
1728:
1722:
1714:
1710:
1706:
1702:
1697:
1692:
1688:
1684:
1680:
1676:
1672:
1665:
1657:
1653:
1649:
1645:
1641:
1637:
1633:
1629:
1625:
1618:
1610:
1606:
1601:
1596:
1592:
1588:
1584:
1580:
1576:
1569:
1555:
1551:
1545:
1537:
1533:
1529:
1525:
1520:
1515:
1511:
1507:
1503:
1496:
1488:
1484:
1478:
1463:
1462:
1461:Science Daily
1457:
1451:
1437:on 2017-08-08
1433:
1429:
1422:
1415:
1401:
1397:
1391:
1380:
1373:
1359:
1355:
1349:
1335:
1331:
1325:
1317:
1311:
1307:
1302:
1301:
1292:
1284:
1278:
1270:
1268:0-471-41077-2
1264:
1260:
1253:
1247:
1242:
1234:
1230:
1225:
1220:
1216:
1212:
1208:
1204:
1200:
1196:
1192:
1185:
1183:
1171:
1167:
1163:
1159:
1155:
1151:
1147:
1140:
1133:
1129:
1118:
1115:
1113:
1110:
1108:
1105:
1103:
1100:
1098:
1095:
1093:
1090:
1088:
1085:
1083:
1080:
1078:
1075:
1073:
1070:
1067:
1064:
1062:
1059:
1057:
1054:
1052:
1049:
1046:
1043:
1041:
1038:
1037:
1031:
1027:
1023:
1019:
1017:
1006:
1002:
1000:
996:
992:
987:
985:
981:
977:
973:
969:
964:
961:
958:
951:
947:
942:
933:
924:
922:
921:phytoplankton
912:
903:
900:
876:
854:
851:
848:
844:
840:
837:
831:
828:
817:
816:
810:
807: is the
792:
789:
786:
782:
774:
747:
743:
737:
733:
726:
718:
714:
708:
704:
697:
689:
685:
679:
675:
658:
655:
649:
646:
639:
622:
618:
610:
609:
608:
607:
606:
587:
584:
581:
577:
573:
570:
564:
561:
555:
550:
547:
544:
540:
534:
530:
526:
523:
515:
511:
505:
501:
494:
491:
484:
483:
482:
480:
451:
445:
442:
437:
416:
407:
399:
398:
397:
380:
377:
355:
354:
353:
351:
339:
331:
306:
302:
299:
296:
290:
285:
281:
278:
275:
272:
266:
251:
250:
249:
244:(or diameter
234:
230:
226:
224:
219:
210:
197:
193:
191:
187:
182:
180:
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127:vortex street
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60: –
59:
55:
54:Find sources:
48:
44:
38:
37:
32:This article
30:
26:
21:
20:
4717:
4703:
4616:Funnel cloud
4534:Haida Eddies
4493:Polar vortex
4051:Herwart 2017
4044:Ophelia 2017
3967:St Jude 2013
3946:Joachim 2011
3925:Xynthia 2010
3883:Jeanett 2002
3868:21st century
3788:Charley 1986
3725:Ulysses 1903
3717:20th century
3671:19th century
3548:Hatteras low
3543:Aleutian Low
3483:Colorado low
3417:Weather bomb
3117:anticyclones
3026:Water column
2974:Oceanography
2949:Observations
2944:Explorations
2914:Marginal sea
2907:
2865:OSTM/Jason-2
2697:Volcanic arc
2672:Slab suction
2389:Head of tide
2279:Loop Current
2219:Ekman spiral
2208:
2005:Stokes drift
1915:Gravity wave
1890:Cnoidal wave
1798:
1763:
1751:
1740:. Retrieved
1730:
1721:
1678:
1674:
1664:
1631:
1627:
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1568:
1557:. Retrieved
1553:
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1509:
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1495:
1486:
1477:
1466:. Retrieved
1459:
1450:
1439:. Retrieved
1432:the original
1427:
1414:
1403:. Retrieved
1400:math.ucr.edu
1399:
1390:
1372:
1361:. Retrieved
1357:
1348:
1337:. Retrieved
1333:
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1299:
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1258:
1252:
1241:
1198:
1194:
1170:the original
1149:
1145:
1132:
1112:Hemodynamics
1107:Laminar flow
1056:Haida Eddies
1045:Eddy pumping
1028:
1024:
1020:
1012:
1003:
999:Haida Eddies
995:anticyclonic
988:
965:
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959:
955:
930:
918:
909:
899:Hemodynamics
897:
894:Hemodynamics
808:
604:
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323:
239:
215:
183:
176:
160:
142:
136:
105:
96:
86:
79:
72:
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53:
41:Please help
36:verification
33:
4674:Steam devil
4594:Mesocyclone
4488:Cut-off low
4476:Upper level
4313:Subtropical
4283:Other areas
4228:Other areas
4204:Asiatic Low
4128:Ciarán 2023
4114:Larisa 2023
4107:Eunice 2022
4093:Aurore 2021
4086:Dennis 2020
4072:Adrian 2018
4037:Xavier 2017
4009:Niklas 2015
3960:Andrea 2012
3953:Dagmar 2011
3904:Kyrill 2007
3890:Gudrun 2005
3876:Oratia 2000
3858:Martin 1999
3851:Lothar 1999
3844:Anatol 1999
3746:Debbie 1961
3732:Iberia 1941
3497:Bighorn Low
3468:Lee Cyclone
3461:Continental
3221:Azores High
3196:Anticyclone
3016:Thermocline
2733:Mesopelagic
2706:Ocean zones
2677:Slab window
2542:Hydrography
2482:Abyssal fan
2449:Tidal range
2439:Tidal power
2434:Tidal force
2319:Rip current
2254:Gulf Stream
2214:Ekman layer
2204:Downwelling
2179:Baroclinity
2166:Circulation
2062:Wave height
2052:Wave action
2035:megatsunami
2015:Stokes wave
1975:Rossby wave
1940:Kelvin wave
1920:Green's law
976:Gulf Stream
811:strain rate
167:Rossby wave
4742:Categories
4679:Fire whirl
4669:Dust devil
4648:Waterspout
4609:Wall cloud
4321:Kona storm
4240:Kona storm
4121:Babet 2023
4100:Malik 2022
4079:Ciara 2020
3974:Xaver 2013
3932:Berit 2011
3918:Klaus 2009
3553:Nor'easter
3176:Superstorm
2954:Reanalysis
2853:Satellites
2834:Sofar bomb
2682:Subduction
2657:Ridge push
2552:Ocean bank
2532:Contourite
2459:Tide gauge
2444:Tidal race
2429:Tidal bore
2419:Slack tide
2384:Earth tide
2304:Ocean gyre
2124:Wind setup
2119:Wind fetch
2082:Wave setup
2077:Wave radar
2072:Wave power
1970:Rogue wave
1900:Dispersion
1742:2021-06-10
1559:2017-02-12
1512:: 111024.
1468:2017-02-12
1441:2017-03-06
1405:2017-02-12
1363:2017-02-12
1339:2017-02-12
1330:"Pressure"
1124:References
972:oxbow lake
69:newspapers
4643:Landspout
4599:Supercell
4579:Whirlwind
4512:Mesoscale
4295:Sudestada
4262:Australia
4184:Genoa low
4030:Zeus 2017
4016:Egon 2017
4002:Tini 2014
3988:Anne 2014
3981:Dirk 2013
3911:Emma 2008
3823:Lili 1996
3422:Sting jet
3181:Hypercane
2816:Acoustics
2768:Sea level
2667:Slab pull
2604:tectonics
2512:Cold seep
2474:Landforms
2351:Whirlpool
2346:Upwelling
2129:Wind wave
2057:Wave base
1985:Sea state
1905:Edge wave
1895:Cross sea
1713:130455873
1705:1520-0485
1656:123151803
1648:0142-727X
1609:0022-3670
1528:0025-326X
1277:cite book
1215:0031-9333
1087:Whirlwind
1082:Whirlpool
997:(such as
877:κ
845:δ
841:κ
838:ρ
753:⟩
730:⟨
724:⟩
701:⟨
695:⟩
672:⟨
647:κ
619:μ
578:δ
574:κ
571:ρ
556:−
531:μ
521:⟩
498:⟨
495:ρ
492:−
443:ρ
438:μ
378:≈
307:μ
297:ρ
286:μ
279:ρ
155:turbulent
99:July 2013
4753:Vortices
4664:Gustnado
4557:Mesohigh
4552:Wake Low
4351:Tropical
4138:See also
3897:Per 2007
3558:Gulf low
3434:Rainband
3385:Concepts
3129:Concepts
3113:Cyclones
3049:Category
3001:Seawater
2728:Littoral
2723:Deep sea
2582:Seamount
2464:Tideline
2409:Rip tide
2339:shutdown
2309:Overflow
2042:Undertow
1885:Clapotis
1536:32319887
1233:21248169
1034:See also
991:cyclonic
948:and the
330:velocity
4621:Tornado
4397:Typhoon
4356:Outline
4341:Thermal
3536:Oceanic
3402:Cyclone
3296:Cyclone
3059:Commons
2929:Mooring
2879:Related
2870:Jason-3
2860:Jason-1
2743:Pelagic
2738:Oceanic
2713:Benthic
2030:Tsunami
2000:Soliton
1683:Bibcode
1587:Bibcode
1224:3844671
1154:Bibcode
946:Madeira
348:is the
338:density
336:is its
328:is the
236:mirror.
151:current
83:scholar
4235:Arctic
3576:Europe
2748:Photic
2577:Seabed
1990:Seiche
1711:
1703:
1654:
1646:
1607:
1534:
1526:
1312:
1265:
1231:
1221:
1213:
1117:Modons
1040:Vortex
982:, the
978:, the
605:where
324:where
163:vortex
85:
78:
71:
64:
56:
4657:Minor
4587:Major
4167:Other
3507:Other
3397:Storm
3325:Polar
3141:Storm
2939:Ocean
2908:Alvin
2758:Swash
2602:Plate
2547:Knoll
2537:Guyot
2492:Atoll
2371:Tides
2134:model
2020:Swell
1852:Waves
1709:S2CID
1652:S2CID
1435:(PDF)
1424:(PDF)
1382:(PDF)
1173:(PDF)
1142:(PDF)
381:2000.
179:swirl
147:fluid
141:, an
90:JSTOR
76:books
4197:Asia
3427:List
3115:and
2906:DSV
2891:Argo
2753:Surf
2209:Eddy
1737:NOAA
1701:ISSN
1644:ISSN
1605:ISSN
1532:PMID
1524:ISSN
1310:ISBN
1283:link
1263:ISBN
1229:PMID
1211:ISSN
809:mean
188:and
143:eddy
62:news
1691:doi
1636:doi
1595:doi
1514:doi
1510:154
1306:240
1219:PMC
1203:doi
1162:doi
993:or
248:):
184:In
137:In
45:by
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502:u
452:.
446:d
433:c
428:e
425:R
417:=
412:c
408:v
373:c
368:e
365:R
346:μ
342:r
334:ρ
326:v
303:d
300:v
291:=
282:r
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273:2
267:=
263:e
260:R
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