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For the scientific journal, see Oceanography (journal).
"Ocean science" redirects here. For the scientific journal, see Ocean Science (journal).
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Thermohaline circulation
Oceanography (compound of the Greek words ὠκεανός meaning "ocean" and γράφω meaning "write"), also known as oceanology and marine science, is the branch of Earth science that 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. These diverse topics reflect multiple disciplines that oceanographers blend to further knowledge of the world ocean and understanding of processes within: astronomy, biology, chemistry, climatology, geography, geology, hydrology, meteorology and physics.
Contents
- 1 History
- 1.1 Early history
- 1.2 Modern oceanography
- 1.3 Ocean acidification
- 1.4 Ocean currents
- 1.5 Ocean heat content
- 1.6 Branches
- 1.7 Oceanographic institutions
- 2 Related disciplines
- 3 See also
- 4 References
- 5 Further reading
- 6 External links
History
Map of the Gulf Stream by Benjamin Franklin, 1769-1770. Courtesy of the NOAA Photo Library.
Early history
Our planet is invested with two great oceans; one visible, the other invisible; one underfoot, the other overhead; one entirely envelopes it, the other covers about two thirds of its surface.
—Matthew F. Maury, The Physical Geography of the Seas and Its Meteorology (1855)
Humans first acquired knowledge of the waves and currents of the seas and oceans in pre-historic times. Observations on tides were recorded by Aristotle and Strabo. Early exploration of the oceans was primarily for cartography and mainly limited to its surfaces and of the animals that fishermen brought up in nets, though depth soundings by lead line were taken.
Although Juan Ponce de León in 1513 first identified the Gulf Stream, and the current was well-known to mariners, Benjamin Franklin made the first scientific study of it and gave it its name. Franklin measured water temperatures during several Atlantic crossings and correctly explained the Gulf Stream's cause. Franklin and Timothy Folger printed the first map of the Gulf Stream in 1769-1770.[1][2]
Map of the currents in the Atlantic and Indian Oceans, by James Rennell in 1799.
Information on the ocean currents of the Pacific was gathered by explorers of the late 18th century, including James Cook and Louis Antoine de Bougainville. James Rennell wrote the first scientific textbooks on oceanography, detailing the current flows of the Atlantic and Indian oceans. During a voyage around the Cape of Good Hope in 1777, he mapped "the banks and currents at the Lagullas". He was also the first to understand the nature of the intermittent current near the Isles of Scilly, (now known as Rennell's Current).[3]
Sir James Clark Ross took the first modern sounding in deep sea in 1840, and Charles Darwin published a paper on reefs and the formation of atolls as a result of the second voyage of HMS Beagle in 1831-6. Robert FitzRoy published a report in four volumes of the three voyages of the Beagle. In 1841–1842 Edward Forbes undertook dredging in the Aegean Sea that founded marine ecology.
As first superintendent of the United States Naval Observatory (1842–1861) Matthew Fontaine Maury devoted his time to the study of marine meteorology, navigation, and charting prevailing winds and currents. His Physical Geography of the Sea, 1855 was one of the first textbooks on oceanography. Many nations sent oceanographic observations to Maury at the Naval Observatory, where he and his colleagues evaluated the information and gave the results worldwide distribution.[4]
Modern oceanography
Despite all this, however, human knowledge of the oceans remained confined to the topmost few fathoms of the water and a small amount of the bottom, mainly in shallow areas. Almost nothing was known of the ocean depths. The Royal Navy's efforts to chart all of the world's coastlines in the mid-19th century reinforced the vague idea that most of the ocean was very deep, although little more was known. As exploration ignited both popular and scientific interest in the polar regions and Africa, so too did the mysteries of the unexplored oceans.
HMS Challenger undertook the first global marine research expedition in 1872.
The seminal event in the founding of the modern science of oceanography was the Challenger expedition. As the first true oceanographic cruise, the Challenger expedition laid the groundwork for an entire academic and research discipline.[5] In 1871, under the recommendations of the Royal Society of London, the British government sponsored an expedition to explore world's oceans and conduct appropriate scientific investigation. Under that sponsorship, the Scots Charles Wyville Thompson and Sir John Murray launched the Challenger expedition, from 1872 to 1876. The ship, leased from the Royal Navy, was modified for scientific work and equipped with separate laboratories for natural history and chemistry.[6] Under the scientific supervision of Thomson, Challenger travelled nearly 70,000 nautical miles (130,000 km) surveying and exploring. On her journey circumnavigating the globe,[6] 492 deep sea soundings, 133 bottom dredges, 151 open water trawls and 263 serial water temperature observations were taken.[7] Also about 4,700 new species of marine life were discovered. The result was the Report Of The Scientific Results of the Exploring Voyage of H.M.S. Challenger during the years 1873-76. John Murray, who supervised the publication, described the report as "the greatest advance in the knowledge of our planet since the celebrated discoveries of the fifteenth and sixteenth centuries". John Murray went on to found the academic discipline of oceanography at the University of Edinburgh, which remained the centre for oceanographic research well into the 20th century.[8] Murray was the first to study marine trenches and in particular the Mid-Atlantic Ridge, and map the sedimentary deposits in the oceans. He tried to map out the world's ocean currents based on salinity and temperature observations, and was the first to correctly understand the nature of coral reef development.
In the late 19th century, other Western nations also sent out scientific expeditions (as did private individuals and institutions). The first purpose built oceanographic ship, the Albatros, was built in 1882. In 1893, Fridtjof Nansen allowed his ship, Fram, to be frozen in the Arctic ice. This enabled him to obtain oceanographic, meteorological and astronomical data.
Ocean currents (1911)
Between 1907 and 1911 Otto Krümmel published the Handbuch der Ozeanographie, influential in awakening public interest in oceanography.[9] The four-month 1910 North Atlantic expedition headed by Sir John Murray and Johan Hjort was at that time the most ambitious research oceanographic and marine zoological project ever, and led to the classic 1912 book The Depths of the Ocean.
The first acoustic measurement of sea depth was made in 1914. Between 1925 and 1927 the "Meteor" expedition gathered 70,000 ocean depth measurements using an echo sounder, surveying the Mid-Atlantic ridge.
In 1942, Sverdrup and Fleming published The Ocean, which was a major landmark. The Sea (in three volumes, covering physical oceanography, seawater and geology) edited by M.N. Hill was published in 1962, while Rhodes Fairbridge's Encyclopedia of Oceanography was published in 1966.
The Great Global Rift, running along the Mid Atlantic Ridge, was discovered by Maurice Ewing and Bruce Heezen in 1953 while the mountain range under the Arctic was found in 1954 by the Arctic Institute of the USSR. The theory of seafloor spreading was developed in 1960 by Harry Hammond Hess. The Ocean Drilling Project started in 1966. Deep sea vents were discovered in 1977 by John Corlis and Robert Ballard in the submersible "Alvin".
In the 1950s, Auguste Piccard invented the bathyscaphe and used the "Trieste" to investigate the ocean's depths. The nuclear submarine Nautilus made the first journey under the ice to the North Pole in 1958. In 1962 there was the first deployment of FLIP (Floating Instrument Platform), a 355 foot spar buoy.
From the 1970s, there has been much emphasis on the application of large scale computers to oceanography to allow numerical predictions of ocean conditions and as a part of overall environmental change prediction. An oceanographic buoy array was established in the Pacific to allow prediction of El Niño events.
1990 saw the start of the World Ocean Circulation Experiment (WOCE) which continued until 2002. Geosat seafloor mapping data became available in 1995.
In recent years studies advanced particular knowledge on ocean acidification, ocean heat content, ocean currents, ENSO, mapping of methane hydrate deposits, the carbon cycle, coastal erosion, weathering and climate feedbacks in regards to climate change interactions.
The study of the oceans is linked to understanding global climate changes, potential global warming and related biosphere concerns. The atmosphere and ocean are linked because of evaporation and precipitation as well as thermal flux (and solar insolation). Wind stress is a major driver of ocean currents while the ocean is a sink for atmospheric carbon dioxide. All these factors specially relate to the ocean's biogeochemical setup.
Ocean acidification
Main article: Ocean acidification
Ocean acidification describes the decrease in ocean pH, caused by anthropogenic carbon dioxide (CO2) emissions into the atmosphere.[10] Seawater is slightly alkaline and had a preindustrial pH of about 8.2. More recently, anthropogenic activities have steadily increased the carbon dioxide content of the atmosphere; about 30–40% of the added CO2 is absorbed by the oceans, forming carbonic acid and lowering the pH (now below 8.1[11]) through ocean acidification.[12][13][14] The pH is expected to reach 7.7 by the year 2100.[15]
An important element for the skeletons of marine animals is calcium, but calcium carbonate becomes more soluble with pressure, so carbonate shells and skeletons dissolve below the carbonate compensation depth.[16] Calcium carbonate becomes more soluble at lower pH, so ocean acidification is likely to affect marine organisms with calcareous shells, such as oysters, clams, sea urchins and corals,[17][18] and the carbonate compensation depth will rise closer to the sea surface. Affected planktonic organisms will include pteropods, coccolithophorids and foraminifera, all important in the food chain. In tropical regions, corals are likely to be severely affected as they become less able to build their calcium carbonate skeletons,[19] in turn adversely impacting other reef dwellers.[15]
The current rate of ocean chemistry change seems to be unprecedented in Earth's geological history, making it unclear how well marine ecosystems will adapt to the shifting conditions of the near future.[20] Of particular concern is the manner in which the combination of acidification with the expected additional stressors of higher temperatures and lower oxygen levels will impact the seas.[21]
Ocean currents
Further information: Ocean current
Since the early ocean expeditions in oceanography, a major interest was the study of the ocean currents and temperature measurements. The tides, the Coriolis effect, changes in direction and strength of wind, salinity and temperature are the main factors determining ocean currents. The thermohaline circulation (THC) thermo- referring to temperature and -haline referring to salt content connects 4 of 5 ocean basins and is primarily dependent on the density of sea water. Ocean currents such as the Gulf Stream are wind-driven surface currents.
Ocean heat content
Oceans of Climate Change NASA
Further information: Oceanic heat content
Oceanic heat content (OHC) is the term used to refer to the heat stored in the ocean. The changes in the ocean heat play an important role in sea level rise, because of thermal expansion. It is with high confidence that Ocean warming accounts for 90% of the energy accumulation from global warming between 1971 and 2010.[22]
Branches
Oceanographic frontal systems on the Southern Hemisphere
The study of oceanography is divided into branches:
- Biological oceanography investigates the ecology of marine organisms in the context of the physical, chemical, and geological characteristics of their ocean environment. It is closely aligned with marine biology, though the latter has more emphasis on the biology of individual marine organisms.
- Chemical oceanography, or marine chemistry, is the study of the chemistry of the ocean and its chemical interaction with the atmosphere;
- Geological oceanography, or marine geology, is the study of the geology of the ocean floor including plate tectonics and paleoceanography;
- Physical oceanography, or marine physics, studies the ocean's physical attributes including temperature-salinity structure, mixing, waves, internal waves, surface tides, internal tides, and currents.
These branches reflect the fact that many oceanographers are first trained in the exact sciences or mathematics and then focus on applying their interdisciplinary knowledge, skills and abilities to oceanography.[23]
Data derived from the work of Oceanographers is used in marine engineering, in the design and building of oil platforms, ships, harbours, and other structures that allow us to use the ocean safely.[24]
Oceanographic data management is the discipline ensuring that oceanographic data both past and present are available to researchers.
Oceanographic institutions
See also: List of oceanographic institutions and programs
The first international organization of oceanography was created in 1902 as the International Council for the Exploration of the Sea. In 1892 the Scripps Institution of Oceanography was founded, followed by Woods Hole Oceanographic Institution in 1930, Virginia Institute of Marine Science in 1938, and later the Lamont-Doherty Earth Observatory at Columbia University, and the School of Oceanography at University of Washington. In Britain, the National Oceanography Centre, Southampton is the successor to the Institute of Oceanography. In Australia, CSIRO Marine and Atmospheric Research, known as CMAR, is a leading center. In 1921, the International Hydrographic Bureau (IHB) was formed in Monaco.
Related disciplines
- Biogeochemistry
- Biogeography
- Climatology
- Coastal geography
- Environmental science
- Geophysics
- Glaciology
- Hydrography
- Hydrology
- Limnology
- Meteorology
See also
| Underwater diving portal |
- Anoxic event – Anoxic sea water
- Argo (oceanography)
- Bathymetric chart
- Ecological Forecasting
- List of ocean circulation models
- List of seas
- List of submarine topographical features
- Marine archaeology
- Marine current power
- Marine engineering
- Ocean colonization
- Ocean engineering
- Oceans Act of 2000
- Sea level
- Sea level rise
References
- ^ 1785: Benjamin Franklin's 'Sundry Maritime Observations'
- ^ Wilkinson, Jerry. History of the Gulf Stream January 01, 2008.
- ^ Lee, Sidney, ed. (1896). "Rennell, James". Dictionary of National Biography 48. London: Smith, Elder & Co.
- ^ Williams, Frances L. Matthew Fontaine Maury, Scientist of the Sea. (1969) ISBN 0-8135-0433-3.
- ^ Then and Now: The HMS Challenger Expedition and the 'Mountains in the Sea' Expedition, Ocean Explorer website (NOAA), accessed 01/02/2012
- ^ a b Rice, A.L. (1999). "The Challenger Expedition". Understanding the Oceans: Marine Science in the Wake of HMS Challenger. Routledge. pp. 27–48. ISBN 978-1-85728-705-9.
- ^ Oceanography: an introduction to the marine environment (Peter K. Weyl, 1970), p.49
- ^ "Sir John Murray (1841-1914) - Founder Of Modern Oceanography". Science and Engineering at The University of Edinburgh. Retrieved 7 November 2013.
- ^ Otto Krümmel (1907). [Online Abstract Handbuch der Ozeanographie]. J. Engelhorn.
- ^ Caldeira, K.; Wickett, M. E. (2003). "Anthropogenic carbon and ocean pH". Nature 425 (6956): 365–365. Bibcode:2001AGUFMOS11C0385C. doi:10.1038/425365a. PMID 14508477. Cite uses deprecated parameters (help)
- ^ "Ocean Acidity". U.S. EPA climate change web site. EPA. 2013-09-13. Retrieved 2013-11-01.
- ^ Feely, R. A.; et al. (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. Cite uses deprecated parameters (help)
- ^ Zeebe, R. E.; Zachos, J. C.; Caldeira, K.; Tyrrell, T. (2008-07-04). "OCEANS: Carbon Emissions and Acidification". Science 321 (5885): 51–52. doi:10.1126/science.1159124. PMID 18599765.
- ^ Gattuso, J.-P.; Hansson, L. (2011-09-15). Ocean Acidification. Oxford University Press. ISBN 978-0-19-959109-1. OCLC 730413873.
- ^ a b "Ocean acidification". Department of Sustainability, Environment, Water, Population & Communities: Australian Antarctic Division. 28 September 2007. Retrieved 17 April 2013.
- ^ Pinet, Paul R. (1996). Invitation to Oceanography. West Publishing Company. pp. 126, 134–135. ISBN 978-0-314-06339-7.
- ^ "What is Ocean Acidification?". NOAA PMEL Carbon Program. Retrieved 15 September 2013.
- ^ Orr, James C.; et al. (2005). "Anthropogenic ocean acidification over the twenty-first century and its impact on calcifying organisms". Nature 437 (7059): 681–686. Bibcode:2005Natur.437..681O. doi:10.1038/nature04095. PMID 16193043. Archived from the original on 2008-06-25. Cite uses deprecated parameters (help)
- ^ Cohen, A.; Holcomb, M. (2009). "Why Corals Care About Ocean Acidification: Uncovering the Mechanism". Oceanography 24 (4): 118–127. doi:10.5670/oceanog.2009.102.
- ^ Hönisch, Bärbel; Ridgwell, Andy; Schmidt, Daniela N.; Thomas, E.; Gibbs, S. J.; Sluijs, A.; Zeebe, R.; Kump, L.; Martindale, R. C.; Greene, S. E.; Kiessling, W.; Ries, J.; Zachos, J. C.; Royer, D. L.; Barker, S.; Marchitto, T. M.; Moyer, R.; Pelejero, C.; Ziveri, P.; Foster, G. L.; Williams, B. (2012). "The Geological Record of Ocean Acidification". Science 335 (6072): 1058–1063. Bibcode:2012Sci...335.1058H. doi:10.1126/science.1208277. PMID 22383840.
- ^ Gruber, N. (2011-04-18). "Warming up, turning sour, losing breath: ocean biogeochemistry under global change". Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 369 (1943): 1980–1996. doi:10.1098/rsta.2011.0003.
- ^ IPCC AR5 WG1 (2013). PDF Summary for policymakers.
- ^ Impact from the Deep; October 2006; Scientific American Magazine; by Peter D. Ward; 8 Page(s)
- ^ Tom Garrison. "Oceanography: An Invitation to Marine Science" 5th edition. Thomson, 2005. Page 4.
Further reading
- Hamblin, Jacob Darwin (2005) Oceanographers and the Cold War: Disciples of Marine Science. University of Washington Press. ISBN 978-0-295-98482-7
- Steele, J., K. Turekian and S. Thorpe. (2001). Encyclopedia of Ocean Sciences. San Diego: Academic Press. (6 vols.) ISBN 0-12-227430-X
- Sverdrup, Keith A., Duxbury, Alyn C., Duxbury, Alison B. (2006). Fundamentals of Oceanography, McGraw-Hill, ISBN 0-07-282678-9.
- Lang, Michael A., Ian G. Macintyre, and Klaus Rützler, eds. Proceedings of the Smithsonian Marine Science Symposium. Smithsonian Contributions to the Marine Sciences, no. 38. Washington, D.C.: Smithsonian Institution Scholarly Press, 2009.
External links
| Wikisource has the text of the 1922 Encyclopædia Britannica article Oceanography. |
| Wikimedia Commons has media related to Oceanography. |
- NASA Jet Propulsion Laboratory - Physical Oceanography Distributed Active Archive Center (PO.DAAC). A data center responsible for archiving and distributing data about the physical state of the ocean.
- Scripps Institution of Oceanography. One of the world's oldest, largest, and most important centers for ocean and Earth science research, education, and public service in the world.
- Woods Hole Oceanographic Institution (WHOI). One of the world's largest private, non-profit ocean research, engineering and education organization.
- British Oceanographic Data Centre. A source of oceanographic data and information.
- NOAA Ocean and Weather Data Navigator. Plot and download ocean data.
- Freeview Video 'Voyage to the Bottom of the Deep Deep Sea' Oceanography Programme by the Vega Science Trust and the BBC/Open University.
- Atlas of Spanish Oceanography by InvestigAdHoc.
- Glossary of Physical Oceanography and Related Disciplines by Steven K. Baum, Department of Oceanography, Texas A&M University
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English Journal
- CpG ODNs induced autophagy via reactive oxygen species (ROS) in Chinese mitten crab, Eriocheir sinensis.
- Sun M1, Wang L2, Jiang S2, Liu R2, Zhao D3, Chen H1, Song X1, Song L4.
- Developmental and comparative immunology.Dev Comp Immunol.2015 Sep;52(1):1-9. doi: 10.1016/j.dci.2015.04.008. Epub 2015 Apr 23.
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- Zou P1, Li K2, Liu S3, Xing R2, Qin Y2, Yu H2, Zhou M1, Li P4.
- Carbohydrate polymers.Carbohydr Polym.2015 Aug 1;126:62-9. doi: 10.1016/j.carbpol.2015.03.028. Epub 2015 Mar 21.
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Japanese Journal
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