Research Article

Toward an Understanding of the Madden-Julian Oscillation: With a Mesoscale-Convection-Resolving Model of 0.2 Degree Grid

Figure 7

Longitude-time section (Hovmöllor diagrams) of the low-level rainwater mixing ratio in case (R). It is reproduced from Figure 6, but only a period from 480 to 640 days is shown. Each of synoptic-scale convective systems is labeled by A–K (except I). Squall-line systems are labeled by S1 and S2.
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