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<p><strong>Abstract.</strong> Precipitation tends to decrease as aerosol concentration increases in warm marine boundary layer clouds at fixed liquid water path (LWP). The quantitative nature of this relationship is captured using the precipitation susceptibility (<i>S</i><sub><i>o</i></sub>) metric. Previously published works disagree on the qualitative behavior of <i>S</i><sub><i>o</i></sub> in marine low clouds: <i>S</i><sub><i>o</i></sub> decreases monotonically with increasing LWP or clouddoi:10.5194/acp-16-11395-2016 fatcat:uai2ybjlo5arlhqqxny4z6f6pq