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- ...es (TUSKs)''' are underwater devices designed to harness energy from ocean currents.<ref>Minesto, 2021</ref> ...e energy technology for generating electricity in regions with predictable currents, such as tidal zones. ...6 KB (799 words) - 17:00, 11 November 2024
- {{For|the album by Dol Ammad|Ocean Dynamics}} ...: mixed (surface) layer, upper ocean (above the [[thermocline]]), and deep ocean. ...7 KB (1,008 words) - 00:21, 5 October 2023
- {{short description|Ocean current with dynamics determined by the presence of a coastline}} ...:North Pacific Subtropical Convergence Zone.jpg|thumb|right|The main ocean currents involved with the North Pacific Gyre]] ...15 KB (2,154 words) - 19:20, 21 October 2023
- ...ription|A summary of wind stress. A very important concept for large scale ocean circulation models.}} ...n of 20–35% and thus, results in a different simulation of the large scale ocean circulation.<ref name=":2" /> ...19 KB (2,992 words) - 19:24, 28 May 2024
- ...open ocean. This velocity, caused by winds blowing over the surface of the ocean, is such that the [[Coriolis force]] on this layer is balanced by the force ...onally on the [[Ekman layer]], which typically is the upper 50–100m in the ocean. The frictional surface flow ('''''u''''') is at an angle to the right of t ...11 KB (1,639 words) - 13:02, 29 January 2025
- ...m of strong [[westerlies]], and hence do not enhance their respective mean currents. Where eddy saturations impacts the [[Antarctic Circumpolar Current]] (ACC) ...|display-authors=etal |date= June 2002 |title= Saturation of the Southern Ocean CO2 Sink Due to Recent Climate Change |url=https://www.researchgate.net/pub ...14 KB (1,903 words) - 11:08, 15 January 2024
- {{short description|Narrow, southward-flowing ocean current along the southeastern coast of the Philippines}} ...th Equatorial Current, (5) Kuroshio current, (6) the beginnings and feeder currents of the Kuroshio (gradated to indicate that it strengthens to the North), (7 ...14 KB (2,024 words) - 02:18, 28 November 2023
- {{Short description|Set of python packages for Langragian ocean analysis}} ...ics.<ref name="langrarianframework">Parcels v0.9: prototyping a Lagrangian Ocean Analysis framework for the petascale age Lange, M and E van Sebille (2017), ...15 KB (2,199 words) - 12:54, 17 August 2024
- ...[Arctic Ocean]] led to a salinity anomaly in the northern [[North Atlantic Ocean]], which affected the [[Atlantic meridional overturning circulation]].<ref> ...ts. For the 1970s GSA, the propagation was traceable around the Atlantic [[Ocean gyre#Subpolar gyres|sub-polar gyre]] from its origins in the northeast of [ ...12 KB (1,782 words) - 05:02, 26 December 2023
- ...=Smith|first3=K. Shafer|date=2011-09-01|title=Baroclinic Turbulence in the Ocean: Analysis with Primitive Equation and Quasigeostrophic Simulations|journal= ...ossby radius of deformation]], which strongly varies with latitude for the ocean. ...18 KB (2,670 words) - 01:53, 3 December 2024
- [[File:Barents Sea map.png|thumb|Location of the Barents Sea in the Arctic Ocean.]] ...ars Henrik |last7=Smirnov |first7=Alexander |date=2016-05-01 |title=Arctic Ocean Heat Impact on Regional Ice Decay: A Suggested Positive Feedback |journal=J ...15 KB (2,261 words) - 22:31, 15 November 2024
- In [[physical oceanography]], '''undertow''' is the [[ocean current|undercurrent]] that moves offshore while [[wind wave|waves]] approa ...hore-approaching waves, whereas rip currents are localized narrow offshore currents occurring at certain locations along the coast.<ref> ...12 KB (1,710 words) - 16:55, 1 December 2024
- ...m of the [[North Equatorial Current]] and consists of northwestern Pacific Ocean water. The other arm is the southward flowing [[Mindanao Current]]. The Kur ...ation of the North Equatorial Current (NEC) into the Kuroshio and Mindanao currents. The anticyclonic gyre in the South China Sea is weaker than the (sub)tropi ...16 KB (2,325 words) - 04:56, 19 October 2024
- ...cation of [[fluid dynamics]] to naturally occurring flows, such as lava, [[ocean]]s, and [[atmosphere]]s, on [[Earth]] and other [[planet]]s.<ref>{{cite jou [[Ocean circulation]] and [[air circulation]] are typically studied in oceanography ...10 KB (1,377 words) - 02:47, 23 February 2025
- ...of [[low-pressure area|low pressure systems]] and [[ocean current|oceanic currents]]. ...indicate the path of the current and the colours indicate the depth of the ocean floor.]] ...12 KB (1,936 words) - 11:29, 16 June 2024
- ...ave]]s on beaches induce variations in radiation stress, driving longshore currents. The resulting longshore [[sediment transport]] shapes the beaches, and may ...he mean surface elevation ([[wave setup]]) and the mean flow (wave-induced currents). ...21 KB (3,060 words) - 19:46, 20 June 2024
- ...|last2=Rosenthal |first2=W. |date=1984 |title=Wave setup and wave-induced currents in coastal zones |url=http://doi.wiley.com/10.1029/JC089iC02p01973 |journal The wave setup at ocean beaches can be significant. For example, a wave with a height of 5 m (on de ...9 KB (1,310 words) - 08:11, 17 February 2024
- ...at loss and evaporation from the free surface, and changes of direction of currents. ...surface waters converge, the surface water is pushed downwards.<ref name="Ocean motion" /> These mixing effects destabilise and reduce stratification. ...25 KB (3,777 words) - 02:34, 23 February 2025
- '''The depth of the seafloor''' on the flanks of a [[mid-ocean ridge]] is determined mainly by the ''age'' of the [[oceanic lithosphere]]; ...a|editor=A. E. J. Engel|place=Boulder, CO|pages=599–620|chapter=History of Ocean Basins|editor2=Harold L. James|editor3=B. F. Leonard|chapter-url=http://www ...17 KB (2,679 words) - 04:38, 21 February 2025
- ...the result of the continental barriers, resonance due to the shape of the ocean basin, the tidal waves impossibility to keep up with the Moons tracking, th ...nd possibly [[Nonlinear dynamics|nonlinear]] relative to tides in the deep ocean.<ref>{{Citation|last1=Parker|first1=Bruce B.|title=Tidal height and current ...25 KB (4,020 words) - 12:30, 3 December 2024