Role of interannual K elvin wave propagations in the equatorial A tlantic on the A ngola B enguela C urrent system
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The link between equatorial Atlantic Ocean variability and the coastal region of Angola‐Namibia is investigated at interannual time scales from 1998 to 2012. An index of equatorial Kelvin wave activity is defined based on Prediction and Research Moored Array in the Tropical Atlantic (PIRATA). Along the equator, results show a significant correlation between interannual PIRATA monthly dynamic height anomalies, altimetric monthly Sea Surface Height Anomalies (SSHA), and SSHA calculated with an Ocean Linear Model. This allows us to interpret PIRATA records in terms of equatorial Kelvin waves. Estimated phase speed of eastward propagations from PIRATA equatorial mooring remains in agreement with the linear theory, emphasizing the dominance of the second baroclinic mode. Systematic analysis of all strong interannual equatorial SSHA shows that they precede by 1–2 months extreme interannual Sea Surface Temperature Anomalies along the African coast, which confirms the hypothesis that major warm and cold events in the Angola‐Benguela current system are remotely forced by ocean atmosphere interactions in the equatorial Atlantic. Equatorial wave dynamics is at the origin of their developments. Wind anomalies in the Western Equatorial Atlantic force equatorial downwelling and upwelling Kelvin waves that propagate eastward along the equator and then poleward along the African coast triggering extreme warm and cold events, respectively. A proxy index based on linear ocean dynamics appears to be significantly more correlated with coastal variability than an index based on wind variability. Results show a seasonal phasing, with significantly higher correlations between our equatorial index and coastal SSTA in October–April season.
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In models, interannual variations of temperature, nitrate, and oxygen concentrations along the southwestern coast of Africa are primarily controlled by oceanic teleconnections associated with equatorial wave variability and along-shore water mass transport.
“In models, interannual variations of temperature, nitrate, and oxygen concentrations along the southwestern coast of Africa are primarily controlled by oceanic teleconnections associated with equatorial wave variability and along-shore water mass transport (Mohrholz et al., 2008;Bachèlery, 2016;Bachèlery et al., 2016a,b;Koungue et al., 2017).”
From The tropical atlantic observing system (2019) · cites this paper as Koungue et al., 2017
The Introduction reports modeling results in which equatorial remote forcing explains more than 80% of interannual coastal sea-surface temperature, nitrate, and oxygen variability. The Summary, Discussion, and Conclusions discusses advection of water masses but says its importance at interannual timescales is difficult to assess; it does not establish along-shore transport as a primary control. (LLM, conf=0.86)
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References 33 · Cited by 48
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- Bache `lery, M.-L., S. Illig, and I. Dadou (2015), Interannual variability in the South-East Atlantic Ocean, focusing on the Benguela Upwelling System: Remote versus local forcing, J. Geophys. Res. Oceans, 120, 284-310, doi:10.1002/2015JC011168. · DOI · Paper page
- Bache `lery, M.-L., S. Illig and I. Dadou (2016), Forcings of nutrient, oxygen and primary production interannual variability in the South-East Atlantic Ocean, Geophys. Res. Lett., 43, 8617-8625, doi:10.1002/2016GL070288. · DOI
- Blamey, L. K., et al. (2015) Ecosystem change in the southern Benguela and the underlying processes, J. Mar. Syst., 144, 9-29, doi:10.1016/ j.jmarsys.2014.11.006. · DOI
- Bourle `s, B., et al. (2008), The Pirata program, Bull. Am. Meteorol. Soc., 89(8), 1111.
- Burmeister, K., P. Brandt, and J. F. L€ ubbecke (2016), Revisiting the cause of the eastern equatorial Atlantic cold event in 2009, J. Geophys. Res. Oceans, 121, 4777-4789, doi:10.1002/2016JC011719. · DOI
- Ducet, N., P. Y. Le Traon, and G. Reverdin (2000), Global high-resolution mapping of ocean circulation from TOPEX/Poseidon and ERS-1 and-2, J. Geophys. Res., 105(C8), 19,477-19,498, doi:10.1029/2000JC900063. · DOI · Paper page
- Foltz, G. R., and M. J. McPhaden (2010a), Interaction between the Atlantic meridional and Niño modes, Geophys. Res. Lett., 37, L18604, doi: 10.1029/2010GL044001. · DOI · Paper page
- Foltz, G. R., and M. J. McPhaden (2010b), Abrupt equatorial wave-induced cooling of the Atlantic cold tongue in 2009, Geophys. Res. Lett., 37, L24605, doi:10.1029/2010GL045522. · DOI
- Goubanova K., S. Illig, E. Machu, V. Garc¸on, and B. Dewitte (2013), SST subseasonal variability in the Benguela upwelling system as inferred from satellite observations (2000-2008), J. Geophys.Res. Oceans, 118, 4092-4110, doi:10.1002/jgrc.20287. · DOI
- Hormann, V., and P. Brandt (2009), Upper equatorial Atlantic variability during 2002 and 2005 associated with equatorial Kelvin waves, J. Geophys. Res., 114, C03007, doi:10.1029/2008JC005101. · DOI
- Illig, S., and B. Dewitte (2006), Local coupled equatorial variability versus remote ENSO forcing in an intermediate coupled model of the tropical Atlantic, J. Clim., 19(20), 5227-5252.
- Illig, S., D. Gushchina, B. Dewitte, N. Ayoub, and Y. du Penhoat (2006), The 1996 equatorial Atlantic warm event: Origin and mechanisms, Geophys. Res. Lett., 33, L09701, doi:10.1029/2005GL025632. · DOI
- Le Traon, P. Y., F. Nadal, and N. Ducet (1998), An improved mapping method of multisatellite altimeter data, J. Atmos. Oceanic Technol., 15(2), 522-534, doi:10.1175/1520-0426. · DOI
- L€ ubbecke, J. F., C. W. B€ oning, N. S. Keenlyside, and S.-P. Xie (2010), On the connection between Benguela and equatorial Atlantic Niños and the role of the South Atlantic Anticyclone, J. Geophys. Res., 115, C09015, doi:10.1029/2009JC005964. · DOI · Paper page
- Marin, F., G. Caniaux, H. Giordani, B. Bourles, Y. Gouriou, and E. Key (2009), Why were sea surface temperatures so different in the eastern equatorial Atlantic in June 2005 and 2006?, J. Phys. Oceanogr., 39(6), 1416-1431, doi:10.1175/2008JPO4030. · DOI · Paper page
- Mohrholz, V., M. Schmidt, and J. R. E. Lutjeharms (2001),The hydrography and dynamics of the Angola-Benguela frontal zone and environ- ment in April 1999, South Afr. J. Sci., 97, 199-208. · DOI · Paper page
- Ostrowski, M., J. C. B. da Silva, and B. Bazik-Sangolay (2009), The response of sound scatterers to El Niño-and La Niña-like oceanographic regimes in the southeastern Atlantic, ICES J. Mar. Sci.,66(6), 1063-1072, doi:10.1093/icesjms/fsp102. · DOI
- Polo, I., A. Lazar, B. Rodriguez-Fonseca, and S. Arnault (2008), Oceanic Kelvin waves and tropical Atlantic intraseasonal variability: 1. Kelvin wave characterization, J. Geophys. Res., 113, C07009, doi:10.1029/2007JC004495. · DOI
- Reynolds, R. W., N. A. Rayner, T. M. Smith, D. C. Stokes, and W. Wang (2002), An improved in situ and satellite SST analysis for climate, J. Clim., 15, 1609-1625, doi:10.1175/1520-0442(2002)015 < 1609:AIISAS> 2.0.CO;2. · DOI
- Richter, I., S. K. Behera, Y. Masumoto, B. Taguchi, N. Komori, and T. Yamagata (2010), On the triggering of Benguela Ninos: Remote equato- rial versus local influences, Geophys. Res. Lett., 37, L20604, doi:10.1029/2010GL044461. · DOI
- Rouault, M. (2012), Bi-annual intrusion of tropical water in the northern Benguela upwelling, Geophys. Res. Lett., 39, L12606, doi:10.1029/ 2012GL052099. · DOI
- Rouault, M., P. Florenchie, N. Fauchereau, and C. J. C. Reason (2003), South east tropical Atlantic warm events and southern African rainfall, Geophys. Res. Lett., 30(5), 8009, doi:10.1029/2002GL014840. · DOI
- Rouault, M., J. Servain, C. J. C. Reason, B. Bourle `s, M. J. Rouault, and N. Fauchereau (2009), Extension of PIRATA in the tropical South-East Atlantic: An initial one-year experiment, Afr. J. Mar. Sci., 31(1), 63-71, doi:10.2989/AJMS.2009.31.1.5.776. · DOI
- Servain, J., A. Busalacchi, M. J. McPhaden, and D. Moura (1998), A pilot research moored array in the tropical Atlantic (PIRATA), Bull. Am. Meteorol. Soc., 79(10), 2019-2031.
- Shannon, L. V., A. J. Boyd, G. B. Brundrit and J. Taunton-Clark (1986), On the existence of an El Niño-type phenomenon in the Benguela sys- tem, J. Mar. Res. 44(3), 495-520.
- Xie, S.-P., and J. A. Carton (2004), Tropical Atlantic variability: Patterns, mechanisms, and impacts, in Earth Climate: The Ocean-Atmosphere Interaction, Geophys. Monogr. Ser., vol. 147, edited by C. Wang, S.-P. Xie, and J. A. Carton, pp. 121-142, AGU, Washington, D. C. Journal of Geophysical Research: Oceans 10.1002/2016JC012463
- Authors
- Imbol Koungue, R. A., Illig, S., & Rouault, M.
- Affiliations
- Department of Oceanography MARE Institute, University of Cape Town Cape Town South Africa
- University of Cape Town (ZA)
- Corresponding author
- Rouault, Mathieu
- Venue
- Journal of Geophysical Research: Oceans
- Publisher
- American Geophysical Union (AGU)
- Published
- 2017-06
- Volume
- 122
- Issue
- 6
- Pages
- 4685-4703
- ISSN
- 2169-9275 (ISSN-L)
- 2169-9291
- OpenAlex
- W2611752423
- Cited by
- 48
- References
- 33
- Citations by year
- 2026: 3 · 2025: 4 · 2024: 10 · 2023: 8 · 2022: 2 · 2021: 4 · 2020: 4 · 2019: 7 · 2018: 5 · 2017: 1
- FWCI
- 3.09
- Type
- journal article
- Language
- en
- Open access
- bronze
- doi.org
- Locations
- Journal of Geophysical Research Oceans (publishedVersion)
- HAL (submittedVersion, other-oa)
- Institutional Archive of Ifremer (French Research Institute for Exploitation of the Sea) (submittedVersion, other-oa)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Oceanographic and Atmospheric Processes
- Physical Sciences › Environmental Science › Global and Planetary Change › Climate variability and models
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Meteorological Phenomena and Simulations
- Keywords
- equatorial Kelvin waves, interannual variability, sea level anomalies, ocean-atmosphere interaction, wind forcing, sea surface temperature anomalies
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