Abstract
The Equatorial Mode (EM) governs the tropical Atlantic inter-annual variability during boreal summer. It has profound impacts on the climate of adjacent and remote areas. However, predicting the EM is one of the most challenging and intriguing issues for the scientific community. Recent studies have suggested a possible connection between the boreal spring Meridional Mode (MM) and the EM through ocean wave propagation. Here, we use a set of sensitivity experiments with a medium-resolution ocean model to determine the precursor role of a MM to create equatorial SST variability. Our results demonstrate that boreal summer equatorial SSTs following a MM, are subject to two counteracting effects: the local wind forcing and remotely-excited oceanic waves. For a positive MM, the anomalous easterly winds blowing along the equator, shallow the thermocline, cooling the sea surface via vertical diffusion and meridional advection. Anomalous wind curl excites a downwelling Rossby wave north of equator, which is reflected at the western boundary becoming an equatorial Kelvin wave (KW). This downwelling KW propagates eastward, deepening the thermocline and activating the thermocline feedbacks responsible for the equatorial warming. Moreover, the local wind forcing and RW-reflected mechanism have a significant and comparable impact on the equatorial SST variability. Changes in the intensity and persistence of these distinct forcings will determine the equatorial SST response during boreal summer. Our results give a step forward to the improvement of the EM predictability.
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References
Amaya DJ, DeFlorio MJ, Miller AJ, Xie S-P (2016) WES feedback and the Atlantic Meridional Mode: observations and CMIP5 comparisons. Clim Dyn 49(5–6):1665–1679
Andreoli RV, Kayano MT (2003) Evolution of the equatorial and dipole modes of the sea-surface temperature in the Tropical Atlantic at decadal scale. Meteorol Atmos Phys 83:277–285
Bjerknes J (1969) Atmospheric teleconnections from the equatorial Pacific. Mon Weather Rev 97:163–172
Brandt P, Funk A, Hormann V, Dengler M, Greatbatch RJ, Toole JM (2011) Interannual atmospheric variability forced by the deep equatorial Atlantic Ocean. Nature 473:497
Brodeau L, Barnier B, Treguier AM, Penduff T, Gulev S (2010) An ERA40-based atmospheric forcing for global ocean circulation models. Ocean Model 31:88–104
Burmeister K, Brandt P, Lübbecke J (2016) Revisiting the cause of the eastern equatorial Atlantic cold event in 2009. J Geophys Res Oceans 121:4777–4789
Butterworth S (1930) On the theory of filter amplifiers. Exp Wirel Wirel Eng 7:536–541
Carton JA, Huang B (1994) Warm events in the Tropical Atlantic. J Phys Oceanogr 24:888–903
Carton JA., Cao X, Giese BS, Da Silva AM (1996) Decadal and interannual SST variability in the tropical Atlantic Ocean. J Phys Oceanogr 26(7):1165–1175
Chang P, Ji L, Li H (1997) A decadal climate variation in the tropical Atlantic Ocean from thermodynamic air-sea interactions. Nature 385(6616):516
Czaja A, Van der Vaart P, Marshall J (2002) A diagnostic study of the role of remote forcing in Tropical Atlantic variability. J Clim 15:3280–3290
Faye S, Lazar A, Sow B, Gaye A (2015) A model study of the seasonality of sea surface temperature and circulation in the Atlantic North-eastern Tropical Upwelling System. Front Phys 3:76
Foltz GR, McPhaden MJ (2010a) Interaction between the Atlantic meridional and Niño modes. Geophys Res Lett 37:L18604. https://doi.org/10.1029/2010GL044001
Foltz GR, McPhaden MJ (2010b) Abrupt equatorial wave-induced cooling of the Atlantic cold tongue in 2009. Geophys Res Lett. https://doi.org/10.1029/2010GL045522
Foltz GR, Grodsky SA, Carton JA, McPhaden MJ (2003) Seasonal mixed layer heat budget of the tropical Atlantic Ocean. J Geophys Res Oceans 108:3146
Handoh IC, Bigg GR, Matthews AJ, Stevens DP (2006) Interannual variability of the Tropical Atlantic independent of and associated with ENSO: Part II. The South Tropical Atlantic. Int J Climatol 26:1957–1976
Huang B, Shukla J (1997) Characteristics of the interannual and decadal variability in a general circulation model of the Tropical Atlantic Ocean. J Phys Oceanogr 27:1693–1712
Illig S et al (2004) Interannual long equatorial waves in the tropical Atlantic from a high-resolution ocean general circulation model experiment in 1981–2000. J Geophys Res Oceans. https://doi.org/10.1029/2003JC001771
Jin D, Huo L (2018) Influence of tropical Atlantic sea surface temperature anomalies on the East Asian summer monsoon. Q J R Meteorol Soc 144:1490–1500
Jouanno J, Hernandez O, Sanchez-Gomez E (2017) Equatorial Atlantic interannual variability and its relation to dynamic and thermodynamic processes. Earth Syst Dyn 8:1061–1069
Keenlyside NS, Latif M (2007) Understanding equatorial Atlantic interannual variability. J Clim 20:131–142
Kucharski F, Bracco A, Yoo JH, Molteni F (2008) Atlantic forced component of the Indian monsoon interannual variability. Geophys Res Lett 35:L04706
Kucharski F, Bracco A, Yoo JH, Tompkins AM, Feudale L, Ruti P, Dell’Aquila A (2009) A Gill–Matsuno-type mechanism explains the tropical Atlantic influence on African and Indian monsoon rainfall. Q J R Meteorol Soc 135:569–579
Latif M, Grötzner A (2000) The equatorial Atlantic oscillation and its response to ENSO. Clim Dyn 16:213–218
Losada T, Rodríguez-Fonseca B, Kucharski F (2012a) Tropical influence on the summer Mediterranean climate. Atmos Sci Lett 13:36–42
Losada T, Rodriguez-Fonseca B, Mohino E, Bader J, Janicot S, Mechoso CR (2012b) Tropical SST and Sahel rainfall: a non-stationary relationship. Geophys Res Lett 39:L12705
Lübbecke J, McPhaden MJ (2012) On the inconsistent relationship between Pacific and Atlantic Niños. J Clim 25:4294–4303
Lübbecke JF, McPhaden MJ (2013) A comparative stability analysis of Atlantic and Pacific Niño modes. J Clim 26:5965–5980
Lübbecke J, Böning CW, Keenlyside NS, Xie S-P (2010) On the connection between Benguela and equatorial Atlantic Niños and the role of the South Atlantic anticyclone. J Geophys Res Oceans 115:C09015
Lübbecke J, Rodríguez-Fonseca B, Richter I, Martín-Rey M, Losada T, Polo I, Keenlyside N (2018) Equatorial Atlantic variability—modes, mechanisms and global teleconnections. WIREs Clim Change 9(4):e527. https://doi.org/10.1002/wcc.527
Madec G (2008) NEMO ocean engine, Note du Pole de modèlisation
Martín-Rey M, Rodríguez-Fonseca B, Polo I, Kucharski F (2014) On the Atlantic-Pacific Niños connection: a multidecadal modulated mode. Clim Dyn 43:3163–3178
Martín-Rey M, Rodríguez-Fonseca B, Polo I (2015) Atlantic opportunities for ENSO prediction. Geophys Res Lett 42:6802–6810
Martín-Rey M, Polo I, Rodríguez-Fonseca B, Lazar A, Losada T (2019) Ocean dynamics shapes the structure and timing of tropical Atlantic variability modes. Geophys Res Lett (under review)
Mohino E, Losada T (2015) Impacts of the Atlantic equatorial mode in a warmer climate. Clim Dyn 45:2255–2271
Murtugudde RG, Ballabrera-Poy J, Beauchamp J, Busalacchi AJ (2001) Relationship between zonal and meridional modes in the tropical Atlantic. Geophys Res Lett 28:4463–4466
Nnamchi H, Li J, Kucharski F, Kang I-S, Keenlyside NS, Chang P, Farneti R (2015) Thermodynamic controls of the Atlantic Niño. Nat Commun 6:8895
Nnamchi HC, Li J, Kucharski F, Kang IS, Keenlyside NS, Chang P, Farneti R (2016) An equatorial-extratropical dipole structure of the Atlantic Niño. J Clim 29:7295–7311
Nobre P, Shukla J (1996) Variations in sea surface temperatura, wind stress, and rainfall over the tropical Atlantic and South America. J Clim 9:2464–2479
Peter A-C et al (2006) A model study of the seasonal mixed layer heat budget in the equatorial Atlantic. J Geophys Res Oceans 111:C06014
Polo I, Rodríguez-Fonseca B, Losada T, García-Serrano J (2008a) Tropical Atlantic variability modes (1979–2002). Part I: time-evolving SST modes related to West African rainfall. J Clim 21:6457–6475
Polo I, Lazar A, Rodriguez-Fonseca B, Arnault S (2008b) Oceanic Kelvin waves and tropical Atlantic intraseasonal variability: 1. Kelvin wave characterization. J Geophys Res Oceans 113:07009
Polo I, Lazar A, Rodriguez-Fonseca B, Mignot J (2015a) Growth and decay of the equatorial Atlantic SST mode by means of closed heat budget in a coupled general circulation model. Front Earth Sci 3:37
Polo I, Martín-Rey M, Rodriguez-Fonseca B, Kucharski F, Mechoso C (2015b) Processes in the Pacific La Niña onset triggered by the Atlantic Niño. Clim Dyn 44:115–131
Rayner NA et al (2003) Global analyses of sea surface temperature, sea ice, and night marine air temperature since the late nineteenth century. J Geophys Res Atmos 108:4407
Richter I, Behera SK, Masumoto Y, Taguchi B, Sasaki H, Yamagata T (2013) Multiple causes of interannual sea surface temperature variability in the equatorial Atlantic Ocean. Nat Geosci 6:43–47
Rodríguez-Fonseca B, Polo I, García-Serrano J, Losada T, Mohino E, Mechoso CR, Kucharski F (2009) Are Atlantic Niños enhancing Pacific ENSO events in recent decades? Geophys Res Lett 36:L20705
Rodríguez-Fonseca B et al (2015) Variability and predictability of West African droughts: a review on the role of sea surface temperature anomalies. J Clim 28:4034–4060
Ruiz-Barradas A, Carton JA, Nigam S (2000) Structure of interannual-to-decadal climate variability in the tropical Atlantic sector. J Clim 13:3285–3297
Servain J, Wainer I, McCreary JP, Dessier A (1999) Relationship between the equatorial and meridional modes of climatic variability in the tropical Atlantic. Geophys Res Lett 26:485–488
Suarez MJ, Schopf PS (1988) A delayed action oscillator for ENSO. J Atmos Sci 45:3283–3287
von Storch H, Zwiers F (2001) Statistical analysis in climate research. Cambridge University Press, Cambridge, p 484
Wagner RG (1996) Mechanisms controlling variability of the interhemispheric sea surface temperature gradient in the tropical Atlantic. J Clim 9(9):2010–2019
Zebiak SE (1993) Air–sea interaction in the equatorial Atlantic Region. J Clim 6:1567–1586
Zhu J, Huang B, Wu Z (2012) The role of ocean dynamics in the interaction between the Atlantic meridional and equatorial modes. J Clim 25:3583–3598
Acknowledgements
The research leading to these results received funding from the EU FP7/2007-2013 under Grant Agreement 603521 (PREFACE project), the MORDICUS grant under contract ANR-13-SENV-0002-01, CNES/EUMETSAT (CNES—DIA/TEC-2016.8595, EUM/LEO-JAS3/DOC/16/852054) and the MSCA-IF-EF-ST FESTIVAL (H2020-EU project 797236). The observed SSTs from HadISST dataset were provided by the MetOffice Hadley Centre, from its website at https://www.metoffice.gov.uk/hadobs/hadisst/. The data from the INTER, MM-REF, MM-WIND and MM-WAVE simulations are available from the authors upon request.
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Martín-Rey, M., Lazar, A. Is the boreal spring tropical Atlantic variability a precursor of the Equatorial Mode?. Clim Dyn 53, 2339–2353 (2019). https://doi.org/10.1007/s00382-019-04851-9
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DOI: https://doi.org/10.1007/s00382-019-04851-9