Bg. Martinsson et al., EXPERIMENTAL-DETERMINATION OF THE CONNECTION BETWEEN CLOUD DROPLET SIZE AND ITS DRY RESIDUE SIZE, Atmospheric environment, 31(16), 1997, pp. 2477-2490
The droplet activation process and droplet growth was studied during e
arly stages of the formation of orographically-induced clouds. The exp
erimental results were compared with the results obtained with a close
d parcel, adiabatic cloud model. Good agreement was in most cases foun
d between model and measurements with respect to cloud droplet number
concentration, cloud droplet solute concentration and particle sizes s
cavenged due to cloud droplet nucleation. The experimental results wer
e mainly obtained with a new instrument, the droplet aerosol analyser
(DAA), which allows the determination of ambient sizes of cloud drople
ts and interstitial aerosol particles directly connected with the size
of its dry residue in a two-parameter data acquisition. The resulting
three-dimensional data set (ambient size, dry size, number concentrat
ion) was utilised to determine several cloud/aerosol properties, where
of some unique. (C) 1996 Elsevier Science Ltd.