Aerosol- and updraft-limited regimes of cloud droplet formation: Influence of particle number, size and hygroscopicity on the activation of cloud condensation nuclei (CCN)

Abstract

We have investigated the formation of cloud droplets under pyro-convective conditions using a cloud parcel model with detailed spectral microphysics and with the κ-Köhler model approach for efficient and realistic description of the cloud condensation nucleus (CCN) activity of aerosol particles. Assuming a typical biomass burning aerosol size distribution (accumulation mode centred at 120 nm), we have calculated initial cloud droplet number concentrations (NCD) for a wide range of updraft velocities (w=0.25-20ms-1) and aerosol particle number concentrations (N CAT=200-105cm-3) at the cloud base. Depending on the ratio between updraft velocity and particle number concentration (w/NCN), we found three distinctly different regimes of CCN activation and cloud droplet formation: (1) An aerosol-limited regime that is characterized by high w/NCN ratios (>≈10-3ms -1 cm3), high maximum values of water vapour supersaturation (Smax≈ 0.5%), and high activated fractions of aerosol particles (NCD/NCN≈90%). In this regime N CD D is directly proportional to NcN and practically independent of w. (2) An updraft-limited regime that is characterized by low w/NCN ratios ( < ≈10-4 ms-1 cm3), low maximum values of water vapour supersaturation (Smax <0.05) and also in the updraft-limited regime for aerosols with higher than average hygroscopicity (κ>0.3) did the relative sensitivities ∂lnNCD/∂lnκ/≈(△N CD/△NCD)/(△κ/κ) exceed values of ∼0.2, indicating that a 50% difference in κ would change N CD by more than 10%. The influence of changing size distribution parameters was stronger than that of particle hygroscopicity. Nevertheless, similar regimes of CCN activation were observed in simulations with varying types of size distributions (polluted and pristine continental and marine aerosols with different proportions of nucleation, Aitken, accumulation, and coarse mode particles). In general, the different regimes can be discriminated with regard to the relative sensitivities of NCD against w and N CN (∂lnNCD/∂lw and ∂lnNCD/ ∂lnNCN)We propose to separate the different regimes by relative sensitivity ratios, (∂nNCD/∂lnw)/(∂lnN CD/∂lnNCN) of 4:1 and 1:4, respectively. The results of this and related studies suggest that the variability of initial cloud droplet number concentration in convective clouds is mostly dominated by the variability of updraft velocity and aerosol particle number concentration in the accumulation and Aitken mode. Coarse mode particles and the variability of particle composition and hygroscopicity appear to play major roles only at low supersaturation in the updraft-limited regime of CCN activation (5max0.2%).