作者: A. Hallberg , K. J. Noone , J. A. Ogren , I. B. Svenningsson , A. Flossmann
DOI: 10.1007/BF00696585
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摘要: The partitioning of aerosol particles between cloud droplets and interstitial air by number volume was determined both in terms an integral value as a function size for clouds on Mt. Kleiner Feldberg (825 m asl), the Taunus Mountains north-west Frankfurt am Main, Germany. Differences values dependent two periods during campaign were observed. Higher concentrations accumulation mode observed Period II compared to I. In I average 87 ± 11% (±one standard deviation) 73 7% incorporated into droplets. For corresponding fractions 42 6% 12 2% one event 64 4% 18 another event. time studied found have little variation. major processes influencing be nucleation scavenging entrainment.