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and MJO amplitude across multimodel simulations in Jiang et al. (2016 , Fig. 3c ). Parameter τ depicts how rapidly precipitation must occur to remove excess column water vapor, or alternately the efficiency of surface precipitation generation per unit column water vapor anomaly, and is highly relevant to the convective onset diagnostics described above. AMOC structure diagnostic. The AMOC, with large temperature ( T ) and salinity ( S ) differences between the northward-flowing upper limb and
and MJO amplitude across multimodel simulations in Jiang et al. (2016 , Fig. 3c ). Parameter τ depicts how rapidly precipitation must occur to remove excess column water vapor, or alternately the efficiency of surface precipitation generation per unit column water vapor anomaly, and is highly relevant to the convective onset diagnostics described above. AMOC structure diagnostic. The AMOC, with large temperature ( T ) and salinity ( S ) differences between the northward-flowing upper limb and
