What is the largest element of the intraseasonal variability in the tropical atmosphere?

Intertropical Convergence Zone
Madden–Julian oscillation
Hadley cell
El Niño–Southern Oscillation
The Madden–Julian oscillation is a large-scale coupling between atmospheric circulation and tropical deep convection. Unlike a standing pattern like the El Niño Southern Oscillation, the Madden–Julian oscillation is a traveling pattern that propagates eastward, through the atmosphere above the warm parts of the Indian and Pacific oceans. This overall circulation pattern manifests itself most clearly as anomalous rainfall.
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Intertropical Convergence Zone
Madden–Julian oscillation
Hadley cell
El Niño–Southern Oscillation
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20%
23%
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14