Research Article

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

Figure 1

Longitude-time sections (Hovmöllor diagrams) of rainwater mixing ratio at the low level (the lowest level of the model, 𝑃 𝐵 = 9 9 6  hPa), surface pressure, and zonal velocity at 𝑃 𝐵 = 9 2 5  hPa in case (N). Values averaged for 5S–5N are shown.
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