Moteki, Q., 2015: Equatorially anti-symmetric features in the initiation processes of the Madden-Julian Oscillation observed in the late October during CINDY2011. J. Meteor. Soc. Japan, 93A, 59-79.
http://doi.org/10.2151/jmsj.2015-040 Graphical Abstract with highlights
- The initiation processes of the October-MJO during CINDY2011 that consisted of four distinct convective components are schematically illustrated in Figure 11.
- The equatorially anti-symmetric features of the MJO (Fig. 11b) were due to distinct dynamical features of the four convective components: s-ITCZ (the southern intertropical convergence zone) between 10°S and 0° along the meridional sea surface temperature gradients, n-ITCZ at the southern edge of the high SST above 29°C over the Bay of Bengal, VDAS (vortex disturbance over the Arabian Sea) in association with the zonal SST gradients, and WPDS (westward-propagating diurnal convection originating from Sumatra WPDS).
- A single larger-scale upward motion of the MJO was barotropically formed over the equator as a result of the merging of the four convective components in association with the weakening of the Mascarene High (Fig. 11c) and the propagating of the extratropical cyclone in the Southern Hemisphere (Fig. 11d).