An increasing trend in L is observed, implying that dry equatorial waves travel longer distances in warmer climates in the presence of dissipation.
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Characterization of Moist Processes Associated With Changes in the Propagation of the MJO With Increasing CO<sub>2</sub>.
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However, neither process shows a clear trend with increasing CO 2 , although their absolute magnitudes increase (Figures 3 and 4 ).
M ∼ e f f has a value that is close to zero in all simulations, with hints of a negative trend.