Ocean gyre

In oceanography, a gyre (/ˈaɪər/) is any large system of circulating ocean currents, particularly those involved with large wind movements. Gyres are caused by the Coriolis effect; planetary vorticity, horizontal friction and vertical friction determine the circulatory patterns from the wind stress curl (torque).[1]

The five major ocean gyres

Gyre can refer to any type of vortex in an atmosphere or a sea,[2] even one that is man-made, but it is most commonly used in terrestrial oceanography to refer to the major ocean systems.

Major gyresEdit

The following are the five most notable ocean gyres:[3]

Other gyresEdit

Tropical gyresEdit

 
All of the world's larger gyres

Tropical gyres are less unified and tend to be mostly east-west with minor north-south extent.

  • Atlantic Equatorial Current System (two counter-rotating circulations)[citation needed]
  • Pacific Equatorial Current System[citation needed]
  • Indian Monsoon Gyres (two counter-rotating circulations in northern Indian Ocean)[4]

Subtropical gyresEdit

The center of a subtropical gyre is a high pressure zone. Circulation around the high pressure is clockwise in the northern hemisphere and counterclockwise in the southern hemisphere, due to the Coriolis effect. The high pressure in the center is due to the westerly winds on the northern side of the gyre and easterly trade winds on the southern side. These cause frictional surface currents towards the latitude at the center of the gyre.

This build-up of water in the center creates flow towards the equator in the upper 1,000 to 2,000 m (3,300 to 6,600 ft) of the ocean, through rather complex dynamics. This flow is returned towards the pole in an intensified western boundary current. The boundary current of the North Atlantic Gyre is the Gulf Stream, of the North Pacific Gyre the Kuroshio Current, of the South Atlantic Gyre the Brazil Current, of the South Pacific Gyre the East Australian Current, and of the Indian Ocean Gyre the Agulhas Current.[citation needed]

Subpolar gyresEdit

Subpolar gyres form at high latitudes (around 60°). Circulation of surface wind and ocean water is counterclockwise in the Northern Hemisphere, around a low-pressure area, such as the persistent Aleutian Low and the Icelandic Low. Surface currents generally move outward from the center of the system. This drives the Ekman transport, which creates an upwelling of nutrient-rich water from the lower depths.[5]

Subpolar circulation in the southern hemisphere is dominated by the Antarctic Circumpolar Current, due to the lack of large landmasses breaking up the Southern Ocean. There are minor gyres in the Weddell Sea and the Ross Sea, the Weddell Gyre and Ross Gyre, which circulate in a clockwise direction.[3]

Climate changeEdit

Recently[when?], stronger winds, especially the subtropical trade winds in the Pacific ocean have provided a mechanism for vertical heat distribution[citation needed]. The effects are changes in the ocean currents, increasing the subtropical overturning, which are also related to the El Niño and La Niña phenomena. Depending on natural variability, during La Niña years around 30% more heat from the upper ocean layer is transported into the deeper ocean.[6] Several studies in recent years, found a multidecadal increase in OHC of the deep and upper ocean regions and attribute the heat uptake to anthropogenic warming.[7]

The influence of the Coriolis effect on westward intensificationEdit

 
Coriolis effect

PollutionEdit

Ocean gyres collect floating pollutants (and other flotsam).

The Great Pacific garbage patch in the central North Pacific Ocean is a gyre of marine debris particles and floating trash halfway between Hawaii and California. It covers an indeterminate large zone depending on plastic concentration chosen to define it. It is estimated 80,000 metric tons of plastic, totaling 1.8 trillion pieces. 92% of the mass is objects larger than 0.5 centimeters.

The North Atlantic garbage patch is a similar scale great patch. It is estimated to be hundreds of kilometers across, with a density of over 200,000 pieces of debris per square kilometer.

See alsoEdit

ReferencesEdit

  1. ^ Heinemann, B. and the Open University (1998) Ocean circulation, Oxford University Press: Page 98
  2. ^ Lissauer, Jack J.; de Pater, Imke (2019). Fundamental Planetary Sciences : physics, chemistry, and habitability. New York, NY, USA: Cambridge University Press. ISBN 9781108411981.
  3. ^ a b The five most notable gyres Archived 2016-03-04 at the Wayback Machine PowerPoint Presentation
  4. ^ Indian Monsoon Gyres
  5. ^ Wind Driven Surface Currents: Gyres
  6. ^ Balmaseda, Trenberth & Källén (2013). "Distinctive climate signals in reanalysis of global ocean heat content". Geophysical Research Letters. 40 (9): 1754–1759. Bibcode:2013GeoRL..40.1754B. doi:10.1002/grl.50382. Archived from the original on 2015-02-13. Retrieved 2013-09-26.
  7. ^ Abraham; et al. (2013). "A review of global ocean temperature observations: Implications for ocean heat content estimates and climate change". Reviews of Geophysics. 51 (3): 450–483. Bibcode:2013RvGeo..51..450A. CiteSeerX 10.1.1.594.3698. doi:10.1002/rog.20022.

External linksEdit