North Brazil Current Retroflection

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Schematic map of the Atlantic ocean and its surface currents. The NBC rings are formed as the NBC retroflects towards the NECC. Inspired from. Schematic map North brazil Current retroflection and rings.png
Schematic map of the Atlantic ocean and its surface currents. The NBC rings are formed as the NBC retroflects towards the NECC. Inspired from.

The North Brazil Current (NBC) retroflects north-eastwards and merges into the North Equatorial Counter Current (NECC). [2] The retroflection occurs in a seasonal pattern when there is strong retroflection from late summer to early winter (borreal fall). There is weakened or no retroflection during other times of the year. Just like in the Agulhas Current, the retroflection also sheds some eddies (which are referred to as the NBC rings) that make their way to the Caribbean Sea through the Lesser Antilles. [1]

Contents

Retroflection

Retroflection of the NBC occurs off the coastal border between Brazil and Guyana between 4ºN to 7ºN and 48ºW to 50ºW. [3] The NBC begins just off the coast of north-eastern Brazil, approximately around 10ºS and 31ºW where the central South Equatorial Current (cSEC) bifurcates into two. The branch that separates southward along the South American continent is called Brazil Current (BC) and the branch that flows northward is called the NBC. [4] The North Brazil Undercurrent (NBUC), which flows in the sub-surface along with the NBC, retroflects as well. However, before the retroflection, there are multiple points of bifurcation along its trajectory. [5] From its origin, it branches off to feed into the South Equatorial Undercurrent (SEUC), the Equatorial Undercurrent (EUC), and finally retroflects to mix with the North Equatorial Undercurrent (NEUC).

The NBC and the North Brazil Undercurrent (NBUC) combined carry a volume of approx. 35 Sv. [5] Approximately, a total of 28 Sv. of water is turned back because of the retroflection. [5] The water at the surface merges with the NECC while the sub-surface water merges into the NEUC. The remaining water can be attributed to the formation of rings and some leakage into the Caribbean Current (CC). [3]

Ring Formation

Animation of the North Brazil Current (NBC) retroflection and ring formation. The rings and retroflection are present only from summer to late winter. Period Nov 1998 to May 2000. Data from GLORYS12V1 product of the Copernicus Marine Service. MygifCurrent.gif
Animation of the North Brazil Current (NBC) retroflection and ring formation. The rings and retroflection are present only from summer to late winter. Period Nov 1998 to May 2000. Data from GLORYS12V1 product of the Copernicus Marine Service.

When the NBC is stronger, the retroflection sheds off anticyclonic rings and they propagate along the coast and head towards the Lesser Antilles. Upon contact with the islands, their coherent structure is either reduced or completely destroyed. [7] These rings originate as a result of the retroflection. The retroflection is so severe that the bulge created breaks off and form anticyclonic rings. So, the maximum number of rings are formed when the retroflection is the strongest. The rings show early signs of formation because the baroclinic instability grows in the region and a wavelike perturbation can be seen from early fall. [8] On average, there are 6 rings generated every year with a minimum of 2-3 rings per year. [8]

However, the mechanisms that contribute to the NBC ring formation and how the dynamics of this generation of rings work are not fully understood. [9] Nonetheless, the properties such as the diameter, lifetime, velocity, etc. are well documented. [10] The rings are recorded using surface drifters, satellite observations of altimetry and color scanners. [10] They are also known to be the largest and lowest-latitude rings that originate from any Western Boundary Current. [9]

Physical properties

NBC rings are characterised by a partly isolated warm-core that can be as large as 450 km of diameter which turns clockwise with an azimuthal speed around 1 m/s. [10] The maximum speed of propagation is observed at the surface but the vertical structure goes even deeper than the thermocline. [10] These rings travel from their area of formation, between 5ºN to 8ºN and 50ºW to 53ºW, until the Lesser Antilles and disperse into the Caribbean Sea. The life span of these rings are typically of 3–4 months and they travel at 8–16 cm/s northwestward. They carry around 1-2 Sv. each ring and are responsible of a total of 6-7 Sv. of water transport towards the islands. [9] At this latitude, NBC rings are responsible for 20% of the total meridional heat transport by the ocean. [11] They are also responsible for the direct mass transport of the Atlantic meridional overturning circulation (AMOC), which accounts for 20-25% of the total upper ocean cross-gyre transport. [11]

Impacts of the NBC rings

The rings play a big role in the mass and heat transport in the equatorial-tropical gyre. [12] The NBC and its rings also bring in nutrient-rich and fresh water from the Amazon River. As the NBC rings are formed near the mouth of the Amazon, these rings act as a vehicle of transport for the freshwater up to the Caribbean Sea. These water masses with low salinity drift in the sea for a long period of time before they are mixed. This process takes around 100 days after the ring formation. [13]

When these anticyclonic rings make contact with the eastern Caribbean, they cause a disturbance in the circulation pattern of the water and the less saline water affects the local fishery. [12] Larvae fish appeared to be pushed away from their natural habitat which resulted in failure of settlement in the eastern borders of Barbados. [14] This creates a need for migration for the local larvae fish population to other areas in the Caribbean. The fish also suffered from reduced growth rates and reduced survival rates. [14]

Map of the Undercurrents in the Atlantic ocean over the eastern border of Brazil. The yellow line representing the surface current and the NBC, while the green lines depicting the undercurrents. Deep currents of the Brazilian coast.png
Map of the Undercurrents in the Atlantic ocean over the eastern border of Brazil. The yellow line representing the surface current and the NBC, while the green lines depicting the undercurrents.

North Brazil Undercurrent

Formation and Trajectory

North Brazil Undercurrent (NBUC) begins much more to the south than the NBC. The NBUC is an extension from the sub-surface current of the southern South Equatorial Current (sSEC). The sSEC travels to the South American continent because of the westward deflection of the Benguela Current from the southeast Atlantic Ocean. [15] When sSEC reaches the Eastern Coast of Brazil, around 15ºS to 20ºS, it splits into two with the northern branch of the bifurcation forming the NBUC. [15]

The core of the flow is 250m deep and the NBUC transports about 24 Sv. (in the upper 1000m) up the Eastern Coast of Brazil. [5] After the northward trajectory reaches 5ºS, the central South Equatorial Current (cSEC) merges with the NBUC, feeding approx. 11 Sv. more. [5] This trajectory continues along the northern coast of Brazil until the NBUC retroflects.

Bifurcations and Retroflection

Because of the ocean floor topography, the North Brazil Undercurrent (NBUC) retroflects just before the NBC. [16] All of the water carried by the NBUC retroflects completely into the North Equatorial Undercurrent (NEUC). But along its trajectory there are ample points of bifurcation. The bifurcations, even though they transport very little water mass, [17] help understand the mapping of the ocean in the west-Atlantic. First, there is observation of bifurcation at 5ºS towards the South Equatorial Undercurrent (SEUC). [18] After splitting to mix with the SEUC, at about 2ºS, the current birfurcates after moving north and merges with the Equatorial Undercurrent (EUC). Then finally, at around 3ºN, the NBUC retroflexes and merges completely with the North Equatorial Undercurrent (EUC). [16]

Related Research Articles

<span class="mw-page-title-main">Agulhas Current</span> Western boundary current of the southwest Indian Ocean that flows down the east coast of Africa

The Agulhas Current is the western boundary current of the southwest Indian Ocean. It flows south along the east coast of Africa from 27°S to 40°S. It is narrow, swift and strong. It is suggested that it is the largest western boundary current in the world ocean, with an estimated net transport of 70 sverdrups, as western boundary currents at comparable latitudes transport less — Brazil Current, Gulf Stream, Kuroshio.

<span class="mw-page-title-main">Kuroshio Current</span> North flowing ocean current on the west side of the North Pacific Ocean

The Kuroshio Current, also known as the Black Current or Japan Current is a north-flowing, warm ocean current on the west side of the North Pacific Ocean basin. It was named for the deep blue appearance of its waters. Similar to the Gulf Stream in the North Atlantic, the Kuroshio is a powerful western boundary current that transports warm equatorial water poleward and forms the western limb of the North Pacific Subtropical Gyre. Off the East Coast of Japan, it merges with the Oyashio Current to form the North Pacific Current.

<span class="mw-page-title-main">Labrador Current</span> Cold current in the Atlantic ocean along the coasts of Labrador, Newfoundland and Nova Scotia

The Labrador Current is a cold current in the North Atlantic Ocean which flows from the Arctic Ocean south along the coast of Labrador and passes around Newfoundland, continuing south along the east coast of Canada near Nova Scotia. Near Nova Scotia, this cold water current meets the warm northward moving Gulf Stream. The combination of these two currents produces heavy fogs and has also created one of the richest fishing grounds in the world.

The North Equatorial Current (NEC) is a westward wind-driven current mostly located near the equator, but the location varies from different oceans. The NEC in the Pacific and the Atlantic is about 5°-20°N, while the NEC in the Indian Ocean is very close to the equator. It ranges from the sea surface down to 400 m in the western Pacific.

<span class="mw-page-title-main">Equatorial Counter Current</span> Shallow eastward flowing current found in the Atlantic, Indian, and Pacific Oceans

The Equatorial Counter Current is an eastward flowing, wind-driven current which extends to depths of 100–150 metres (330–490 ft) in the Atlantic, Indian, and Pacific Oceans. More often called the North Equatorial Countercurrent (NECC), this current flows west-to-east at about 3-10°N in the Atlantic, Indian Ocean and Pacific basins, between the North Equatorial Current (NEC) and the South Equatorial Current (SEC). The NECC is not to be confused with the Equatorial Undercurrent (EUC) that flows eastward along the equator at depths around 200 metres (660 ft) in the western Pacific rising to 100 metres (330 ft) in the eastern Pacific.

The North Brazil Current (NBC) is a warm water ocean current that is part of the southwestern North Atlantic Gyre. It begins when the westward moving Atlantic South Equatorial Current splits in half and flows northwestward, following the coastline of north Brazil. It ends at the border of Brazil and Guiana, where it is renamed the Guiana Current. It is predominantly a salt water current, but it does help transport fresh water from the Amazon River northward.

<span class="mw-page-title-main">Mindanao Current</span> Narrow, southward-flowing ocean current along the southeastern coast of the Philippines

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Retroflection is the movement of an ocean current that doubles back on itself.

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References

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  2. ↑ Metcalf, W. G.; Stalcup, M. C. (1967-10-15). "Origin of the Atlantic Equatorial Undercurrent". Journal of Geophysical Research. 72 (20): 4959–4975. Bibcode:1967JGR....72.4959M. doi:10.1029/jz072i020p04959. ISSN   0148-0227.
  3. 1 2 Garzoli, Silvia L. (2004). "North Brazil Current retroflection and transports". Journal of Geophysical Research. 109 (C1). Bibcode:2004JGRC..109.1013G. doi: 10.1029/2003jc001775 . ISSN   0148-0227.
  4. ↑ da Silveira, Ilson C. A.; de Miranda, Luiz B.; Brown, Wendell S. (1994). "On the origins of the North Brazil Current". Journal of Geophysical Research. 99 (C11): 22501. Bibcode:1994JGR....9922501D. doi:10.1029/94jc01776. ISSN   0148-0227.
  5. 1 2 3 4 5 6 Schott, Friedrich A.; Fischer, Jürgen; Stramma, Lothar (October 1998). "Transports and Pathways of the Upper-Layer Circulation in the Western Tropical Atlantic". Journal of Physical Oceanography. 28 (10): 1904–1928. Bibcode:1998JPO....28.1904S. doi: 10.1175/1520-0485(1998)028<1904:TAPOTU>2.0.CO;2 . S2CID   53317039.
  6. ↑ European Union-Copernicus Marine Service (2018). "Data | Copernicus Marine". resources.marine.copernicus.eu. doi:10.48670/moi-00021 . Retrieved 2022-04-01.
  7. ↑ Barnier, Bernard; Reynaud, Thierry; Beckmann, Aike; Böning, Claus; Molines, Jean-Marc; Barnard, Sally; Jia, Yanli (January 2001). "On the seasonal variability and eddies in the North Brazil Current: insights from model intercomparison experiments". Progress in Oceanography. 48 (2–3): 195–230. Bibcode:2001PrOce..48..195B. doi:10.1016/s0079-6611(01)00005-2.
  8. 1 2 Glickson, Deborah A.; Fratantoni, David M.; Wooding, Christine M.; Richardson, Philip L. (2000). North Brazil Current Rings Experiment : surface drifter data report, November 1998-June 2000. Woods Hole, MA: Woods Hole Oceanographic Institution. doi:10.1575/1912/95. hdl:1912/95.
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  10. 1 2 3 4 Jochum, Markus; Malanotte-Rizzoli, Paola (2003-03-01). "On the generation of North Brazil Current rings". Journal of Marine Research. 61 (2): 147–173. doi:10.1357/002224003322005050.
  11. 1 2 Fratantoni, David M.; Johns, William E.; Townsend, Tamara L. (1995). "Rings of the North Brazil Current: Their structure and behavior inferred from observations and a numerical simulation". Journal of Geophysical Research. 100 (C6): 10633. Bibcode:1995JGR...10010633F. doi:10.1029/95jc00925. ISSN   0148-0227.
  12. 1 2 Cowen, R.K.; Sponaugle, S.; Paris, C.B.; Fortuna, J.L.; Lwiza, K.M.M.; Dorsey, S. (2003), "Impact of North Brazil Current rings on local circulation and coral reef fish recruitment to Barbados, West Indies", Interhemispheric Water Exchange in the Atlantic Ocean, Elsevier Oceanography Series, Elsevier, vol. 68, pp. 443–462, doi:10.1016/s0422-9894(03)80157-5, ISBN   9780444512673 , retrieved 2022-04-08
  13. ↑ Kelly, Peter S.; Lwiza, Kamazima M. M.; Cowen, Robert K.; Goni, Gustavo J. (2000-08-15). "Low-salinity pools at Barbados, West Indies: Their origin, frequency, and variability". Journal of Geophysical Research: Oceans. 105 (C8): 19699–19708. Bibcode:2000JGR...10519699K. doi: 10.1029/1999jc900328 . ISSN   0148-0227.
  14. 1 2 Cowen, R.K.; Sponaugle, S.; Paris, C.B.; Fortuna, J.L.; Lwiza, K.M.M.; Dorsey, S. (2003), "Impact of North Brazil Current rings on local circulation and coral reef fish recruitment to Barbados, West Indies", Interhemispheric Water Exchange in the Atlantic Ocean, Elsevier Oceanography Series, Elsevier, vol. 68, pp. 443–462, doi:10.1016/s0422-9894(03)80157-5, ISBN   9780444512673 , retrieved 2022-03-25
  15. 1 2 Stramma, Lothar; England, Matthew (1999-09-15). "On the water masses and mean circulation of the South Atlantic Ocean". Journal of Geophysical Research: Oceans. 104 (C9): 20863–20883. Bibcode:1999JGR...10420863S. doi:10.1029/1999jc900139. ISSN   0148-0227.
  16. 1 2 Goes, Marlos; Molinari, Robert; da Silveira, Ilson; Wainer, Ilana (April 2005). "Retroflections of the North Brazil Current during February 2002". Deep Sea Research Part I: Oceanographic Research Papers. 52 (4): 647–667. Bibcode:2005DSRI...52..647G. doi:10.1016/j.dsr.2004.10.010. ISSN   0967-0637.
  17. ↑ Dossa, Alina N.; Silva, Alex C.; Chaigneau, Alexis; Eldin, Gérard; Araujo, Moacyr; Bertrand, Arnaud (January 2021). "Near-surface western boundary circulation off Northeast Brazil". Progress in Oceanography. 190: 102475. Bibcode:2021PrOce.19002475D. doi:10.1016/j.pocean.2020.102475. ISSN   0079-6611. S2CID   228853927.
  18. ↑ Stramma, Lothar; Fischer, Jürgen; Reppin, Jörg (1995-05-01). "The North Brazil Undercurrent". Deep Sea Research Part I: Oceanographic Research Papers. 42 (5): 773–795. Bibcode:1995DSRI...42..773S. doi:10.1016/0967-0637(95)00014-W. ISSN   0967-0637.
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