Investigation of the marine boundary layer cloud and CCN properties under coupled and decoupled conditions over the Azores

Six coupled and decoupled marine boundary layer (MBL) clouds were chosen from the 19month Atmospheric Radiation Measurement Mobile Facility data set over the Azores. Thresholds of liquid water potential temperature difference (L)<0.5K (>0.5K) and total water mixing ratio difference q(t)<0.5g/kg (>0.5g/kg) below the cloud base were used for selecting the coupled (decoupled) cases. A schematic diagram was given to demonstrate the coupled and decoupled MBL vertical structures and how they associate with nondrizzle, virga, and rain drizzle events. Out of a total of 2676 5min samples, 34.5% were classified as coupled and 65.5% as decoupled, 36.2% as nondrizzle and 63.8% as drizzle (47.7% as virga and 16.1% as rain), and 33.4% as daytime and 66.6% as nighttime. The decoupled cloud layer is deeper (0.406km) than coupled cloud layer (0.304km), and its liquid water path and cloud droplet effective radius (r(e)) values (122.1gm(-2) and 13.0 mu m) are higher than coupled ones (83.7gm(-2) and 10.4 mu m). Conversely, decoupled stratocumuli have lower cloud droplet number concentration (N-d) and surface cloud condensation nucleus (CCN) concentration (N-CCN) (74.5cm(-3) and 150.9cm(-3)) than coupled stratocumuli (111.7cm(-3) and 216.4cm(-3)). The linear regressions between r(e) and N-d with N-CCN have demonstrated that coupled r(e) and N-d strongly depend on N-CCN and have higher correlations (-0.56 and 0.59) with N-CCN than decoupled results (-0.14 and 0.25). The MBL cloud properties under nondrizzle and virga drizzle conditions are similar to each other but significantly different to those of rain drizzle.