In this study, a statistical model is developed that exploits the slow evolution of the Madden-Julian oscillation (MJO) to predict tropical rainfall variability at long lead times (i.e., 5-20 days). The model is based on a fieldto-field decomposition that uses previous and present pentads of outgoing longwave radiation (OLR; predictors) to predict future pentads of OLR (predictands). The model was developed using 30-70-day bandpassed OLR data from 1979 to 1989 and validated on data from 1990 to 1996. For the validation period, the model exhibits temporal correlations to observed bandpassed data of about 0.5-0.9 over a significant region of the Eastern Hemisphere at lead times from 5 to 20 days, after which the correlation drops rapidly with increasing lead time. Correlations against observed total anomalies are on the order of 0.3-0.5 over a smaller region of the Eastern Hemisphere.
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Waliser et al. (1999) studied this question.
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