How sensitive are the Pacific–tropical North Atlantic teleconnections to the position and intensity of El Niño-related warming?
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The atmospheric teleconnections associated with the Eastern Pacific El Niño and El Niño Modoki events onto the tropical Atlantic Ocean are investigated. The Eastern Pacific El Niños drive significant warming of the tropical North Atlantic basin during boreal spring after its peak via the atmospheric bridge and tropospheric temperature mechanisms. However, the tropical Atlantic does not show a robust response to El Niño Modoki events. Here our results suggest that the preconditioning of the tropical North Atlantic sea surface temperature (SST) anomalies in boreal winter plays an important role in the following season, not only during Eastern Pacific El Niños but also during El Niño Modoki events. Additionally, we examine three other factors that could explain potential differences in the tropical Atlantic teleconnections from El Niño Modoki and Eastern Pacific El Niño events: (1) The distant location of the maximum SST warming in the Pacific; (2) The weak warming associated with this pattern; and (3) The SST pattern including a cooling in the eastern Pacific. Using numerical experiments forced with idealised SST in the equatorial Pacific, we show that the location of the El Niño Modoki SST warming during its mature phase could be favourable for exciting atmospheric teleconnections in boreal winter but not in the following spring season due to the seasonal shift of the Inter-Tropical Convergence Zone that modulates deep convection over the anomalous SST. This demonstrates the importance of the mean seasonal atmospheric circulation in modulating the remote teleconnections from the central-western Pacific warming in the model. However, it is suggested here that the cooling in the eastern Pacific associated with El Niño Modoki counteracts the atmospheric response driven by the central western Pacific warming, generating a consequent weaker connection to the tropical Atlantic compared to the stronger link during Eastern Pacific El Niño events. Finally we show that the modeled Pacific–tropical Atlantic teleconnections to an eastern Pacific warming depends strongly on the underlying seasonal cycle of SST.
KeywordsEl Niño El Niño Modoki Tropical Atlantic Atmospheric teleconnections
This research was supported by the Australian Research Council (ARC) including the ARC Centre of Excellence for Climate System Science (ARCCSS). This work is also part of the research conducted by the INCT-MC, INCT-Mar COI, and Rede CLIMA. The numerical experiments were undertaken on the NCI National Facility at the ANU, Australia, via the provision of computing resources. Use of NCAR’s CCSM3 model is gratefully acknowledged. We thank all the Institutions responsible for the observations and reanalysis products for having made their data available. Observational and reanalysis data provided by the NOAA/OAR/ESRL PSD, Boulder, Colorado, USA, is from their web site at http://www.esrl.noaa.gov/psd/. We thank Kris Karnauskas and one anonymous reviewer for their comments on the manuscript.
- Ashok K, Iizuka S, Rao SA, Saji NH, Lee W-J (2009) Processes and boreal summer impacts of the 2004 El Niño Modoki: an AGCM study. Geophys Res Lett 36:L04703Google Scholar
- Chiang JCH, Kushnir Y, Giannini A (2002) Deconstructing Atlantic Intertropical Convergence Zone variability: influence of the local cross-equatorial sea surface temperature gradient and remote forcing from the eastern equatorial Pacific. J Geophys Res 107:4004. doi: 10.1029/2000JD000307 CrossRefGoogle Scholar
- Matsuno T (1966) Quasi-geostrophic motions in the equatorial area. J Meteor Soc Jpn 44:25–43Google Scholar
- Rowell DP, Folland CK, Maskel K, Owen JA, Ward MN (1995) Variability of the summer rainfall over tropical North Africa (1906–92): observations and modeling. Q J R Meteorol Soc 121:669–704Google Scholar
- Schneider U, Becker A, Finger P, Meyer-Christoffer A, Ziese M, Rudolf B (2013) GPCC’s new land surface precipitation climatology based on quality-controlled in situ data and its role in quantifying the global water cycle. Theor App Climatol 115(1–2):15–40Google Scholar