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Meng-Pai Hung, Jia-Lin Lin, Wanqiu Wang, Daehyun Kim, Toshiaki Shinoda, and Scott J. Weaver

these waves, there exists another mode of the tropical intraseasonal variability, the Madden–Julian oscillation (MJO; Madden and Julian 1971 ; Zhang 2005 ). The MJO involves the interaction between the convection and large-scale circulation and is characterized by the eastward propagation of planetary-scale (wavenumber 1–3) and low-frequency (period 30–60 days) waves. The MJO and CCEWs strongly affect the tropical weather such as the onset and breaks of the Asian and Australian monsoon systems (e

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Suzana J. Camargo

values of relative humidity in mid levels in the reanalysis compared to the climate models, as there are known differences between the relative humidity in the 40-yr European Centre for Medium-Range Weather Forecasts Re-Analysis (ERA) and NCEP reanalysis ( Daoud et al. 2009 ) and biases in the midtroposphere relative humidity in the NCEP reanalysis ( Bony et al. 1997 ). We calculated the difference between the models and NCEP reanalysis for the annual zonal-mean climatological relative humidity at

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