The ocean (also the sea or the world ocean) is the body of salt water which covers approximately 71% of the surface of the Earth. It is also "any of the large bodies of water into which the great ocean is divided". These five oceans are, in descending order by area, the Pacific, Atlantic, Indian, Southern (Antarctic), and Arctic Oceans.
Saline seawater covers approximately 361,000,000 km2 (139,000,000 sq mi) and is customarily divided into several principal oceans and smaller seas, with the ocean as a whole covering approximately 71% of Earth's surface and 90% of the Earth's biosphere. The oceans contains 97% of Earth's water, and oceanographers have stated that less than 20% of the oceans have been mapped. The total volume is approximately 1.35 billion cubic kilometers (320 million cu mi) with an average depth of nearly 3,700 meters (12,100 ft).
As the world's ocean is the principal component of Earth's hydrosphere, it is integral to life, forms part of the carbon cycle, and influences climate and weather patterns. The ocean is the habitat of 230,000 known species, but because much of it is unexplored, the number of species in the ocean is much larger, possibly over two million. The origin of Earth's oceans is unknown; oceans are thought to have formed in the Hadean eon and may have been the cause for the emergence of life.
Extraterrestrial oceans may be composed of water or other elements and compounds. The only confirmed large stable bodies of extraterrestrial surface liquids are the lakes of Titan, although there is evidence for oceans' existence elsewhere in the Solar System.
The phrases "the ocean" or "the sea" used without specification refer to the interconnected body of salt water covering the majority of the Earth's surface. it includes the Atlantic, Pacific, Indian, Southern and Arctic Oceans. As a general term, "the ocean" is mostly interchangeable with "the sea" in American English, but not in British English. Strictly speaking, a sea is a body of water (generally a division of the world ocean) partly or fully enclosed by land. The word "sea" can also be used for many specific, much smaller bodies of seawater, such as the North Sea or the Red Sea. There is no sharp distinction between seas and oceans, though generally seas are smaller, and are often partly (as marginal seas) or wholly (as inland seas) bordered by land.
The global, interconnected body of salt water is sometimes referred to as the "World Ocean" or global ocean. The concept of a continuous body of water with relatively free interchange among its parts is of fundamental importance to oceanography. The contemporary concept of the World Ocean was coined in the early 20th century by the Russian oceanographer Yuly Shokalsky to refer to the continuous ocean that covers and encircles most of Earth. Plate tectonics, post-glacial rebound, and sea level rise continually change the coastline and structure of the world ocean. That said a global ocean has existed in one form or another on Earth for eons.
The word ocean comes from the figure in classical antiquity, Oceanus (//; Greek: Ὠκεανός Ōkeanós, pronounced [ɔːkeanós]), the elder of the Titans in classical Greek mythology, believed by the ancient Greeks and Romans to be the divine personification of an enormous river encircling the world.
The concept of Ōkeanós has an Indo-European connection. Greek Ōkeanós has been compared to the Vedic epithet ā-śáyāna-, predicated of the dragon Vṛtra-, who captured the cows/rivers. Related to this notion, the Okeanos is represented with a dragon-tail on some early Greek vases.
|1||Pacific Ocean||Separates Asia and Australasia from the Americas||168,723,000
|2||Atlantic Ocean||Separates the Americas from Europe and Africa||85,133,000
|3||Indian Ocean||Borders southern Asia and separates Africa and Australia||70,560,000
|4||Southern Ocean||Encircles Antarctica. Sometimes considered an extension of the Pacific, Atlantic and Indian Oceans,||21,960,000
|5||Arctic Ocean||Borders northern North America and Eurasia and covers much of the Arctic. Sometimes considered a sea or estuary of the Atlantic. ||15,558,000
Sources: Encyclopedia of Earth, International Hydrographic Organization, Regional Oceanography: an Introduction (Tomczak, 2005), Encyclopædia Britannica, and the International Telecommunication Union.
The mid-ocean ridges of the world are connected and form a single global mid-oceanic ridge system that is part of every ocean and the longest mountain range in the world. The continuous mountain range is 65,000 km (40,000 mi) long (several times longer than the Andes, the longest continental mountain range).
The total mass of the hydrosphere is about 1.4 quintillion tonnes (1.4×1018 long tons or 1.5×1018 short tons), which is about 0.023% of Earth's total mass. Less than 3% is freshwater; the rest is saltwater, almost all of which is in the ocean. The area of the World Ocean is about 361.9 million square kilometers (139.7 million square miles), which covers about 70.9% of Earth's surface, and its volume is approximately 1.335 billion cubic kilometers (320.3 million cubic miles). This can be thought of as a cube of water with an edge length of 1,101 kilometers (684 mi). Its average depth is about 3,688 meters (12,100 ft), and its maximum depth is 10,994 meters (6.831 mi) at the Mariana Trench. Nearly half of the world's marine waters are over 3,000 meters (9,800 ft) deep. The vast expanses of deep ocean (anything below 200 meters or 660 feet) cover about 66% of Earth's surface. This does not include seas not connected to the World Ocean, such as the Caspian Sea.
The bluish ocean color is a composite of several contributing agents. Prominent contributors include dissolved organic matter and chlorophyll. Mariners and other seafarers have reported that the ocean often emits a visible glow which extends for miles at night. In 2005, scientists announced that for the first time, they had obtained photographic evidence of this glow. It is most likely caused by bioluminescence.
Oceanographers divide the ocean into different vertical zones defined by physical and biological conditions. The pelagic zone includes all open ocean regions, and can be divided into further regions categorized by depth and light abundance. The photic zone includes the oceans from the surface to a depth of 200 m; it is the region where photosynthesis can occur and is, therefore, the most biodiverse. Because plants require photosynthesis, life found deeper than the photic zone must either rely on material sinking from above (see marine snow) or find another energy source. Hydrothermal vents are the primary source of energy in what is known as the aphotic zone (depths exceeding 200 m). The pelagic part of the photic zone is known as the epipelagic.
The pelagic part of the aphotic zone can be further divided into vertical regions according to temperature. The mesopelagic is the uppermost region. Its lowermost boundary is at a thermocline of 12 °C (54 °F), which, in the tropics generally lies at 700–1,000 meters (2,300–3,300 ft). Next is the bathypelagic lying between 10 and 4 °C (50 and 39 °F), typically between 700–1,000 meters (2,300–3,300 ft) and 2,000–4,000 meters (6,600–13,100 ft), lying along the top of the abyssal plain is the abyssopelagic, whose lower boundary lies at about 6,000 meters (20,000 ft). The last zone includes the deep oceanic trench, and is known as the hadalpelagic. This lies between 6,000–11,000 meters (20,000–36,000 ft) and is the deepest oceanic zone.
The benthic zones are aphotic and correspond to the three deepest zones of the deep-sea. The bathyal zone covers the continental slope down to about 4,000 meters (13,000 ft). The abyssal zone covers the abyssal plains between 4,000 and 6,000 m. Lastly, the hadal zone corresponds to the hadalpelagic zone, which is found in oceanic trenches.
The pelagic zone can be further subdivided into two sub regions: the neritic zone and the oceanic zone. The neritic zone encompasses the water mass directly above the continental shelves whereas the oceanic zone includes all the completely open water.
In contrast, the littoral zone covers the region between low and high tide and represents the transitional area between marine and terrestrial conditions. It is also known as the intertidal zone because it is the area where tide level affects the conditions of the region.
If a zone undergoes dramatic changes in temperature with depth, it contains a thermocline. The tropical thermocline is typically deeper than the thermocline at higher latitudes. Polar waters, which receive relatively little solar energy, are not stratified by temperature and generally lack a thermocline because surface water at polar latitudes are nearly as cold as water at greater depths. Below the thermocline, water is very cold, ranging from −1 °C to 3 °C. Because this deep and cold layer contains the bulk of ocean water, the average temperature of the world ocean is 3.9 °C.  If a zone undergoes dramatic changes in salinity with depth, it contains a halocline. If a zone undergoes a strong, vertical chemistry gradient with depth, it contains a chemocline.
The halocline often coincides with the thermocline, and the combination produces a pronounced pycnocline.
The deepest point in the ocean is the Mariana Trench, located in the Pacific Ocean near the Northern Mariana Islands. Its maximum depth has been estimated to be 10,971 meters (35,994 ft) (plus or minus 11 meters; see the Mariana Trench article for discussion of the various estimates of the maximum depth.) The British naval vessel Challenger II surveyed the trench in 1951 and named the deepest part of the trench the "Challenger Deep". In 1960, the Trieste successfully reached the bottom of the trench, manned by a crew of two men.
Ocean currents have different origins. Tidal currents are in phase with the tide, hence are quasiperiodic; they may form various knots in certain places, most notably around headlands. Non-periodic currents have for origin the waves, wind and different densities.
The wind and waves create surface currents (designated as "drift currents"). These currents can decompose in one quasi-permanent current (which varies within the hourly scale) and one movement of Stokes drift under the effect of rapid waves movement (at the echelon of a couple of seconds).). The quasi-permanent current is accelerated by the breaking of waves, and in a lesser governing effect, by the friction of the wind on the surface.
This acceleration of the current takes place in the direction of waves and dominant wind. Accordingly, when the sea depth increases, the rotation of the earth changes the direction of currents in proportion with the increase of depth, while friction lowers their speed. At a certain sea depth, the current changes direction and is seen inverted in the opposite direction with current speed becoming null: known as the Ekman spiral. The influence of these currents is mainly experienced at the mixed layer of the ocean surface, often from 400 to 800 meters of maximum depth. These currents can considerably alter, change and are dependent on the various yearly seasons. If the mixed layer is less thick (10 to 20 meters), the quasi-permanent current at the surface adopts an extreme oblique direction in relation to the direction of the wind, becoming virtually homogeneous, until the Thermocline.
Ocean currents greatly affect Earth's climate by transferring heat from the tropics to the polar regions. Transferring warm or cold air and precipitation to coastal regions, winds may carry them inland. Surface heat and freshwater fluxes create global density gradients that drive the thermohaline circulation part of large-scale ocean circulation. It plays an important role in supplying heat to the polar regions, and thus in sea ice regulation. Changes in the thermohaline circulation are thought to have significant impacts on Earth's energy budget. In so far as the thermohaline circulation governs the rate at which deep waters reach the surface, it may also significantly influence atmospheric carbon dioxide concentrations.
The Antarctic Circumpolar Current encircles that continent, influencing the area's climate and connecting currents in several oceans.
Oceans have a significant effect on the biosphere. Oceanic evaporation, as a phase of the water cycle, is the source of most rainfall, and ocean temperatures determine climate and wind patterns that affect life on land. Life within the ocean evolved 3 billion years prior to life on land. Both the depth and the distance from shore strongly influence the biodiversity of the plants and animals present in each region.
As it is thought that life evolved in the ocean, the diversity of life is immense, including:
- Bacteria : ubiquitous single-celled prokaryotes found throughout the world
- Archaea : prokaryotes distinct from bacteria, that inhabit many environments of the ocean, as well as many extreme environments
- Algae : algae is a "catch-all" term to include many photosynthetic, single-celled eukaryotes, such as green algae, diatoms, and dinoflagellates, but also multicellular algae, such as some red algae (including organisms like Pyropia, which is the source of the edible nori seaweed), and brown algae (including organisms like kelp).
- Plants : including sea grasses, or mangroves
- Fungi : many marine fungi with diverse roles are found in oceanic environments
- Animals : most animal phyla have species that inhabit the ocean, including many that are only found in marine environments such as sponges, Cnidaria (such as corals and jellyfish), comb jellies, Brachiopods, and Echinoderms (such as sea urchins and sea stars). Many other familiar animal groups primarily live in the ocean, including cephalopods (includes octopus and squid), crustaceans (includes lobsters, crabs, and shrimp), fish, sharks, cetaceans (includes whales, dolphins, and porpoises).
In addition, many land animals have adapted to living a major part of their life on the oceans. For instance, seabirds are a diverse group of birds that have adapted to a life mainly on the oceans. They feed on marine animals and spend most of their lifetime on water, many only going on land for breeding. Other birds that have adapted to oceans as their living space are penguins, seagulls and pelicans. Seven species of turtles, the sea turtles, also spend most of their time in the oceans.
|Gas||Concentration of seawater, by mass (in parts per million), for the whole ocean||% dissolved gas, by volume, in seawater at the ocean surface|
|Carbon dioxide (CO2)||64 to 107||15%|
|Nitrogen (N2)||10 to 18||48%|
|Oxygen (O2)||0 to 13||36%|
|Characteristic||Oceanic waters in polar regions||Oceanic waters in temperate regions||Oceanic waters in tropical regions|
|Precipitation vs. evaporation||P > E||P > E||E > P|
|Sea surface temperature in winter||−2 °C||5 to 20 °C||20 to 25 °C|
|Average salinity||28‰ to 32‰||35‰||35‰ to 37‰|
|Annual variation of air temperature||≤ 40ªC||10 °C||< 5 °C|
|Annual variation of water temperature||< 5ªC||10 °C||< 5 °C|
|Constituent||Residence time (in years)|
A zone of rapid salinity increase with depth is called a halocline. The temperature of maximum density of seawater decreases as its salt content increases. Freezing temperature of water decreases with salinity, and boiling temperature of water increases with salinity. Typical seawater freezes at around −2 °C at atmospheric pressure. If precipitation exceeds evaporation, as is the case in polar and temperate regions, salinity will be lower. If evaporation exceeds precipitation, as is the case in tropical regions, salinity will be higher. Thus, oceanic waters in polar regions have lower salinity content than oceanic waters in temperate and tropical regions.
Salinity can be calculated using the chlorinity, which is a measure of the total mass of halogen ions (includes fluorine, chlorine, bromine, and iodine) in seawater. By international agreement, the following formula is used to determine salinity:
- Salinity (in ‰) = 1.80655 × Chlorinity (in ‰)
The average chlorinity is about 19.2‰, and, thus, the average salinity is around 34.7‰ 
Absorption of light
|Color (wavelength in nm)||Depth at which 99 percent of the wavelength is absorbed (in meters)||Percent absorbed in 1 meter of water|
Waves and swell
The motions of the ocean surface, known as undulations or waves, are the partial and alternate rising and falling of the ocean surface. The series of mechanical waves that propagate along the interface between water and air is called swell.
Human uses of the oceans
Humans have been using the ocean for a variety of purposes, for example navigation, exploration, war, travel, trade, food, leisure, power generation, extractive industries.
Many of the world's goods are moved by ship between the world's seaports. Oceans are also the major supply source for the fishing industry. Some of the major harvests are shrimp, fish, crabs, and lobster.
Human activities affect marine life and marine habitats through overfishing, habitat loss, the introduction of invasive species, ocean pollution, ocean acidification and ocean warming. These impact marine ecosystems and food webs and may result in consequences as yet unrecognized for the biodiversity and continuation of marine life forms.
2) from the atmosphere. The main cause of ocean acidification is the burning of fossil fuels. Seawater is slightly basic (meaning pH > 7), and ocean acidification involves a shift towards pH-neutral conditions rather than a transition to acidic conditions (pH < 7). The issue of ocean acidification is the decreased production of the shells of shellfish and other aquatic life with calcium carbonate shells. The calcium carbonate shells can not reproduce under high saturated acidotic waters. An estimated 30–40% of the carbon dioxide from human activity released into the atmosphere dissolves into oceans, rivers and lakes. Some of it reacts with the water to form carbonic acid. Some of the resulting carbonic acid molecules dissociate into a bicarbonate ion and a hydrogen ion, thus increasing ocean acidity (H+ ion concentration). Between 1751 and 1996, surface ocean pH is estimated to have decreased from approximately 8.25 to 8.14, representing an increase of almost 30% in H+ ion concentration in the world's oceans. Earth System Models project that, by around 2008, ocean acidity exceeded historical analogues and, in combination with other ocean biogeochemical changes, could undermine the functioning of marine ecosystems and disrupt the provision of many goods and services associated with the ocean beginning as early as 2100.
Other effects of climate change on oceans
Although Earth is the only known planet with large stable bodies of liquid water on its surface and the only one in the Solar System, other celestial bodies are thought to have large oceans. In June 2020, NASA scientists reported that it is likely that exoplanets with oceans may be common in the Milky Way galaxy, based on mathematical modeling studies.
- Blue carbon
- Brackish water
- European Atlas of the Seas
- Four Seas
- International Maritime Organization
- List of bodies of water by salinity
- List of oceans with alternative names
- List of seas
- Ocean general circulation model
- Ocean governance
- Panthalassa – Prehistoric superocean that surrounded Pangaea
- Polar seas
- Sea ice
- Sea in culture
- Sea state
- Seven Seas
- Superocean – An ocean that surrounds a supercontinent
- United Nations Convention on the Law of the Sea
- Water distribution on Earth
- Water hemisphere
- Wind wave
- World Oceans Day
- World Ocean Atlas – A data product of the Ocean Climate Laboratory of the National Oceanographic Data Center (U.S.)
- "Ocean." Merriam-Webster.com Dictionary, Merriam-Webster, https://www.merriam-webster.com/dictionary/ocean. Accessed March 14, 2021.
- "ocean, n". Oxford English Dictionary. Retrieved February 5, 2012.
- "ocean". Merriam-Webster. Retrieved February 6, 2012.
- "NOAA – National Oceanic and Atmospheric Administration – Ocean". Noaa.gov. Retrieved February 16, 2020.
- Qadri, Syed (2003). "Volume of Earth's Oceans". The Physics Factbook. Retrieved June 7, 2007.
- Charette, Matthew; Smith, Walter H. F. (2010). "The volume of Earth's ocean". Oceanography. 23 (2): 112–114. doi:10.5670/oceanog.2010.51. Retrieved September 27, 2012.
- "Volumes of the World's Oceans from ETOPO1". NOAA. Archived from the original on March 11, 2015. Retrieved March 7, 2015.CS1 maint: bot: original URL status unknown (link)
- Drogin, Bob (August 2, 2009). "Mapping an ocean of species". Los Angeles Times. Retrieved August 18, 2009.
- "Sea". Merriam-webster.com. Retrieved March 13, 2013.
- Bromhead, Helen, Landscape and Culture – Cross-linguistic Perspectives, p. 92, John Benjamins Publishing Company, 2018, ISBN 9027264007, 9789027264008; unlike Americans, speakers of British English do not go swimming in "the ocean" but always "the sea".
- "WordNet Search — sea". Princeton University. Retrieved February 21, 2012.
- "What's the difference between an ocean and a sea?". Ocean facts. National Oceanic and Atmospheric Administration. Retrieved April 19, 2013.
- "Ocean". Sciencedaily.com. Retrieved November 8, 2012.
- ""Distribution of land and water on the planet". UN Atlas of the Oceans. Archived from the original on March 3, 2016.
- Spilhaus, Athelstan F. (July 1942). "Maps of the whole world ocean". Geographical Review. 32 (3): 431–5. doi:10.2307/210385. JSTOR 210385.
- Bruckner, Lynne and Dan Brayton (2011). Ecocritical Shakespeare (Literary and Scientific Cultures of Early Modernity). Ashgate Publishing, Ltd. ISBN 978-0754669197.
- Ὠκεανός, Henry George Liddell, Robert Scott, A Greek-English Lexicon, at Perseus project
- Matasović, Ranko, A Reader in Comparative Indo-European Religion Zagreb: Univ of Zagreb, 2016. p. 20.
- "Ocean-bearing Planets: Looking For Extraterrestrial Life In All The Right Places". Sciencedaily.com. Retrieved November 8, 2012.
- "CIA World Factbook". CIA. Retrieved April 5, 2015.
- Charette, Matthew; Smith, Walter H. F. (2010). "The volume of Earth's ocean". Oceanography. 23 (2): 112–114. doi:10.5670/oceanog.2010.51. Retrieved January 13, 2014.
- World The World Factbook, CIA. Retrieved January 13, 2014.
- "Pacific Ocean". Encyclopedia of Earth. Retrieved March 7, 2015.
- "Atlantic Ocean". Encyclopedia of Earth. Retrieved March 7, 2015.
- "Indian Ocean". Encyclopedia of Earth. Retrieved March 7, 2015.
- "Southern Ocean". Encyclopedia of Earth. Retrieved March 10, 2015.
- "Limits of Oceans and Seas, 3rd edition" (PDF). International Hydrographic Organization. 1953. Archived from the original (PDF) on October 8, 2011. Retrieved December 28, 2020.
- Tomczak, Matthias; Godfrey, J. Stuart (2003). Regional Oceanography: an Introduction (2 ed.). Delhi: Daya Publishing House. ISBN 978-81-7035-306-5. Archived from the original on June 30, 2007. Retrieved April 10, 2006.
- Ostenso, Ned Allen. "Arctic Ocean". Encyclopædia Britannica. Retrieved July 2, 2012.
As an approximation, the Arctic Ocean may be regarded as an estuary of the Atlantic Ocean.
- "Arctic Ocean". Encyclopedia of Earth. Retrieved March 7, 2015.
- "Recommendation ITU-R RS.1624: Sharing between the Earth exploration-satellite (passive) and airborne altimeters in the aeronautical radionavigation service in the band 4 200–4 400 MHz (Question ITU-R 229/7)" (PDF). ITU Radiotelecommunication Sector (ITU-R). Retrieved April 5, 2015.
The oceans occupy about 3.35×108 km2 of area. There are 377412 km of oceanic coastlines in the world.
- "What is the longest mountain range on earth?". National Ocean Service. US Department of Commerce. Retrieved October 17, 2014.
- "Scientists map Mariana Trench, deepest known section of ocean in the world". The Telegraph. Telegraph Media Group. December 7, 2011. Retrieved March 23, 2012.
- Drazen, Jeffrey C. "Deep-Sea Fishes". School of Ocean and Earth Science and Technology, the University of Hawai'i at Mānoa. Archived from the original on May 24, 2012. Retrieved June 7, 2007.
- Coble, Paula G. (2007). "Marine Optical Biogeochemistry: The Chemistry of Ocean Color". Chemical Reviews. 107 (2): 402–418. doi:10.1021/cr050350+. PMID 17256912.
- Britt, Robert Roy (October 4, 2005). "Mystery Ocean Glow Confirmed in Satellite Photos".
- Holladay, April (November 21, 2005). "A glowing sea, courtesy of algae". USA Today.
- "Sea's eerie glow seen from space". New Scientist. October 5, 2005.
- Casey, Amy (August 8, 2003). "The Incredible Glowing Algae". NASA Earth Observatory. NASA.
- "What is a thermocline?". National Ocean Service. US Department of Commerce. Retrieved February 7, 2021.
- "Tidal Currents - Currents: NOAA's National Ocean Service Education". National Ocean Service. US Department of Commerce. Retrieved February 7, 2021.
- Étude de la dérive à la surface sous l’effet du vent, Observation and estimation of Lagrangian, Stokes and Eulerian currents induced by wind and waves at the sea surface, F. Ardhuin, L. Marié, N. Rascle, P. Forget, and A. Roland, 2009: J. Phys. Oceanogr., vol. 39, n° 11, pp. 2820–2838.
- Mesure de l'effet de frottement à la surface de la mer, "Tangential stress beneath wind-driven air-water interfaces", M. L. Banner and W. L. Peirson, J. Fluid Mech., vol. 364, pp. 115–145, 1998.
- Courants mesurés près de la surface, The drift current from observations made on the bouee laboratoire, Joseph Gonella, 1971: Cahiers Océanographiques, vol. 23, pp. 1–15.
- "Chapter 34: The Biosphere: An Introduction to Earth's Diverse Environment". Biology: Concepts & Connections. section 34.7.
- "Dissolved Gases other than Carbon Dioxide in Seawater" (PDF). soest.hawaii.edu. Retrieved May 5, 2014.
- "Dissolved Oxygen and Carbon Dioxide" (PDF). chem.uiuc.edu.
- "12.742. Marine Chemistry. Lecture 8. Dissolved Gases and Air-sea exchange" (PDF). Retrieved May 5, 2014.
- "5.6 Synthesis – AR4 WGI Chapter 5: Observations: Oceanic Climate Change and Sea Level". Ipcc.ch. Retrieved May 5, 2014.
- "Evaporation minus precipitation, Latitude-Longitude, Annual mean". ERA-40 Atlas. ECMWF. Archived from the original on February 2, 2014.
- Barry, Roger Graham; Chorley, Richard J. (2003). Atmosphere, Weather, and Climate. Routledge. p. 68.
- "Ocean Stratification". Eesc.columbia.edu. Retrieved May 5, 2014.
- Huang, Rui Xin (2010). Ocean Circulation: Wind-Driven and Thermohaline Processes. Cambridge University Press.
- Deser, C.; Alexander, M. A.; Xie, S. P.; Phillips, A. S. (2010). "Sea Surface Temperature Variability: Patterns and Mechanisms" (PDF). Annual Review of Marine Science. 2: 115–43. Bibcode:2010ARMS....2..115D. doi:10.1146/annurev-marine-120408-151453. PMID 21141660. Archived from the original (PDF) on May 14, 2014.
- "Chapter 6 – Temperature, Salinity, and Density – Geographical Distribution of Surface Temperature and Salinity". Introduction to Physical Oceanography. Oceanworld.tamu.edu. March 23, 2009. Retrieved May 5, 2014.
- "Calculation of residence times in seawater of some important solutes" (PDF). gly.uga.edu.
- Chester, Roy; Jickells, Tim (2012). Marine Geochemistry. Blackwell Publishing. pp. 225–230. ISBN 978-1-118-34907-6.
- "Can the ocean freeze? Ocean water freezes at a lower temperature than freshwater". NOAA. Retrieved January 2, 2019.
- Chester, Roy; Jickells, Tim (2012). Marine Geochemistry. Blackwell Publishing. ISBN 978-1-118-34907-6.
- Zacharias, Mark (March 14, 2014). Marine Policy: An Introduction to Governance and International Law of the Oceans. Routledge. ISBN 9781136212475.
- Halpern, B.S.; Frazier, M.; Afflerbach, J.; et al. (2019). "Recent pace of change in human impact on the world's ocean". Scientific Reports. 9 (1): 11609. Bibcode:2019NatSR...911609H. doi:10.1038/s41598-019-47201-9. PMC 6691109. PMID 31406130.
- Human impacts on marine ecosystems GEOMAR Helmholtz Centre for Ocean Research. Retrieved October 22, 2019.
- Duce, Robert, Galloway, J. and Liss, P. (2009). "The Impacts of Atmospheric Deposition to the Ocean on Marine Ecosystems and Climate WMO Bulletin Vol 58 (1)". Retrieved September 22, 2020.
- "What is the biggest source of pollution in the ocean?". National Ocean Service.
- The State of World Fisheries and Aquaculture 2018; Meeting the sustainable development goals (PDF). Rome: FAO. 2018. p. 40. ISBN 978-92-5-130562-1. Retrieved December 29, 2019.
- Caldeira, K.; Wickett, M. E. (2003). "Anthropogenic carbon and ocean pH". Nature. 425 (6956): 365. Bibcode:2001AGUFMOS11C0385C. doi:10.1038/425365a. PMID 14508477. S2CID 4417880.
- The ocean would not become acidic even if it were to absorb the CO2 produced from the combustion of all fossil fuel resources.
- Millero, Frank J. (1995). "Thermodynamics of the carbon dioxide system in the oceans". Geochimica et Cosmochimica Acta. 59 (4): 661–677. Bibcode:1995GeCoA..59..661M. doi:10.1016/0016-7037(94)00354-O.
- Feely, R. A.; Sabine, C. L.; Lee, K.; Berelson, W.; Kleypas, J.; Fabry, V. J.; Millero, F. J. (July 2004). "Impact of Anthropogenic CO2 on the CaCO3 System in the Oceans". Science. 305 (5682): 362–366. Bibcode:2004Sci...305..362F. doi:10.1126/science.1097329. PMID 15256664. S2CID 31054160. Retrieved January 25, 2014 – via Pacific Marine Environmental Laboratory (PMEL).
- Jacobson, M. Z. (2005). "Studying ocean acidification with conservative, stable numerical schemes for nonequilibrium air-ocean exchange and ocean equilibrium chemistry". Journal of Geophysical Research: Atmospheres. 110: D07302. Bibcode:2005JGRD..11007302J. doi:10.1029/2004JD005220.
- Hall-Spencer, J. M.; Rodolfo-Metalpa, R.; Martin, S.; et al. (July 2008). "Volcanic carbon dioxide vents show ecosystem effects of ocean acidification". Nature. 454 (7200): 96–9. Bibcode:2008Natur.454...96H. doi:10.1038/nature07051. hdl:10026.1/1345. PMID 18536730. S2CID 9375062.
- "Report of the Ocean Acidification and Oxygen Working Group, International Council for Science's Scientific Committee on Ocean Research (SCOR) Biological Observatories Workshop" (PDF).
- Mora, C (2013). "The projected timing of climate departure from recent variability". Nature. 502 (7470): 183–187. Bibcode:2013Natur.502..183M. doi:10.1038/nature12540. PMID 24108050. S2CID 4471413.
Global mean ocean pH moved outside its historical variability by 2008 (±3 years s.d.), regardless of the emissions scenario analysed
- Mora, C.; et al. (2013). "Biotic and Human Vulnerability to Projected Changes in Ocean Biogeochemistry over the 21st Century". PLOS Biology. 11 (10): e1001682. doi:10.1371/journal.pbio.1001682. PMC 3797030. PMID 24143135.
- Where's the heat? In the oceans! April 11, 2013 USA Today
- Mora, C.; et al. (2013). "Biotic and Human Vulnerability to Projected Changes in Ocean Biogeochemistry over the 21st Century". PLOS Biology. 11 (10): e1001682. doi:10.1371/journal.pbio.1001682. PMC 3797030. PMID 24143135.
- Dyches, Preston; Chou, Felcia (April 7, 2015). "The Solar System and Beyond is Awash in Water". NASA. Retrieved April 8, 2015.
- NASA (June 18, 2020). "Are planets with oceans common in the galaxy? It's likely, NASA scientists find". EurekAlert!. Retrieved June 20, 2020.
- Shekhtman, Lonnie; et al. (June 18, 2020). "Are Planets with Oceans Common in the Galaxy? It's Likely, NASA Scientists Find". NASA. Retrieved June 20, 2020.