Rectification of the MJO into the ENSO cycle
Figures from a talk on MJO rectification into the ENSO cycle
Figures from work done with Richard Kleeman (BMRC, Melbourne), submitted to J.Climate. These are the figures I showed during a talk on this work at the University of Washington, School of Oceanography, Phys.O. lunch seminar.
Comments are welcome! william.s.kessler@noaa.gov
Get the pdf version of the paper published in J. Climate
- Introductory slide
- (Fig. 16 from: Madden and Julian, J.Atmos.Sci., 1972, p1122; and Fig. 1 from Rui and Wang, J.Atmos.Sci., 1990, p358)
- SST, zonal wind and OLR along the equator during the onset of the 1997-98 El Niño
- OLR intraseasonal RMS and the Southern Oscillation Index
- Description of the OGCM
- Idealized MJO zonal wind anomalies on the equator imposed in the OGCM
- Rectified SST and surface current on the equator due to MJOs
- Three rectifying effects list
- Surface current differences due to MJOs (average over year 4) (map)
- Divergence of zonal momentum flux due to oscillating zonal winds
- Mean vector winds and windspeed from the ECMWF reanalysis
- Wind speed and latent heat flux in the W Pacific warm pool. Compare climatological and MJO OGCM runs
- Vertical advection under oscillating winds
- Vertical section of U showing out-of-phase currents at the surface and in the thermocline
- Momentum balance terms under oscillating winds
- Phases of temperature vertical advection features
- Mean model heat flux terms due to MJOs
- d(SST)/dx on the equator. Compare climatological and MJO OGCM runs
- Introductory slide for coupled model
- SST on the equator in the coupled model. Compare control forecast and MJO run
- Conclusion slide
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