Thermohaline circulation

Short description: Part of large-scale ocean circulation

A summary of the path of the thermohaline circulation. Blue paths represent deep-water currents, while red paths represent surface currents.

File:Thermohaline Circulation using Improved Flow Field.ogv

Thermohaline circulation (THC) is a part of the large-scale ocean circulation driven by global density gradients formed by surface heat and freshwater fluxes.[1][2] The name thermohaline is derived from thermo-, referring to temperature, and haline, referring to salt content—factors which together determine the density of sea water.

Wind-driven surface currents (such as the Gulf Stream) travel polewards from the equatorial Atlantic Ocean, cooling and sinking en-route to higher latitudes \- eventually becoming part of the North Atlantic Deep Water \- before flowing into the ocean basins.[3] While the bulk of thermohaline water upwells in the Southern Ocean, the oldest waters (with a transit time of approximately 1000 years) upwell in the North Pacific;[4] extensive mixing takes place between the ocean basins, reducing the difference in their densities, forming the Earth's oceans a global system.[3] The water in these circuits transport energy - as heat - and mass - as dissolved solids and gases - around the globe. Consequently, the state of the circulation greatly impacts the climate of Earth.

The thermohaline circulation is often referred to as the ocean conveyor belt, great ocean conveyor, or "global conveyor belt" - a term coined by climate scientist Wallace Smith Broecker.[5][6] It is also known as the meridional overturning circulation, or MOC; a name used to signify that circulation patterns caused by temperature and salinity gradients are not necessarily part of a single global circulation. This is due, in part, to the difficulty in separating parts of the circulation driven by temperature and salinity from those affected by factors such as wind and tidal force.[7]

This global circulation comprises two major "limbs;" the Atlantic meridional overturning circulation (AMOC) centered in the north Atlantic Ocean, and the Southern Ocean overturning circulation, or Southern Ocean meridional circulation (SMOC) located near Antarctica. Since 90% of the human population occupies the Northern Hemisphere,[8] more extensive research has been undertaken on the AMOC, however the SMOC is of equal importance to the global climate. Evidence suggests both circulations are slowing due to climate change in line with increasing rates of dilution from melting ice sheets \- critically affecting the salinity of Antarctic bottom water.[9][10] In addition, the potential for outright collapse of either circulation to a much weaker state exemplifies tipping points in the climate system. If either hemisphere experiences collapse of its circulation, the likelihood of prolonged dry spells and droughts would increase as precipitation decreases, while the other hemisphere will become wetter. Marine ecosystems are then more likely to receive fewer nutrients and experience greater ocean deoxygenation. In the Northern Hemisphere, the collapse of AMOC would lead to substantially lower temperatures in many European countries, while the east coast of North America is predicted to see accelerated sea level rise. The collapse of these circulations is generally accepted to be more than a century away, and may only occur in the event of rapid and high sea-temperature increases. However, these projections are marked by significant uncertainty.[10][11]

## Contents

* 1 History of research
* 2 Structure
* 3 Upwelling
* 4 Effects on global climate
* 4.1 Slowdown or collapse of AMOC
* 4.2 Slowdown or collapse of SMOC
* 5 See also
* 6 References
* 7 Other sources
* 8 External links

## History of research

Effect of temperature and salinity upon sea water density maximum and sea water freezing temperature

It has long been known that wind can drive ocean currents, but only at the surface.[12] In the 19th century, some oceanographers suggested that the convection of heat could drive deeper currents. In 1908, Johan Sandström performed a series of experiments at a Bornö Marine Research Station which proved that the currents driven by thermal energy transfer can exist, but require that "heating occurs at a greater depth than cooling".[1][13] Normally, the opposite occurs, because ocean water is heated from above by the Sun and becomes less dense, so the surface layer floats on the surface above the cooler, denser layers, resulting in ocean stratification. However, wind and tides cause mixing between these water layers, with diapycnal mixing caused by tidal currents being one example.[14] This mixing is what enables the convection between ocean layers, and thus, deep water currents.[1]

In the 1920s, Sandström's framework was expanded by accounting for the role of salinity in ocean layer formation.[1] Salinity is important because like temperature, it affects water density. Water becomes less dense as its temperature increases and the distance between its molecules expands, but more dense as the salinity increases, since there is a larger mass of salts dissolved within that water.[15] Further, while fresh water is at its most dense at 4 °C, seawater only gets denser as it cools, up until it reaches the freezing point. That freezing point is also lower than for fresh water due to salinity, and can be below −2 °C, depending on salinity and pressure.[16]

## Structure

The global conveyor belt on a continuous-ocean map (animation)

These density differences caused by temperature and salinity ultimately separate ocean water into distinct water masses, such as the North Atlantic Deep Water (NADW) and Antarctic Bottom Water (AABW). These two waters are the main drivers of the circulation, which was established in 1960 by Henry Stommel and Arnold B. Arons.[17] They have chemical, temperature and isotopic ratio signatures (such as 231Pa / 230Th ratios) which can be traced, their flow rate calculated, and their age determined. NADW is formed because North Atlantic is a rare place in the ocean where precipitation, which adds fresh water to the ocean and so reduces its salinity, is outweighed by evaporation, in part due to high windiness. When water evaporates, it leaves salt behind, and so the surface waters of the North Atlantic are particularly salty. North Atlantic is also an already cool region, and evaporative cooling reduces water temperature even further. Thus, this water sinks downward in the Norwegian Sea, fills the Arctic Ocean Basin and spills southwards through the Greenland-Scotland-Ridge – crevasses in the submarine sills that connect Greenland, Iceland and Great Britain. It cannot flow towards the Pacific Ocean due to the narrow shallows of the Bering Strait, but it does slowly flow into the deep abyssal plains of the south Atlantic.[18]

In the Southern Ocean, strong katabatic winds blowing from the Antarctic continent onto the ice shelves will blow the newly formed sea ice away, opening polynyas in locations such as Weddell and Ross Seas, off the Adélie Coast and by Cape Darnley. The ocean, no longer protected by sea ice, suffers a brutal and strong cooling (see polynya). Meanwhile, sea ice starts reforming, so the surface waters also get saltier, hence very dense. In fact, the formation of sea ice contributes to an increase in surface seawater salinity; saltier brine is left behind as the sea ice forms around it (pure water preferentially being frozen). Increasing salinity lowers the freezing point of seawater, so cold liquid brine is formed in inclusions within a honeycomb of ice. The brine progressively melts the ice just beneath it, eventually dripping out of the ice matrix and sinking. This process is known as brine rejection. The resulting Antarctic bottom water sinks and flows north and east. It is denser than the NADW, and so flows beneath it. AABW formed in the Weddell Sea will mainly fill the Atlantic and Indian Basins, whereas the AABW formed in the Ross Sea will flow towards the Pacific Ocean. At the Indian Ocean, a vertical exchange of a lower layer of cold and salty water from the Atlantic and the warmer and fresher upper ocean water from the tropical Pacific occurs, in what is known as overturning. In the Pacific Ocean, the rest of the cold and salty water from the Atlantic undergoes haline forcing, and becomes warmer and fresher more quickly.[19][20][21][22][23]

File:Thermohaline conveyor belt (NASA).webm

The out-flowing undersea of cold and salty water makes the sea level of the Atlantic slightly lower than the Pacific and salinity or halinity of water at the Atlantic higher than the Pacific. This generates a large but slow flow of warmer and fresher upper ocean water from the tropical Pacific to the Indian Ocean through the Indonesian Archipelago to replace the cold and salty Antarctic Bottom Water. This is also known as 'haline forcing' (net high latitude freshwater gain and low latitude evaporation). This warmer, fresher water from the Pacific flows up through the South Atlantic to Greenland, where it cools off and undergoes evaporative cooling and sinks to the ocean floor, providing a continuous thermohaline circulation.[25][26]

## Upwelling

As the deep waters sink into the ocean basins, they displace the older deep-water masses, which gradually become less dense due to continued ocean mixing. Thus, some water is rising, in what is known as upwelling. Its speeds are very slow even compared to the movement of the bottom water masses. It is therefore difficult to measure where upwelling occurs using current speeds, given all the other wind-driven processes going on in the surface ocean. Deep waters have their own chemical signature, formed from the breakdown of particulate matter falling into them over the course of their long journey at depth. A number of scientists have tried to use these tracers to infer where the upwelling occurs. Wallace Broecker, using box models, has asserted that the bulk of deep upwelling occurs in the North Pacific, using as evidence the high values of silicon found in these waters. Other investigators have not found such clear evidence.[27]

Computer models of ocean circulation increasingly place most of the deep upwelling in the Southern Ocean, associated with the strong winds in the open latitudes between South America and Antarctica.[28] Direct estimates of the strength of the thermohaline circulation have also been made at 26.5°N in the North Atlantic, by the UK-US RAPID programme. It combines direct estimates of ocean transport using current meters and subsea cable measurements with estimates of the geostrophic current from temperature and salinity measurements to provide continuous, full-depth, basin-wide estimates of the meridional overturning circulation. However, it has only been operating since 2004, which is too short when the timescale of the circulation is measured in centuries.[29]

## Effects on global climate

The thermohaline circulation plays an important role in supplying heat to the polar regions, and thus in regulating the amount of sea ice in these regions, although poleward heat transport outside the tropics is considerably larger in the atmosphere than in the ocean.[30] Changes in the thermohaline circulation are thought to have significant impacts on the Earth's radiation budget.

Large influxes of low-density meltwater from Lake Agassiz and deglaciation in North America are thought to have led to a shifting of deep water formation and subsidence in the extreme North Atlantic and caused the climate period in Europe known as the Younger Dryas.[31]

### Slowdown or collapse of AMOC

Modelled 21st century warming under the "intermediate" global warming scenario (top). The potential collapse of the subpolar gyre in this scenario (middle). The collapse of the entire Atlantic Meridional Overturning Circulation (bottom).

This section is an excerpt from Atlantic meridional overturning circulation#Major review studies[ edit ]

This section is an excerpt from Atlantic meridional overturning circulation#Effects of AMOC slowdown[ edit ]

### Slowdown or collapse of SMOC

This section is an excerpt from Southern Ocean overturning circulation#Climate change impacts[ edit ]

## See also

* Earth:Atlantic multidecadal oscillation - Climate cycle that affects the surface temperature of the North Atlantic
* Earth:Contourite
* Earth:Downwelling
* Earth:Halothermal circulation - Part of world ocean circulation system
* Earth:Hydrothermal circulation - Circulation of water driven by heat exchange

## References

1. ↑ 1.0 1.1 1.2 1.3 Rahmstorf, S (2003). "The concept of the thermohaline circulation". Nature 421 (6924): 699. doi:10.1038/421699a. PMID 12610602. Bibcode: 2003Natur.421..699R. http://www.pik-potsdam.de/~stefan/Publications/Nature/nature_concept_03.pdf.
2. ↑ Lappo, SS (1984). "On reason of the northward heat advection across the Equator in the South Pacific and Atlantic ocean". Study of Ocean and Atmosphere Interaction Processes (Moscow Department of Gidrometeoizdat (in Mandarin)): 125–9.
3. ↑ 3.0 3.1 "What is the global ocean conveyor belt?". NOAA. https://oceanservice.noaa.gov/facts/conveyor.html.
4. ↑ Primeau, F (2005). "Characterizing transport between the surface mixed layer and the ocean interior with a forward and adjoint global ocean transport model". Journal of Physical Oceanography 35 (4): 545–64. doi:10.1175/JPO2699.1. Bibcode: 2005JPO....35..545P. https://escholarship.org/content/qt5f76r4wn/qt5f76r4wn.pdf?t=n3tp5j.
5. ↑ Schwartz, John (20 February 2019). "Wallace Broecker, 87, Dies; Sounded Early Warning on Climate Change" (in en-US). The New York Times. ISSN 0362-4331. https://www.nytimes.com/2019/02/19/obituaries/wallace-broecker-dead.html.
6. ↑ de Menocal, Peter (2019-03-26). "Wallace Smith Broecker (1931–2019)" (in en). Nature 568 (7750): 34. doi:10.1038/d41586-019-00993-2. Bibcode: 2019Natur.568...34D.
7. ↑ Wunsch, C (2002). "What is the thermohaline circulation?". Science 298 (5596): 1179–81. doi:10.1126/science.1079329. PMID 12424356.
8. ↑ Collins, Kevin (3 November 2023). "El Niño may be drying out the southern hemisphere – here's how that affects the whole planet". The Conversation. https://theconversation.com/el-nino-may-be-drying-out-the-southern-hemisphere-heres-how-that-affects-the-whole-planet-216928.
9. ↑ "NOAA Scientists Detect a Reshaping of the Meridional Overturning Circulation in the Southern Ocean". NOAA. 29 March 2023. https://www.aoml.noaa.gov/noaa-scientists-detect-reshaping-of-the-meridional-overturning-circulation-in-southern-ocean/.
10. ↑ 10.0 10.1 Lenton, T. M.; Armstrong McKay, D.I.; Loriani, S.; Abrams, J.F.; Lade, S.J.; Donges, J.F.; Milkoreit, M.; Powell, T. et al. (2023). ﻿The Global Tipping Points Report 2023﻿ (Report). University of Exeter. https://global-tipping-points.org/download/4608/.
11. ↑ Logan, Tyne (29 March 2023). "Landmark study projects 'dramatic' changes to Southern Ocean by 2050". ABC News. https://www.abc.net.au/news/2023-03-30/dramatic-south-ocean-circulation-changes-study/102154690.
12. ↑ Schmidt, Gavin (26 May 2005). "Gulf Stream slowdown?". RealClimate. https://www.realclimate.org/index.php?p=159.
13. ↑ Rahmstorf, S (2006). "Thermohaline Ocean Circulation". in Elias, S. A.. Encyclopedia of Quaternary Sciences. Elsevier Science. ISBN 0-444-52747-8. http://pik-potsdam.de/~stefan/Publications/Book_chapters/rahmstorf_eqs_2006.pdf.
14. ↑ Eden, Carsten (2012). Ocean Dynamics. Springer. pp. 177. ISBN 978-3-642-23449-1. https://archive.org/details/oceandynamics00olbe.
15. ↑ Wyrtki, K (1961). "The thermohaline circulation in relation to the general circulation in the oceans". Deep-Sea Research 8 (1): 39–64. doi:10.1016/0146-6313(61)90014-4. Bibcode: 1961DSR.....8...39W.
16. ↑ Pawlowicz, Rich (2013). "Key Physical Variables in the Ocean: Temperature, Salinity, and Density". Nature Magazine. https://www.nature.com/scitable/knowledge/library/key-physical-variables-in-the-ocean-temperature-102805293/.
17. ↑ Stommel, H., & Arons, A. B. (1960). On the abyssal circulation of the world ocean. – I. Stationary planetary flow patterns on a sphere. Deep Sea Research (1953), 6, 140–154.
18. ↑ Reagan, James; Seidov, Dan; Boyer, Tim (11 June 2018). "Water Vapor Transfer and Near-Surface Salinity Contrasts in the North Atlantic Ocean" (in en). Scientific Reports 8: 8830. doi:10.1038/s41598-018-27052-6. PMID 29891855. Bibcode: 2018NatSR...8.8830R.
19. ↑ Massom, R.; Michael, K.; Harris, P.T.; Potter, M.J. (1998). "The distribution and formative processes of latent heat polynyas in East Antarctica". Annals of Glaciology 27: 420–426. doi:10.3189/1998aog27-1-420-426. Bibcode: 1998AnGla..27..420M.
20. ↑ Tamura, Takeshi; Ohshima, Kay I.; Nihashi, Sohey (April 2008). "Mapping of sea ice production for Antarctic coastal polynyas" (in en). Geophysical Research Letters 35 (7). doi:10.1029/2007GL032903. ISSN 0094-8276. Bibcode: 2008GeoRL..35.7606T. https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2007GL032903.
21. ↑ Morrison, A. K.; Hogg, A. McC.; England, M. H.; Spence, P. (May 2020). "Warm Circumpolar Deep Water transport toward Antarctica driven by local dense water export in canyons" (in en). Science Advances 6 (18). doi:10.1126/sciadv.aav2516. ISSN 2375-2548. PMID 32494658. Bibcode: 2020SciA....6.2516M.
22. ↑ Williams, G. D.; Herraiz-Borreguero, L.; Roquet, F.; Tamura, T.; Ohshima, K. I.; Fukamachi, Y.; Fraser, A. D.; Gao, L. et al. (2016-08-23). "The suppression of Antarctic bottom water formation by melting ice shelves in Prydz Bay" (in en). Nature Communications 7 (1). doi:10.1038/ncomms12577. ISSN 2041-1723. PMID 27552365. Bibcode: 2016NatCo...712577W.
23. ↑ Narayanan, Aditya; Gille, Sarah T.; Mazloff, Matthew R.; du Plessis, Marcel D.; Murali, K.; Roquet, Fabien (June 2023). "Zonal Distribution of Circumpolar Deep Water Transformation Rates and Its Relation to Heat Content on Antarctic Shelves" (in en). Journal of Geophysical Research: Oceans 128 (6). doi:10.1029/2022JC019310. ISSN 2169-9275. Bibcode: 2023JGRC..12819310N. https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2022JC019310.
24. ↑ The Thermohaline Circulation – The Great Ocean Conveyor Belt NASA Scientific Visualization Studio, visualizations by Greg Shirah, 8 October 2009.  This article incorporates text from this source, which is in the public domain.
25. ↑ United Nations Environment Programme / GRID-Arendal, 2006, [1] . Potential Impact of Climate Change
26. ↑ Talley, Lynne (1999). "Some aspects of ocean heat transport by the shallow, intermediate and deep overturning circulations". Mechanisms of Global Climate Change at Millennial Time Scales. Geophysical Monograph Series. 112. pp. 1–22. doi:10.1029/GM112p0001. ISBN 0-87590-095-X. Bibcode: 1999GMS...112....1T.
27. ↑ S., Broecker, Wallace (2010). The great ocean conveyor: discovering the trigger for abrupt climate change. Princeton University Press. ISBN 978-0-691-14354-5. OCLC 695704119.
28. ↑ Marshall, John; Speer, Kevin (26 February 2012). "Closure of the meridional overturning circulation through Southern Ocean upwelling". Nature Geoscience 5 (3): 171–80. doi:10.1038/ngeo1391. Bibcode: 2012NatGe...5..171M. https://zenodo.org/record/889555.
29. ↑ "RAPID: monitoring the Atlantic Meridional Overturning Circulation at 26.5N since 2004". http://www.rapid.ac.uk/rapidmoc/overview.php.
30. ↑ Trenberth, K; Caron, J (2001). "Estimates of Meridional Atmosphere and Ocean Heat Transports". Journal of Climate 14 (16): 3433–43. doi:10.1175/1520-0442(2001)014<3433:EOMAAO>2.0.CO;2. Bibcode: 2001JCli...14.3433T. https://zenodo.org/record/1234671.
31. ↑ Broecker, WS (2006). "Was the Younger Dryas Triggered by a Flood?". Science 312 (5777): 1146–8. doi:10.1126/science.1123253. PMID 16728622.

## Other sources

* Apel, JR (1987). Principles of Ocean Physics. Academic Press. ISBN 0-12-058866-8.
* Gnanadesikan, A.; R. D. Slater; P. S. Swathi; G. K. Vallis (2005). "The energetics of ocean heat transport". Journal of Climate 18 (14): 2604–16. doi:10.1175/JCLI3436.1. Bibcode: 2005JCli...18.2604G.
* Knauss, JA (1996). Introduction to Physical Oceanography. Prentice Hall. ISBN 0-13-238155-9.

## External links

* Ocean Conveyor Belt
* THOR FP7 projects http://arquivo.pt/wayback/20141126093524/http://www.eu-thor.eu/ investigates on the topic "Thermohaline overturning- at risk?" and the predictability of changes of the THC. THOR is financed by the 7th Framework Programme of the European Commission.

* v
* t
* e

Atmospheric, oceanographic, cryospheric, and climate models

Model types

* Atmospheric model
* Oceanographic model
* Cryospheric model
* Climate model
* Numerical weather prediction
* Tropical cyclone forecast model
* Atmospheric dispersion modeling
* Chemical transport model
* Upper-atmospheric models
* Ensemble forecasting
* Model output statistics
* Meteorological reanalysis
* Parametrization

Specific models

| Climate|

* IGCM
* HadCM3
* HadGEM1
* GFDL CM2.X
* CGCM
* CCSM
* CESM
* CFSv2
* ECHAM

|

Global weather|

* IFS (ECMWF)
* FIM
* GEM / GDPS
* FV3 GFS
* MPAS
* NAEFS
* NAVGEM
* UM
* JMA-GSM
* GME / ICON
* ARPEGE

Regional and mesoscale atmospheric|

* NAM
* RR / RAP
* RAMS
* WRF
* RAQMS
* HIRLAM
* LAPS
* RPM
* HWRF

Regional and mesoscale oceanographic|

* HyCOM
* ROMS
* POM
* MOM
* FVCOM
* MITgcm
* FESOM
* ADCIRC

Atmospheric dispersion|

* ADMS
* AERMOD
* ATSTEP
* AUSTAL2000
* CALPUFF
* DISPERSION21
* ISC3
* MEMO
* MERCURE
* NAME
* OSPM
* PUFF-PLUME
* RIMPUFF
* SAFE AIR

Chemical transport|

* CLaMS
* MOZART
* GEOS-Chem

Land surface parametrization|

* JULES
* CLASS
* ISBA

Cryospheric models|

* CICE

Discontinued|

* AVN / MRF / GSM / GFS
* Eta
* LFM
* MM5
* NGM
* NOGAPS
* RUC

* Mathematical model
* Statistical model
* Scientific modelling
* Computer simulation

* v
* t
* e

Ocean currents and gyres

Currents|

| Arctic Ocean|

* East Greenland
* North Icelandic
* Norwegian
* Transpolar Drift Stream

|

Atlantic Ocean|

* Angola
* Antilles
* Azores
* Baffin Island
* Benguela
* Brazil
* Canary
* Cape Horn
* Caribbean
* East Greenland
* East Iceland
* Falkland
* Florida
* Guinea
* Gulf Stream
* Irminger
* Labrador
* Lomonosov
* Loop
* North Atlantic
* North Brazil
* North Equatorial
* Norwegian
* Portugal
* Slope Jet
* South Atlantic
* South Equatorial
* West Greenland
* West Spitsbergen

Indian Ocean|

* Agulhas
* Agulhas Return
* East Madagascar
* Equatorial Counter
* Indian Monsoon
* Indonesian Throughflow
* Leeuwin
* Madagascar
* Mozambique
* North Madagascar
* Somali
* South Australian
* South Equatorial
* West Australian

Pacific Ocean|

* Alaska
* Aleutian
* California
* Cromwell
* Davidson
* East Australian
* East Korea Warm
* Equatorial Counter
* Humboldt
* Indonesian Throughflow
* Kamchatka
* Kuroshio
* Mindanao
* North Equatorial
* North Korea Cold
* North Pacific
* Oyashio
* South Equatorial
* Tasman Front

Southern Ocean|

* Antarctic Circumpolar
* Tasman Outflow

Gyres|

| Major gyres|

* Indian Ocean Gyre
* North Atlantic Gyre
* South Atlantic Gyre
* North Pacific Gyre
* South Pacific Gyre

|

Other gyres|

* Beaufort Gyre
* Ross Gyre
* Weddell Gyre

Related|

* Atmospheric circulation
* Boundary current
* Coriolis force
* Ekman transport
* Marine debris
* Marine garbage patches
* Great Pacific
* Indian Ocean
* North Atlantic
* South Pacific
* Thermohaline circulation

* v
* t
* e

Physical oceanography

Waves|

* Airy wave theory
* Ballantine scale
* Benjamin–Feir instability
* Boussinesq approximation
* Breaking wave
* Clapotis
* Cnoidal wave
* Cross sea
* Dispersion
* Edge wave
* Equatorial waves
* Fetch
* Gravity wave
* Green's law
* Infragravity wave
* Internal wave
* Iribarren number
* Kelvin wave
* Kinematic wave
* Longshore drift
* Luke's variational principle
* Mild-slope equation
* Radiation stress
* Rogue wave
* Rossby wave
* Rossby-gravity waves
* Sea state
* Seiche
* Significant wave height
* Soliton
* Stokes boundary layer
* Stokes drift
* Stokes wave
* Swell
* Trochoidal wave
* Tsunami
* megatsunami
* Undertow
* Ursell number
* Wave action
* Wave base
* Wave height
* Wave power
* Wave radar
* Wave setup
* Wave shoaling
* Wave turbulence
* Wave–current interaction
* Waves and shallow water
* one-dimensional Saint-Venant equations
* shallow water equations
* Wind wave
* model

Circulation|

* Atmospheric circulation
* Baroclinity
* Boundary current
* Coriolis force
* Coriolis–Stokes force
* Craik–Leibovich vortex force
* Downwelling
* Eddy
* Ekman layer
* Ekman spiral
* Ekman transport
* El Niño–Southern Oscillation
* General circulation model
* Geochemical Ocean Sections Study
* Geostrophic current
* Global Ocean Data Analysis Project
* Gulf Stream
* Halothermal circulation
* Humboldt Current
* Hydrothermal circulation
* Langmuir circulation
* Longshore drift
* Loop Current
* Modular Ocean Model
* Ocean dynamics
* Ocean gyre
* Princeton ocean model
* Rip current
* Subsurface currents
* Sverdrup balance
* Thermohaline circulation
* shutdown
* Upwelling
* Whirlpool
* World Ocean Circulation Experiment

Tides|

* Amphidromic point
* Earth tide
* Head of tide
* Internal tide
* Lunitidal interval
* Perigean spring tide
* Rip tide
* Rule of twelfths
* Slack water
* Tidal bore
* Tidal force
* Tidal power
* Tidal race
* Tidal range
* Tidal resonance
* Tide gauge
* Tideline
* Theory of tides

Landforms|

* Abyssal fan
* Abyssal plain
* Atoll
* Bathymetric chart
* Coastal geography
* Cold seep
* Continental margin
* Continental rise
* Continental shelf
* Contourite
* Guyot
* Hydrography
* Oceanic basin
* Oceanic plateau
* Oceanic trench
* Passive margin
* Seabed
* Seamount
* Submarine canyon
* Submarine volcano

Plate
tectonics|

* Convergent boundary
* Divergent boundary
* Fracture zone
* Hydrothermal vent
* Marine geology
* Mid-ocean ridge
* Mohorovičić discontinuity
* Vine–Matthews–Morley hypothesis
* Oceanic crust
* Outer trench swell
* Ridge push
* Seafloor spreading
* Slab pull
* Slab suction
* Slab window
* Subduction
* Transform fault
* Volcanic arc

Ocean zones|

* Benthic
* Deep ocean water
* Deep sea
* Littoral
* Mesopelagic
* Oceanic
* Pelagic
* Photic
* Surf
* Swash

Sea level|

* Deep-ocean Assessment and Reporting of Tsunamis
* Future sea level
* Global Sea Level Observing System
* North West Shelf Operational Oceanographic System
* Sea-level curve
* Sea level rise
* World Geodetic System

Acoustics|

* Deep scattering layer
* Hydroacoustics
* Ocean acoustic tomography
* Sofar bomb
* SOFAR channel
* Underwater acoustics

Satellites|

* Jason-1
* Jason-2 (Ocean Surface Topography Mission)
* Jason-3

Related|

* Argo
* Benthic lander
* Color of water
* DSV Alvin
* Marginal sea
* Marine energy
* Marine pollution
* Mooring
* National Oceanographic Data Center
* Ocean
* Ocean exploration
* Ocean observations
* Ocean reanalysis
* Ocean surface topography
* Ocean thermal energy conversion
* Oceanography
* Pelagic sediment
* Sea surface microlayer
* Sea surface temperature
* Seawater
* Science On a Sphere
* Thermocline
* Underwater glider
* Water column
* World Ocean Atlas

* Category
* Commons

0.00

(0 votes)

Original source: https://en.wikipedia.org/wiki/Thermohaline circulation. Read more

|

Retrieved from "https://handwiki.org/wiki/index.php?title=Earth:Thermohaline_circulation&oldid=4162416"
*[v]: View this template
*[t]: Discuss this template
*[e]: Edit this template