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Rectification of the Madden-Julian Oscillation into the ENSO cycle

W. S. Kessler1 and R. Kleeman2

1Pacific Marine Environmental Laboratory, National Oceanic and Atmospheric Administration, Seattle, Washington, 98115
2Bureau of Meteorology Research Center, Melbourne, Australia
Current affiliation: Courant Institute for Mathematical Sciences, New York University, New York, New York

Journal of Climate, 13(20), 3560–3575 (2000).
Copyright ©2000 by the American Meteorological Society. Further electronic distribution is not allowed.


An ocean general circulation model, forced with idealized, purely oscillating wind stress over the western equatorial Pacific similar to those observed during the Madden-Julian oscillation (MJO), developed rectified low-frequency anomalies in SST and zonal currents, compared to a run in which the forcing was climatological. The rectification in SST resulted from increased evaporation under stronger than normal winds of either sign, from correlated intraseasonal oscillations in both vertical temperature gradient and upwelling speed forced by the winds, and from zonal advection due to nonlinearly generated equatorial currents. The net rectified signature produced by the MJO-like wind stresses was SST cooling (about 0.4°C) in the west Pacific, and warming (about 0.1°C) in the central Pacific, tending to flatten the background zonal SST gradient. It is hypothesized that, in a coupled system, such a pattern of SST anomalies would spawn additional westerly wind anomalies as a result of SST-induced changes in the low-level zonal pressure gradient. This was tested in an intermediate coupled model initialized to 1 January 1997, preceding the 1997-98 El Niño. On its own, the model hindcast a relatively weak warm event, but when the effect of the rectified SST pattern was imposed, a coupled response produced the hypothesized additional westerlies and the hindcast El Niño became about 50% stronger (measured by east Pacific SST anomalies), suggesting that the MJO can interact constructively with the ENSO cycle. This implies that developing the capacity to predict, if not individual MJO events, then the conditions that affect their amplitude, may enhance predictability of the strength of oncoming El Niños.

1. Introduction
2. Model formulations and data processing
a. Ocean general circulation model
b. Intermediate coupled model
c. Observational data used for comparison
3. Results from the OGCM forced by idealized MJO wind stresses
a. Model temperature and current differences due to MJO winds
b. Rectifying processes in the OGCM
c. Model tests of the sensitivity to parameter choices and the form of the wind
4. Coupled effects of the rectified SST
5. Summary and discussion; Acknowledgments
6. Appendix A and B

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