Abstract
Caribbean rainfall and associated regional-scale ocean–atmosphere anomalies are analyzed during and after warm pool (WP) and cold tongue (CT) El Niño (EN) events (i.e. from the usual peak of EN events in boreal winter to next summer from 1950 to 2011). During and after a CT event, a north–south dipolar pattern with positive (negative) rainfall anomalies over the northern (southern) Caribbean during the boreal winter tends to reverse in spring, and then to vanish in summer. On the contrary, during and after a WP event, weak rainfall anomalies during the boreal winter intensify themselves from spring, with anomalous wet conditions over most of the Caribbean basin observed during summer, except over the eastern coast of Nicaragua and Costa Rica. The Caribbean rainfall anomalies associated with WP and CT events are shaped by competition between at least four different, but interrelated, mechanisms; (1) the near-equatorial large-scale subsidence anomaly over the equatorial Atlantic linked to the zonal adjustment of the Walker circulation; (2) the extra-tropical wave-like train combining positive phase of the Pacific/North American mode and negative phase of the North Atlantic Oscillation; (3) the wind-evaporation-sea surface temperature (SST) positive feedback coupling warmer-than-normal SST with weaker-than-normal low level easterlies over the tropical North Atlantic; and (4) the air-sea coupling between the speed of low level easterlies, including the Caribbean low level jet, and the SST anomaly (SSTA) gradient between the Caribbean basin and the eastern equatorial Pacific. It seems that Caribbean rainfall anomalies are shaped mostly by mechanisms (1–3) during CT events from the boreal winter to spring. These mechanisms seem less efficient during WP events when the atmospheric response seems driven mostly by mechanism (4), coupling positive west-east SSTA gradient with weaker-than-normal low level easterlies, and secondary by mechanism (3), from the boreal spring to summer.
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References
Alexander M, Blade I, Newman M, Lazante J, Lau NC, Scott J (2002) The atmospheric bridge: the influence of ENSO teleconnections on air–sea interaction over global oceans. J Clim 15:2205–2231
Ashok K, Behera SK, Rao SA, Weng H, Yamagata T (2007) El Niño Modoki and its possible teleconnection. J Geophys Res 112:C11007. doi:10.1029/2006JC003798
Barbero R, Moron V (2011) Seasonal to decadal modulation of the ENSO impact on New Caledonia rainfall (1950–2010). J Geophys Res 116:D23111. doi:10.1029/2011JD16577
Chang P, Ji L, Li H (1997) A decadal climate variation in the tropical Atlantic ocean from thermodynamic air–sea interactions. Nature 385:516–518
Chen A, Taylor MA (2002) Investigating the link between the early season Caribbean rainfall and the Niño+1 year. Int J Clim 28:87–106
Chen M, Xie P, Janowiak JE, Arkin PA (2002) Global land precipitation: a 50-yr monthly analysis based on gauge observations. J Hydrometeor 3:249–266
Enfield D (1996) Relationships of inter-American rainfall to tropical Atlantic and Pacific SST variability. Geophys Res Lett 23:3305–3308
Enfield D, Alfaro EJ (1999) The dependence of Caribbean rainfall on the interaction of the tropical Atlantic and Pacific ocean. J Clim 12:2093–2103
Frankignoul C, Kestenare E (2005) Air–sea interactions in the tropical Atlantic: a view based on lagged rotated maximum covariance analysis. J Clim 18:3874–3890
Gamble DW, Curtis S (2008) Caribbean precipitation: review, model and prospect. Prog Phys Geogr 32:265–276
Giannini A, Kushnir Y, Cane MA (2000) Interannual variability of Caribbean rainfall, ENSO and the Atlantic ocean. J Clim 13:297–311
Giannini A, Chiang JCH, Cane MA, Kushnir Y, Seager R (2001) The ENSO teleconnection to the tropical Atlantic ocean: contributions of the remote and local SSTs to rainfall variability in the tropical Americas. J Clim 14:4530–4544
Goldenberg SB, Shapiro LJ (1996) Physical mechanisms for the association of el niño and west african rainfall with Atlantic major hurricane activity. J Clim 9(6):1169–1187
Gouirand I, Moron V, Zorita E (2007) Teleconnections between ENSO and North Atlantic in an ECHO-G simulation of the 100–1990 period. Geophys Res Lett 34:L06706. doi:10.1029/2006GL028852
Gouirand I, Jury M, Sing B (2012) An analysis of low- and high-frequency summer climate variability around the Caribbean Antilles. J Clim 25(11):3942–3952. doi:10.1175/JCLI-D-11-00269.1
Horel JD, Wallace JM (1981) Planetary scale atmospheric phenomena associated to the southern oscillation. Mon Weather Rev 109:813–829
Hu Z-Z, Kumar A, Huang B, Xue Y, Wang W, Jha B (2011) Persistent atmospheric and oceanic anomalies in the north Atlantic from summer 2009 to summer. J Clim 24(22):5812–5830. doi:10.1175/2011JCLI4213.1
Hu Z-Z, Kumar A, Jha B, Wang B, Huang Bohua, Huang Boyin (2012) An analysis of warm pool and cold tongue El Niños: air–sea coupling processes, global influences, and recent trends. Clim Dyn 38:2017–2035. doi:10.1007/s00382-011-1224-9
Kalnay E et al (1996) The NCEP/NCAR 40-year reanalysis project. Bull Am Met Soc 77:437–471
Kao HY, Yu JY (2009) Contrasting eastern-Pacific and central-Pacific types of El Niño. J Clim 22:615–632
Klein SA, Soden BJ, Lau NG (1999) Remote sea surface temperature variations during ENSO: evidence for a tropical atmospheric bridge. J Clim 12:917–932
Kug JS, Jin FF, An SI (2009) Two types of El Niño events: cold tongue El Niño and warm pool El Niño. J Clim 22:1499–1515. doi:10.1175/2008JCLI2624.1
Kug JS, Choi J, An SI, Jin FF, Wittenberg AT (2010) Warm pool and cold tongue El Niño events as simulated by the GFDL 2.1 coupled GCM. J Clim 23:1226–1239
Moron V, Gouirand I (2003) Seasonal modulation of the El Niño southern oscillation relationship with sea level pressure anomalies over the north Atlantic in October-March 1873–1996. Int J Clim 23:143–155
Moron V, Bigot S, Roucou P (1995) Rainfall variability in subequatorial America and Africa and relationships with the main sea surface temperatures modes (1951–1990). Int J Clim 15:1297–1322
Nobre P, Shukla J (1996) Variations of sea surface temperature, wind stress and rainfall over the tropical Atlantic and South America. J Clim 9:2464–2479
Seager R, Naik N, Ting M, Cane MA, Harnik N, Kushnir Y (2010) Adjustment of the atmospheric circulation to tropical Pacific SST anomalies: variability of transient eddy propagation in the Pacific–North America sector. QJR Meteorol. Soc. 136:277–296. doi:10.1002/qj.588
Smith TM, Reynolds RW, Peterson TC, Lawrimore J (2008) Improvements to NOAA’s historical merged land-ocean surface temperature analysis (1880–2006). J Clim 21:2283–2296
Taylor MA, Enfield DB, Chen A (2002) Influence of the tropical Atlantic versus the tropical Pacific on Caribbean rainfall. J Geophys Res Ocean 107:3127. doi:10.1029/2001JC001097
Taylor MA, Stephenson TS, Owino A, Chen A, Campbell D (2011) Tropical gradient influences on the Caribbean rainfall. J Geophys Res 116:D00Q08. doi:10.1029/2010JD015580
Weng H, Ashok K, Behera SK, Rao S, Yamagata T (2007) Impacts of recent El Nino Modoki on dry/wet conditions in the Pacific rim during boreal summer. Clim Dyn. doi:10.1007/s00382-007-0234-0
Xie SP (1999) A dynamic ocean-atmosphere model of the tropical Atlantic decadal variability. J Clim 12:64–70
Xie SP, Carton JA (2004) Tropical Atlantic variability: patterns, mechanisms, and impacts. Earth climate: the ocean–atmosphere interaction. In: Wang C et al. (eds) AGU Geophys Monogr Ser 147:121–142
Xie SP, Philander SGH (1994) A coupled ocean–atmosphere model of relevance to the ITCZ in the eastern Pacific. Tellus 46A:340–350
Yeh S et al (2009) El Niño in a changing climate. Nature 461:511–514
Yu JY, Kim ST (2011) Relationships between extratropical sea level pressure variations and the central Pacific and eastern Pacific types of ENSO. J Clim 24:708–720. doi:10.1175/2010JCLI3688.1
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The authors appreciate two reviewers for their constructive suggestions which help us to improve the manuscript significantly.
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Gouirand, I., Moron, V., Hu, ZZ. et al. Influence of the warm pool and cold tongue El Niños on the following Caribbean rainy season rainfall. Clim Dyn 42, 919–929 (2014). https://doi.org/10.1007/s00382-013-1753-5
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DOI: https://doi.org/10.1007/s00382-013-1753-5