Liquids/Liquid objects/Oceans

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This image shows the Earth's oceans and their bottoms. Credit: NOAA.

Def. on Earth one "of the five large bodies of water separating the continents"[1] is called an ocean.

Oceanography[edit | edit source]

Def. the "exploration and scientific study of the oceans and ocean floor"[2] is called an oceanography.

Oceanography, also called oceanology or marine science, studies the ocean. It covers a wide range of topics, including marine organisms and ecosystem dynamics; ocean currents, waves, and geophysical fluid dynamics; plate tectonics and the geology of the sea floor; and fluxes of various chemical substances and physical properties within the ocean and across its boundaries.


Marine biology[edit | edit source]

A deep-sea chimaera image shows its snout covered with tiny pores capable of detecting animals by perturbations in electric fields. Credit: NOAA.

Oceans average nearly four kilometres in depth and are fringed with coastlines that run for 360,000 kilometres.[3][4]

The ocean is a complex three-dimensional world[5] covering approximately 71% of the Earth's surface.

Marine organisms contribute significantly to the oxygen cycle, and are involved in the regulation of the Earth's climate.[6] Shorelines are in part shaped and protected by marine life, and some marine organisms even help create new land.[7]

The development of technology such as sound navigation ranging, scuba diving gear, submersibles and remotely operated vehicles allowed marine biologists to discover and explore life in deep oceans that was once thought to not exist.[8]

Microbes are responsible for virtually all the photosynthesis that occurs in the ocean, as well as the cycling of carbon, nitrogen, phosphorus and other nutrients and trace elements.[9]

Over 1500 species of fungi are known from marine environments.[10] These are parasitic on marine algae or animals, or are saprobes on algae, corals, protozoan cysts, sea grasses, wood and other substrata, and can also be found in sea foam.[11] Spores of many species have special appendages which facilitate attachment to the substratum.[12] A very diverse range of unusual secondary metabolites is produced by marine fungi.[13]

33,400 species of fish, including bony and cartilaginous fish, had been described by 2016,[14] more than all other vertebrates combined. About 60% of fish species live in saltwater.[15]

Despite their marine adaptations, most sea snakes prefer shallow waters nearby land, around islands, especially waters that are somewhat sheltered, as well as near estuaries.[16][17]

All marine mammals are air-breathing, and while some such as the sperm whale can dive for prolonged periods, all must return to the surface to breathe.[18][19]

Marine chemistry[edit | edit source]

Marine chemistry, also known as ocean chemistry and chemical oceanography, studies the chemistry of marine environments under the influence of different variables, such as currents, sediments, pH levels, atmospheric constituents, metamorphic activity, and ecology.

Temperatures[edit | edit source]

This illustration shows the Earth's sea surface temperature from infrared observations by the Advanced Very High Resolution Radiometer (AVHRR) during July 1984. Credit: NASA.
The histogram represents annual anomalies (units: ZJ) from the upper 2000 m Ocean Heat Content from 1955 through 2019, wherein positive anomalies relative to a 1981−2010 baseline are shown as red bars and negative anomalies as blue. Credit: Lijing Cheng, John Abraham, Jiang Zhu, Kevin E. Trenberth, John Fasullo, Tim Boyers, Ricardo Locarnini, Bin Zhang, Fujiang Yu, Liying Wan, Xingrong Chen, Xiangzhou Song, Yulong Liu, and Michael E. Mann.{{fairuse}}
An analysis of sea surface temperature data collected by satellites is shown. Credit: R. W. Schlegel, Marine Heatwave Tracker (2020).{{fairuse}}

"The above illustration of Earth's sea surface temperature was obtained from two weeks of infrared observations by the Advanced Very High Resolution Radiometer (AVHRR), an instrument on board NOAA-7 during July 1984. Temperatures are color coded with red being warmest and decreasing through oranges, yellows, greens, and blues. Temperature patterns seen in this image are the result of many influences, including the circulation of the ocean, surface winds, and solar heating. The image indicates a large pool of warm water in the Western Pacific and a tongue of relatively cold water extending along the Equator westward from South America. Every few years, there occurs an interrelated set of changes in the global atmospheric and oceanic circulation known as an El Nino in which the region of warm equatorial water in the West extends eastward across the Pacific and blankets the cool, productive regions along the coast of South America. Fish, birds, and marine mammals that depend upon the normally phytoplankton-rich waters often die in large numbers during El Nino. Images of sea surface temperature such as this help scientists to better monitor and ultimately understand the changes to Earth caused by events such as El Nino."[20]

"The [ocean heat content] OHC values (for the upper 2000 m) were obtained from the Institute of Atmospheric Physics (IAP) ocean analysis [...], which uses a relatively new method to treat data sparseness and updates in the instruments that have been used to measure ocean temperature (Cheng et al., 2017). The evolution of OHC [see the image on the right] shows that the upper 2000 m OHC in 2019 was 228 ± 9 ZJ [Zetta Joules (ZJ, 1 ZJ=1021 Joules)] above the 1981–2010 average. The record-setting ocean warmth is also found in National Oceanic and Atmospheric Administration/National Center for Environmental Information (NOAA/NCEI) data, showing 217± 4 ZJ in 2019 above 1981−2010 average (21 ZJ above 2018) [...] (updated from Levitus et al. 2012). With these newly available IAP data, a ranking of the warmest years since 1950s is now possible [...]. The past five years are the top five warmest years in the ocean historically with modern instruments, and the past ten years are also the top ten years on record. The same ranking also applies to NOAA/NCEI data [...]."[21]

"A large marine heatwave, dubbed The Blob, developed off the western coast of North America in 2013 and lingered to the middle of 2016. This map [on the right] shows satellite measurements of ocean surface temperatures, with colours indicating values higher (red) and lower ([white]) than the average from [2011] to [2020]."[22]

Salinity[edit | edit source]

The map above shows salinity near the ocean surface as measured by the Aquarius instrument on the Satélite de Aplicaciones Científicas (SAC)-D satellite. Credit: NASA's Earth Observatory.

"Salinity—the amount of dissolved salt in the water—is critical to so many aspects of the ocean, from circulation to climate to the global water cycle. For much of the past year, NASA and Argentina’s Comisión Nacional de Actividades Espaciales (CONAE) have been making comprehensive observations of sea surface salinity from space. Launched on June 10, 2011, the Aquarius mission is slowly compiling a more complete picture of the salty sea and how it varies."[23]

"The map above shows salinity near the ocean surface as measured by the Aquarius instrument on the Satélite de Aplicaciones Científicas (SAC)-D satellite. The data depicted shows average salinity from May 27 to June 2, 2012, in a range from 30 to 40 grams per kilogram, with 35 grams being the average. Lower values are represented in purples and blues; higher values are shown in shades of orange and red. Black areas occur where no data was available, either due to the orbit of the satellite or because the ocean was covered by ice, which Aquarius cannot see through."[23]

"[T]he Atlantic Ocean is saltier than the Pacific and Indian Oceans. Rivers such as the Amazon carry tremendous amounts of fresh runoff from land and spread plumes far into the sea. And in the tropics—particularly near the Pacific’s Inter-Tropical Convergence Zone—extra rainfall makes equatorial waters somewhat fresher."[23]

"Near most coastlines and inland seas in the map, waters appear much fresher or saltier than in open-ocean locations. Look, for instance, at the Red Sea and the Mediterranean for saltier waters; significantly fresher waters appear in the Black Sea, in the icy high latitudes, and around the many islands and peninsulas of Southeast Asia. Indeed, runoff from rivers and melting ice does make water fresher, and strong evaporation and other processes do make the Red and Mediterranean Seas saltier. But mostly those extreme salinity measurements around the coastlines are a distortion of the satellite signal."[23]

"Technically, Aquarius measures the emissivity or “brightness temperature” of the surface waters, notes Gary Lagerloef, Aquarius principal investigator, based at Earth and Space Research in Seattle. Land masses have a higher emissivity than the ocean, so any measurement close to land tends to be skewed by its brightness. Over time, the Aquarius research team should be able to calibrate the measurements and develop mathematical tools to better distinguish the salt signal. But for now, the measurements are so new that the team is still working on the big picture of ocean salinity."[23]

“An overarching question in climate research is to understand how changes in the Earth’s water cycle—meaning rainfall and evaporation, river discharges and so forth—ocean circulation, and climate link together,” said Lagerloef.[23]

"Most global precipitation and evaporation events take place over the ocean and are very difficult to measure. But rainfall freshens the ocean’s surface waters, and Aquarius can detect these changes in saltiness."[23]

“Salinity is the variable we can use to measure that coupling. It’s a critical factor, and it will eventually be used to improve climate forecasts.”[23]

Thermohaline circulations[edit | edit source]

A summary of the path of the thermohaline circulation. Blue paths represent deep-water currents, while red paths represent surface currents. Credit: Robert Simmon, NASA.{{free media}}
Thermohaline circulation shows improved flow fields. Credit: NASA/Goddard Space Flight Center.{{free media}}

Thermohaline circulation (THC) is a part of the large-scale ocean circulation that is driven by global density gradients created by surface heat and freshwater fluxes.[24][25] The adjective thermohaline derives from thermo- referring to temperature and -haline referring to salinity (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 en route, and eventually sinking at high latitudes (forming North Atlantic Deep Water), dense water then flows into the ocean basins, while the bulk of it upwells in the Southern Ocean, the oldest waters (with a transit time of about 1000 years)[26] upwell in the North Pacific.[27]

Aragonites[edit | edit source]

This map shows changes in the amount of aragonite dissolved in ocean surface waters between the 1880s and the most recent decade (2003-2012). Credit: US EPA.

"Aragonite is a form of calcium carbonate that many marine animals use to build their skeletons and shells. Aragonite saturation is a ratio that compares the amount of aragonite that is actually present with the total amount of aragonite that the water could hold if it were completely saturated. The more negative the change in aragonite saturation, the larger the decrease in aragonite available in the water, and the harder it is for marine creatures to produce their skeletons and shells."[28]

"Measurements made over the last few decades have demonstrated that ocean carbon dioxide levels have risen in response to increased carbon dioxide in the atmosphere, leading to an increase in acidity (that is, a decrease in pH)"[28].

"Historical modeling suggests that since the 1880s, increased carbon dioxide has led to lower aragonite saturation levels (less availability of minerals) in the oceans around the world (see [above image])."[28]

"The largest decreases in aragonite saturation have occurred in tropical waters (see [above image]). However, decreases in cold areas may be of greater concern because colder waters typically have lower aragonite levels to begin with."[28]

Mixed layers[edit | edit source]

The illustration shows the mixed layer depth in meters from the surface down to the considered depth below which mixing is lacking or much less. Credit: Giorgiogp2.

The oceanic mixed layer is a layer in which active turbulence has homogenized variables such as temperature and salinity to some range of depths. The surface mixed layer is a layer where this turbulence is generated by winds, cooling, or processes such as evaporation or sea ice formation which result in an increase in salinity.

The mixed layer is characterized by being nearly uniform in properties such as temperature and salinity throughout the layer. Velocities, however, may exhibit significant shears within the mixed layer. The bottom of the mixed layer is characterized by a gradient, where the water properties change.

The depth of the mixed layer is often determined by hydrography—making measurements of water properties.

Gulf Stream[edit | edit source]

The figure shows the near-surface currents of the Gulf Stream for 09 January 1995. Credit: FLAME/Drakkar modeling group IFM-GEOMAR.
Gulf stream map is made from NOAA 2 minute color relief images. Credit: RedAndr.{{free media}}
This shows the general near-surface current of the Gulf Stream. Credit: NASA.
Warm, salty waters of the tropical Atlantic circulate north to the sub-polar regions of the North Atlantic via the Gulf Stream (dark blue arrows). Credit: Matthew W. Schmidt (Department of Oceanography, Texas A&M University, College Station, TX) & Jennifer E. Hertzberg (Department of Oceanography, Texas A&M University, College Station, TX).
A satellite picture of the Atlantic before North America in May 2001. Credit: Max-Planck Institute for Meteorology.

In the figure on the right, blue areas shows slower, yellow and red areas faster currents.

"In the middle of the Ocean, between Greenland and Norway and before Newfoundland, enormous masses of water disappear from the surface and plunge straight down to the bottom – thousands of meters deep, according to scientists. Like the drain-hole of a bathtub, this succion movement draws twenty times more water into the abyss than all the rivers of Earth together carry into the oceans."[29]

"This downward motion is the engine which from all appareances powers the whole global conveyer belt, the mighty system of water exchanges between the seas and oceans of Earth. The Gulfstream participates prominently in this so-called thermohaline circulation: in tropical regions, the sun heats up the surface waters and through evaporation, it increases the level of salinity. Additionally propulsed by winds and deviated by means of the Coriolis force created by the Earth’s rotation, the Gulfstream transports water from the Equator to the North."[29]

"But where are the mega-streams hiding?"[29]

"Where and how the water sinks down, we do not know.”[30]

"Despite the fact that scientific research vessels have been cruising the area for almost one hundred years, and that they have studied the ocean all the way to the bottom, and are constantly watching measurement buoys in the waters, scientists have been merely able to identify tiny downward swirls."[29]

"In the Sea of Labrador and in front of Greenland alone, 150 times more water is supposed to sink to the bottom than is driven into the ocean by the Amazon. But merely trickles have been found."[29]

The vertical twirls are “small and therefore not directly measurable. It’s a challenge, to have a measuring instrument at the ready in the right spot and at the right time.”[31]

"The search is made more difficult because the water apparently sinks only sporadically, and the areas of down-welling move around."[32]

The "colors [in the third figure down on the right] symbolize the repartition of temperatures on the surface of the water. In the red areas, it reaches up to 25° C."[29]

"The correlation is astonishing, because it implies that the dramatic climate changes during the first more than 50 kyrs of the glaciation elapsed nearly in parallel on both sides of the North Atlantic Ocean, presumably controlled by varying sea ice cover. Thus, the Gulf Stream was not just deflected toward North Africa in cold periods, it was rather turned off."[33]

Hydrology[edit | edit source]

This true-color image is the most detailed of the entire Earth produced to date. Credit: NASA, MODIS, USGS, and DMSP.

"This spectacular “blue marble” image is the most detailed true-color image of the entire Earth to date. Using a collection of satellite-based observations, scientists and visualizers stitched together months of observations of the land surface, oceans, sea ice, and clouds into a seamless, true-color mosaic of every square kilometer (.386 square mile) of our planet."[34]

"Much of the information contained in this image came from a single remote-sensing device-NASA’s Moderate Resolution Imaging Spectroradiometer, or MODIS. Flying over 700 km above the Earth onboard the Terra satellite, MODIS provides an integrated tool for observing a variety of terrestrial, oceanic, and atmospheric features of the Earth. The land and coastal ocean portions of these images are based on surface observations collected from June through September 2001 and combined, or composited, every eight days to compensate for clouds that might block the sensor’s view of the surface on any single day. Two different types of ocean data were used in these images: shallow water true color data, and global ocean color (or chlorophyll) data. Topographic shading is based on the GTOPO 30 elevation dataset compiled by the U.S. Geological Survey’s EROS Data Center. MODIS observations of polar sea ice were combined with observations of Antarctica made by the National Oceanic and Atmospheric Administration’s AVHRR sensor—the Advanced Very High Resolution Radiometer. The cloud image is a composite of two days of imagery collected in visible light wavelengths and a third day of thermal infra-red imagery over the poles."[34]

See also[edit | edit source]

References[edit | edit source]

  1. 217.225.67.54 (17 March 2004). "ocean". San Francisco, California: Wikimedia Foundation, Inc. Retrieved 2014-12-16.
  2. SemperBlotto (21 April 2005). "oceanography". San Francisco, California: Wikimedia Foundation, Inc. Retrieved 2014-12-16.
  3. Charette, Matthew; Smith, Walter H. F. (2010). "The volume of Earth's ocean". Oceanography 23 (2): 112–114. doi:10.5670/oceanog.2010.51. http://www.tos.org/oceanography/archive/23-2_charette.html. Retrieved 13 January 2014. 
  4. World The World Factbook, CIA. Retrieved 13 January 2014.
  5. Oceanographic and Bathymetric Features Marine Conservation Institute. Uploaded 18 September 2013.
  6. Foley, Jonathan A.; Taylor, Karl E.; Ghan, Steven J. (1991). "Planktonic dimethylsulfide and cloud albedo: An estimate of the feedback response". Climatic Change 18 (1): 1. doi:10.1007/BF00142502. 
  7. Sousa, Wayne P. (1986) [1985]. "7, Disturbance and Patch Dynamics on Rocky Intertidal Shores". In Pickett, Steward T. A.; White, P. S.. The Ecology of Natural Disturbance and Patch Dynamics. Academic Press. ISBN 978-0-12-554521-1. https://books.google.com/books?id=jIj-qAflWxQC&pg=PA101&dq=patch+dynamics+shoreline. 
  8. Anderson, Genny. "Beginnings: History of Marine Science".
  9. "Functions of global ocean microbiome key to understanding environmental changes". www.sciencedaily.com. University of Georgia. December 10, 2015. Retrieved December 11, 2015.
  10. Hyde, K.D.; E.B.J. Jones; E. Leaño; S.B. Pointing; A.D. Poonyth; L.L.P. Vrijmoed (1998). "Role of fungi in marine ecosystems". Biodiversity and Conservation 7 (9): 1147–1161. doi:10.1023/A:1008823515157. 
  11. Kirk, P.M., Cannon, P.F., Minter, D.W. and Stalpers, J. "Dictionary of the Fungi". Edn 10. CABI, 2008
  12. Hyde, K.D.; E.B.J. Jones (1989). "Spore attachment in marine fungi". Botanica Marina 32 (3): 205–218. doi:10.1515/botm.1989.32.3.205. 
  13. San-Martín, A.; S. Orejanera; C. Gallardo; M. Silva; J. Becerra; R. Reinoso; M.C. Chamy; K. Vergara et al. (2008). "Steroids from the marine fungus Geotrichum sp". Journal of the Chilean Chemical Society 53 (1): 1377–1378. 
  14. "Fishbase". Retrieved 6 February 2017.
  15. Moyle, P. B.; Leidy, R. A. (1992). Fiedler, P. L.. ed. Loss of biodiversity in aquatic ecosystems: Evidence from fish faunas. Chapman and Hall. pp. 128–169. 
  16. Stidworthy J. 1974. Snakes of the World. Grosset & Dunlap Inc. 160 pp. isbn 0-448-11856-4.
  17. Food and Agriculture Organization of the United Nations. Accessed 7 August 2007.
  18. Kaschner, K.; Tittensor, D. P.; Ready, J.; Gerrodette, T.; Worm, B. (2011). "Current and Future Patterns of Global Marine Mammal Biodiversity". PLoS ONE 6 (5): e19653. doi:10.1371/journal.pone.0019653. PMID 21625431. 
  19. Pompa, S.; Ehrlich, P. R.; Ceballos, G. (2011-08-16). "Global distribution and conservation of marine mammals". Proceedings of the National Academy of Sciences 108 (33): 13600–13605. doi:10.1073/pnas.1101525108. PMID 21808012. 
  20. Michael Hahn (May 13, 2010). Global Sea Surface Temperature. Goddard Space Flight Center. http://grin.hq.nasa.gov/ABSTRACTS/GPN-2003-00032.html. Retrieved 2013-02-27. 
  21. Lijing Cheng; John Abraham; Jiang Zhu; Kevin E. Trenberth; John Fasullo; Tim Boyers; Ricardo Locarnini; Bin Zhang et al. (February 2020). "Record-Setting Ocean Warmth Continued in 2019". Advances in Atmospheric Sciences 37 (2): 137-42. doi:10.1007/s00376-020-9283-7. https://link.springer.com/content/pdf/10.1007/s00376-020-9283-7.pdf. Retrieved 15 January 2020. 
  22. Giuliana Viglione (5 May 2021). "Fevers are plaguing the oceans — and climate change is making them worse". Nature. Retrieved 6 May 2021.
  23. 23.0 23.1 23.2 23.3 23.4 23.5 23.6 23.7 Norman Kuring; Robert Simmon; Mike Carlowicz; Maria-Jose Vinas (June 12, 2012). A Measure of Salt. NASA Earth Observatory. http://earthobservatory.nasa.gov/IOTD/view.php?id=78250&src=flickr. Retrieved 2013-02-27. 
  24. Rahmstorf, S (2003). "The concept of the thermohaline circulation". Nature 421 (6924): 699. doi:10.1038/421699a. PMID 12610602. http://www.pik-potsdam.de/~stefan/Publications/Nature/nature_concept_03.pdf. 
  25. 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. 
  26. The global ocean conveyor belt is a constantly moving system of deep-ocean circulation driven by temperature and salinity; What is the global ocean conveyor belt?
  27. 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. https://escholarship.org/content/qt5f76r4wn/qt5f76r4wn.pdf?t=n3tp5j. 
  28. 28.0 28.1 28.2 28.3 R.A. Feely; S.C. Doney; S.R. Cooley (December 12, 2012). Ocean Acidity. United States Environmental Protection Agency. http://www.epa.gov/climatechange/science/indicators/oceans/acidity.html#fragment-2. Retrieved 2013-02-27. 
  29. 29.0 29.1 29.2 29.3 29.4 29.5 Axel Bojanowski, translated by Anne-Marie de Grazia (24 July 2009). Mega-Streams of the Atlantic Where are they hiding?. Der Spiegel. http://www.q-mag.org/mega-streams-of-the-atlantic.html. Retrieved 2015-01-13. 
  30. Jochem Marotzke, translated by Anne-Marie de Grazia (24 July 2009). Mega-Streams of the Atlantic Where are they hiding?. Der Spiegel. http://www.q-mag.org/mega-streams-of-the-atlantic.html. Retrieved 2015-01-13. 
  31. Detlef Stammer, translated by Anne-Marie de Grazia (24 July 2009). Mega-Streams of the Atlantic Where are they hiding?. Der Spiegel. http://www.q-mag.org/mega-streams-of-the-atlantic.html. Retrieved 2015-01-13. 
  32. Detlef Quadfasel, translated by Anne-Marie de Grazia (24 July 2009). Mega-Streams of the Atlantic Where are they hiding?. Der Spiegel. http://www.q-mag.org/mega-streams-of-the-atlantic.html. Retrieved 2015-01-13. 
  33. Willi Dansgaard (2005). The Department of Geophysics of The Niels Bohr Institute for Astronomy Physics and Geophysics at The University of Copenhagen Denmark. ed. Frozen Annals Greenland Ice Cap Research. Copenhagen, Denmark: Niels Bohr Institute. pp. 123. ISBN 87-990078-0-0. http://www.iceandclimate.nbi.ku.dk/publications/FrozenAnnals.pdf/. Retrieved 2014-10-05. 
  34. 34.0 34.1 Reto Stöckli; Robert Simmon (February 8, 2002). The Blue Marble: Land Surface, Ocean Color, Sea Ice and Clouds. Greenbelt, Maryland USA: NASA Visible Earth, NASA Goddard Space Flight Center. http://visibleearth.nasa.gov/view.php?id=57735. Retrieved 2013-02-28. 

External links[edit | edit source]