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References

  • Gill, A. E. (1980), Some simple solutions for heat-induced tropical circulation, Q. J. R. Meteorol. Soc., 106, 447462.
  • Hsu, H. H., and F.-F. Jin (1990), The 1985/1986 intraseasonal oscillation and the role of the extratropics, J. Atmos. Sci., 47, 832839.
  • Ichikawa, H., and T. Yasunari (2006), Time–space characteristics of diurnal rainfall over Borneo and surrounding oceans as observed by TRMM-PR, J. Clim., 19, 12381260.
  • Liberti, G. L., F. Cheruy, and M. Desbois (2001), Land effect on the diurnal cycle of clouds over the TOGA COARE area, as observed from GMS IR data, Mon. Weather Rev., 129, 15001517.
  • Madden, R. A. (1986), Seasonal variation of the 40–50 day oscillation in the tropics, J. Atmos. Sci., 43, 31383158.
  • Madden, R. A., and P. R. Julian (1971), Detection of a 40–50 day oscillation in the zonal wind in the tropical Pacific, J. Atmos. Sci., 28, 702708.
  • Madden, R. A., and P. R. Julian (1972), Detection of global-scale circulation cells in the tropics with a 40–50 day period, J. Atmos. Sci., 29, 11091123.
  • Masunaga, H., T. S. L'Ecuyer, and C. D. Kummerow (2006), The Madden-Julian Oscillation recorded in early observations from the Tropical Rainfall Measuring Mission (TRMM), J. Atmos. Sci., 63, 27772794.
  • Matsuno, T. (1996), Quasi-geostrophic motions in the equatorial area, J. Meteorol. Soc. Jpn., 44, 2543.
  • Mori, S., J.-I. Hamada, Y. I. Tauhid, M. D. Yamanaka, N. Okamoto, F. Murata, N. Sakurai, H. Hashiguchi, and T. Sribimawati (2004), Diurnal land-sea rainfall peak migration over Sumatra island, Indonesian Maritime Continent, observed by TRMM satellite and intensive Rawinsonde soundings, Mon. Weather Rev., 132, 20212039.
  • Nakazawa, T. (1988), Tropical super clusters within intraseasonal variations over the western Pacific, J. Meteorol. Soc. Jpn., 66, 823836.
  • Nitta, T., T. Mizuno, and K. Takahashi (1992), Multi-scale convective systems during the initial phase of the 1986/87 El Nino, J. Meteorol. Soc. Jpn., 70, 317335.
  • Ramage, C. S. (1968), Role of a tropical “maritime continent” in the atmospheric circulation, Mon. Weather Rev., 96, 365370.
  • Sakurai, N., F. Murata, M. D. Yamanaka, S. Mori, J.-I. Hamada, H. Hashiguchi, Y. I. Tauhid, T. Sribimawati, and B. Suhardi (2005), Diurnal cycle of cloud system migration over Sumatera Island, J. Meteorol. Soc. Jpn., 83, 835850.
  • Sui, C.-H., and K. M. Lau (1992), Multiple phenomena in the tropical atmosphere over the western Pacific, Mon. Weather. Rev., 120, 407430.
  • Takayabu, Y. N. (1994a), Large-scale cloud disturbance associated with equatorial waves. part 1: Spectral features of the cloud disturbances, J. Meteorol. Soc. Jpn., 72, 433449.
  • Takayabu, Y. N. (1994b), Large-scale cloud disturbance associated with equatorial waves. part 2: Westward-propagating inertio-gravity waves, J. Meteorol. Soc. Jpn., 72, 451465.
  • Tian, B., D. E. Waliser, and E. J. Fetzer (2006), Modulation of the diurnal cycle of tropical convective clouds by MJO, Geophys. Res. Lett., 33, L20704, doi:10.1029/2006GL027752.
  • Weickmann, K. M., and S. J. S. Khalsa (1990), The shift of convection from the Indian Ocean to the Western Pacific Ocean during 30–60 day oscillation, Mon. Weather Rev., 120, 407430.
  • Wheeler, M., and G. N. Kiladis (1999), Convectively coupled equatorial waves: Analysis of clouds and temperature in the wavenumber-frequency domain, J. Atmos. Sci., 56, 374399.