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Stephen E. Lang and Wei-Kuo Tao

( Choudhury and Krishnan 2011 ). The convectively coupled Madden–Julian oscillation (MJO; Madden and Julian 1971 , 1972 ) is another frequently studied, larger-scale tropical circulation strongly influenced by LH, including its characteristic transition from low-level heating during its build-up phase ( Wu 2003 ) to a top-heavy, stratiform-type heating profile during its mature phase ( Lin et al. 2004 ). Its propagation also depends on the depth and shape of the vertical heating profile ( Lau and Peng

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