Abstract. Here we analyze regional-scale data collected on board the NOAA WP-3D aircraft during the 2013
Southeast Nexus (SENEX) campaign to study the aerosol–cloud droplet link and quantify the
sensitivity of droplet number to aerosol number, chemical composition, and vertical velocity. For
this, the observed aerosol size distributions, chemical composition, and vertical-velocity
distribution are introduced into a state-of-the-art cloud droplet parameterization to show that
cloud maximum supersaturations in the region range from 0.02 % to 0.52 %, with
an average of 0.14±0.05 %. Based on these low values of supersaturation, the
majority of activated droplets correspond to particles with a dry diameter of 90 nm and above.
An important finding is that the standard deviation of the vertical velocity
(σw) exhibits considerable diurnal variability (ranging from
0.16 m s−1 during nighttime to over 1.2 m s−1 during day), and it tends to
covary with total aerosol number (Na). This σw–Na
covariance amplifies the predicted response in cloud droplet number (Nd) to
Na increases by 3 to 5 times compared to expectations based on Na
changes alone. This amplified response is important given that droplet formation is often
velocity-limited and therefore should normally be insensitive to aerosol changes. We also find
that Nd cannot exceed a characteristic concentration that depends solely on
σw. Correct consideration of σw and its covariance with time
and Na is important for fully understanding aerosol–cloud interactions and the
magnitude of the aerosol indirect effect. Given that model assessments of aerosol–cloud–climate
interactions do not routinely evaluate for overall turbulence or its covariance with other
parameters, datasets and analyses such as the one presented here are of the highest priority to
address unresolved sources of hydrometeor variability, bias, and the response of droplet number to
aerosol perturbations.