Cloud-Scale Droplet Number Sensitivity to Liquid Water Path in Marine Stratocumulus
Cloud droplet number concentration (N c ) is retrieved from remotely observed marine stratocumulus cloud liquid water path (LWP), cloud optical depth (τ c ), and cloud thickness, using an optical model that assumes liquid water content (LWC) increases linearly from cloud base. Assuming that LWC is vertically uniform would underestimate τ c by 5% and N c by 14%. Individual retrievals of N c from 10-min averages vary by orders of magnitude from long-term averages. Surface cloud condensation nuclei (CCN) number concentration N CCN is weakly but significantly correlated with N c (R = 0.3) for the day leading and 6 hr following N c . Consistent with coalescence and drizzle scavenging cloud droplets, lag correlations show that N c decreases for 1 hr after the peak area-average rain rate. Greater observed LWP for lower N c [d(log N c )/d(log LWP) = 2.3] is consistent with enhanced entrainment drying of clouds with greater N c and consistent with removal of N c by thicker clouds with more coalescence and drizzle. Stronger precipitation in clouds with greater N c is the opposite sensitivity as expected were LWP to be controlled by the “cloud lifetime” indirect aerosol effect. The strong sensitivity of N c to LWP suggests that cloud dynamic and thermodynamic forcings drive macrophysical variability that controls N c in southeastern tropical Pacific stratocumulus clouds. Regressions are relatively insensitive to assumptions about the covariance of errors among the sensors.