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Dynamics of the Intertropical Convergence Zone

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Figure

Figure 2.1: Qualitative behavior of the ITCZ position (large dots) as the northwardcross-equatorial atmospheric energy fluxenergy input to the equatorial atmosphere ⟨v h⟩0 decreases (blue line) and as the net S0 − L0 − O0 = ∂y⟨v h⟩0 increases (redline)
Figure 2.2: (a) Mass flux streamfunction and (b) precipitation for global-mean = 298 K
Figure 2.3: ITCZ position in GCM simulations under (a) global and (b) tropicalwarming
Figure 2.4: (a) Mass flux streamfunction and (b) precipitation for equatorial surfacetemperaturesin (b) mark the precipitation maximum
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