Editorial Type:
Article
Article Type:
Research Article

Interactive Feedback between ENSO and the Indian Ocean

Jong-Seong Kug Climate Environment System Research Center, Seoul National University, Seoul, South Korea

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In-Sik Kang Climate Environment System Research Center, Seoul National University, Seoul, South Korea

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Print Publication:
01 May 2006
DOI:
https://doi.org/10.1175/JCLI3660.1
Page(s):
1784–1801
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Abstract

A feedback process of the Indian Ocean SST on ENSO is investigated by using observed data and atmospheric GCM. It is suggested that warming in the Indian Ocean produces an easterly wind stress anomaly over Indonesia and the western edge of the Pacific during the mature phase of El Niño. The anomalous easterly wind in the western Pacific during El Niño helps a rapid termination of El Niño and a fast transition to La Niña by generating upwelling Kelvin waves. Thus, warming in the Indian Ocean, which is a part of the El Niño signal, operates as a negative feedback mechanism to ENSO. This Indian Ocean feedback appears to operate mostly for relatively strong El Niños and results in a La Niña one year after the mature phase of the El Niño. This 1-yr period of phase transition implies a possible role of Indian Ocean–ENSO coupling in the biennial tendency of the ENSO. Atmospheric GCM experiments show that Indian Ocean SST forcing is mostly responsible for the easterly wind anomalies in the western Pacific.

Corresponding author address: Prof. In-Sik Kang, School of Earth and Environmental Sciences, Seoul National University, Seoul, 151-742, South Korea. Email: kang@climate.snu.ac.kr

Abstract

A feedback process of the Indian Ocean SST on ENSO is investigated by using observed data and atmospheric GCM. It is suggested that warming in the Indian Ocean produces an easterly wind stress anomaly over Indonesia and the western edge of the Pacific during the mature phase of El Niño. The anomalous easterly wind in the western Pacific during El Niño helps a rapid termination of El Niño and a fast transition to La Niña by generating upwelling Kelvin waves. Thus, warming in the Indian Ocean, which is a part of the El Niño signal, operates as a negative feedback mechanism to ENSO. This Indian Ocean feedback appears to operate mostly for relatively strong El Niños and results in a La Niña one year after the mature phase of the El Niño. This 1-yr period of phase transition implies a possible role of Indian Ocean–ENSO coupling in the biennial tendency of the ENSO. Atmospheric GCM experiments show that Indian Ocean SST forcing is mostly responsible for the easterly wind anomalies in the western Pacific.

Corresponding author address: Prof. In-Sik Kang, School of Earth and Environmental Sciences, Seoul National University, Seoul, 151-742, South Korea. Email: kang@climate.snu.ac.kr

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  • Allan, R., and Coauthors, 2001: Is there an Indian Ocean dipole, and is it independent of the El Niño–Southern Oscillation? CLIVAR Exchanges, Vol. 6, No. 3, 18–22.

  • An, S-I., and I-S. Kang, 2001: Tropical Pacific basin-wide adjustment and oceanic waves. Geophys. Res. Lett., 28 , 3975–3978.

  • Annamalai, H., S-P. Xie, J. P. McCreary, and R. Murtugudde, 2005: Impact of Indian Ocean sea surface temperature on developing El Niño. J. Climate, 18 , 302–319.

    • Search Google Scholar
    • Export Citation

  • Baquero-Bernal, A., M. Latif, and L. Stephanie, 2002: On dipolelike variability of sea surface temperature in the tropical Indian Ocean. J. Climate, 15 , 1358–1368.

    • Search Google Scholar
    • Export Citation

  • Battisti, D., and A. C. Hirst, 1989: Interannual variability in a tropical atmosphere-ocean model: Influence of the basic state, ocean geometry, and nonlinearity. J. Atmos. Sci., 46 , 1687–1712.

    • Search Google Scholar
    • Export Citation

  • Bjerknes, J., 1969: Atmospheric teleconnections from the equatorial Pacific. Mon. Wea. Rev., 97 , 163–172.

  • Carton, J. A., G. Chepurin, X. Cao, and B. Giese, 2000a: A Simple Ocean Data Assimilation analysis of the global upper ocean 1950–95. Part I: Methodology. J. Phys. Oceanogr., 30 , 294–309.

    • Search Google Scholar
    • Export Citation

  • Carton, J. A., G. Chepurin, and X. Cao, 2000b: A Simple Ocean Data Assimilation analysis of the global upper ocean 1950–95. Part II: Results. J. Phys. Oceanogr., 30 , 311–326.

    • Search Google Scholar
    • Export Citation

  • Cohen, J., and P. Cohen, 1983: Applied Multi Regression/Correlation Analysis for the Behavioral Sciences. Lawrence Erlbam Associate, 545 pp.

    • Search Google Scholar
    • Export Citation

  • Harrison, D. E., 1987: Monthly mean island surface winds in the central tropical Pacific and El Niño. Mon. Wea. Rev., 115 , 3133–3145.

    • Search Google Scholar
    • Export Citation

  • Hastenrath, S., 2002: Dipoles, temperature gradients, and tropical climate anomalies. Bull. Amer. Meteor. Soc., 83 , 735–740.

  • Hastenrath, S., 2003: Reply. Bull. Amer. Meteor. Soc., 84 , 1424–1425.

  • Jin, F-F., 1997a: An equatorial ocean recharge paradigm for ENSO. Part I: Conceptual model. J. Atmos. Sci., 54 , 811–829.

  • Jin, F-F., 1997b: An equatorial ocean recharge paradigm for ENSO. Part II: A stripped-down coupled model. J. Atmos. Sci., 54 , 830–847.

    • Search Google Scholar
    • Export Citation

  • Kalnay, E., and Coauthors, 1996: The NCEP/NCAR 40-Year Reanalysis Project. Bull. Amer. Meteor. Soc., 77 , 437–471.

  • Kang, I-S., and J-S. Kug, 2000: An El-Niño prediction system with an intermediate ocean and a statistical atmosphere model. Geophys. Res. Lett., 27 , 1167–1170.

    • Search Google Scholar
    • Export Citation

  • Kim, J-K., I-S. Kang, and C-H. Ho, 1998: East Asian summer monsoon simulated by the Seoul National University GCM. Proc. Int. Conf. on Monsoon and Hydrologic Cycle, Kyongju, Korea, Korean Meteorological Society, 66–69.

  • Klein, S. A., B. J. Soden, and N. G. Lau, 1999: Remote sea surface temperature variation during ENSO: Evidence for a tropical atmosphere bridge. J. Climate, 12 , 917–932.

    • Search Google Scholar
    • Export Citation

  • Krishnamurthy, V., and B. P. Kirtman, 2003: Variability of the Indian Ocean: Relation to monsoon and ENSO. Quart. J. Roy. Meteor. Soc., 129 , 1623–1646.

    • Search Google Scholar
    • Export Citation

  • Kug, J-S., I-S. Kang, and S. E. Zebiak, 2001: The impacts of the model assimilated wind stress data in the initialization of an intermediate ocean and the ENSO predictability. Geophys. Res. Lett., 28 .3713, doi:10.1029/2000GL012793.

    • Search Google Scholar
    • Export Citation

  • Kug, J-S., S-I. An, F-F. Jin, and I-S. Kang, 2005: Preconditions for El Niño and La Niña onsets and their relation to the Indian Ocean. Geophys. Res. Lett., 32 .L05706, doi:10.1029/2004GL021674.

    • Search Google Scholar
    • Export Citation

  • Lau, N-C., and M. J. Nath, 2000: Impact of ENSO on the variability of the Asian–Australian monsoons as simulated in GCM experiments. J. Climate, 13 , 4287–4309.

    • Search Google Scholar
    • Export Citation

  • Lau, N-C., and M. J. Nath, 2003: Atmosphere–ocean variations in the Indo–Pacific sector during ENSO episodes. J. Climate, 16 , 3–20.

    • Search Google Scholar
    • Export Citation

  • Lau, N-C., and M. J. Nath, 2004: Simulation of tropical Indian Ocean SST variability with east–west asymmetry using a coupled atmosphere–ocean GCM. J. Climate, 17 , 245–265.

    • Search Google Scholar
    • Export Citation

  • Li, T., Y. Zhang, E. Lu, and D. Wang, 2002: Relative role of dynamic and thermodynamic processes in the development of the Indian Ocean dipole: An OGCM diagnosis. Geophys. Res. Lett., 29 .2110, doi:10.1029/2002GL015789.

    • Search Google Scholar
    • Export Citation

  • Misra, V., 2004: The teleconnection between the western Indian and the western Pacific Oceans. Mon. Wea. Rev., 132 , 445–455.

  • Moorthi, S., and M. J. Suarez, 1992: Relaxed Arakawa–Schubert: A parameterization of moist convection for general circulation models. Mon. Wea. Rev., 120 , 978–1002.

    • Search Google Scholar
    • Export Citation

  • Nakajima, T., M. Tsukamoto, Y. Tsushima, and A. Numaguti, 1995: Modelling of the radiative process in a AGCM. Climate System Dynamics and Modelling, Vol. I-3, T. Matsuno, Ed., Center for Climate System Research, 104–123.

    • Search Google Scholar
    • Export Citation

  • Reynolds, R. W., 1988: A real-time global sea surface temperature analysis. J. Climate, 1 , 75–86.

  • Reynolds, R. W., and T. M. Smith, 1994: Improved global sea surface temperature analyses using optimum interpolation. J. Climate, 7 , 929–948.

    • Search Google Scholar
    • Export Citation

  • Saji, N. H., and T. Yamagata, 2003: Structure of SST and surface wind variability during Indian Ocean dipole mode events: COADS observations. J. Climate, 16 , 2735–2751.

    • Search Google Scholar
    • Export Citation

  • Saji, N. H., B. N. Goswami, P. N. Vinayachandran, and T. Yamagata, 1999: A dipole mode in the tropical Indian Ocean. Nature, 401 , 360–363.

    • Search Google Scholar
    • Export Citation

  • Schopf, P. S., and M. J. Suarez, 1988: Vacillations in a coupled ocean-atmosphere model. J. Atmos. Sci., 45 , 549–566.

  • Shukla, J., and D. A. Paolino, 1983: The Southern Oscillation and long range forecasting of the summer monsoon anomalies over India. Mon. Wea. Rev., 111 , 1830–1837.

    • Search Google Scholar
    • Export Citation

  • Venzke, S., M. Latif, and A. Villwock, 2000: The coupled GCM ECHO-2. Part II: Indian Ocean response to ENSO. J. Climate, 13 , 1371–1383.

    • Search Google Scholar
    • Export Citation

  • Wang, B., and Q. Zhang, 2002: Pacific–East Asian teleconnection. Part II: How the Philippine Sea anticyclone established during the development of El Niño. J. Climate, 15 , 3252–3265.

    • Search Google Scholar
    • Export Citation

  • Wang, B., R. Wu, and R. Lukas, 1999: Roles of the western North Pacific wind variation in thermocline adjustment and ENSO phase transition. J. Meteor. Soc. Japan, 77 , 1–16.

    • Search Google Scholar
    • Export Citation

  • Wang, B., R. Wu, and X. Fu, 2000: Pacific–East Asia teleconnection: How does ENSO affect East Asian climate? J. Climate, 13 , 1517–1536.

    • Search Google Scholar
    • Export Citation

  • Wang, B., R. Wu, R. Lukas, and S. I. An, 2001: A possible mechanism for ENSO turnabout. Dynamics of Atmospheric General circulation and Climate, IAP/Academia Sinica, Ed., China Meteorological Press, 552–578.

    • Search Google Scholar
    • Export Citation

  • Wang, B., R. Wu, and T. Li, 2003: Atmosphere–warm ocean interaction and its impacts on Asian–Australian monsoon variation. J. Climate, 16 , 1195–1211.

    • Search Google Scholar
    • Export Citation

  • Wang, C., R. H. Weisberg, and J. I. Virmani, 1999: Western Pacific interannual variability associated with the El Niño-Southern Oscillation. J. Geophys. Res., 104 , 5131–5149.

    • Search Google Scholar
    • Export Citation

  • Watanabe, M., and F-F. Jin, 2002: Role of Indian Ocean warming in the development of the Philippine Sea anticyclone during ENSO. Geophys. Res. Lett., 29 .1478, doi:10.1029/2001GL014318.

    • Search Google Scholar
    • Export Citation

  • Watanabe, M., and F-F. Jin, 2003: A moist linear baroclinic model: Coupled dynamical–convective response to El Niño. J. Climate, 16 , 1121–1140.

    • Search Google Scholar
    • Export Citation

  • Webster, P. J., and T. N. Palmer, 1997: The past and the future of El Niño. Nature, 390 , 562–564.

  • Webster, P. J., A. M. Moore, J. P. Loschnigg, and R. R. Leben, 1999: Coupled ocean-atmosphere dynamics in the Indian Ocean during 1997-98. Nature, 401 , 356–360.

    • Search Google Scholar
    • Export Citation

  • Weisberg, R. H., and C. Wang, 1997a: Slow variability in the equatorial west-central Pacific in relation to ENSO. J. Climate, 10 , 1998–2017.

    • Search Google Scholar
    • Export Citation

  • Weisberg, R. H., and C. Wang, 1997b: A western Pacific oscillator paradigm for the El Niño-Southern Oscillation. Geophys. Res. Lett., 24 , 779–782.

    • Search Google Scholar
    • Export Citation

  • Wu, R., and B. Kirtman, 2004: Understanding the impacts of the Indian Ocean on ENSO variability in a coupled GCM. J. Climate, 17 , 4019–4031.

    • Search Google Scholar
    • Export Citation

  • Xie, S-P., H. Annamalai, F. A. Schott, and J. P. McCreary Jr., 2002: Structure and mechanisms of South Indian Ocean climate variability. J. Climate, 15 , 864–878.

    • Search Google Scholar
    • Export Citation

  • Yamagata, T., S. K. Behera, S. A. Rao, and H. N. Saji, 2003: Comments on “Dipoles, temperature gradients, and tropical climate anomalies.”. Bull. Amer. Meteor. Soc., 84 , 1418–1422.

    • Search Google Scholar
    • Export Citation

  • Yu, J-Y., C. R. Mechoso, J. C. McWilliams, and A. Arakawa, 2002: Impacts of the Indian Ocean on the ENSO cycle. Geophys. Res. Lett., 29 .1204, doi:10.1029/2001GL014098.

    • Search Google Scholar
    • Export Citation
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