Validation of very high cloud droplet number concentrations in air masses transported thousands of kilometres over the ocean

Bengt G. Martinsson, Göran Frank, Sven Inge Cederfelt, Olle H. Berg, Besim Mentes, Giorgos Papaspiropoulos, Erik Swietlicki, Jingchuan Zhou, Michael Flynn, Keith N. Bower, Tom W. Choularton, Jyrki Mäkelä, Aki Virkkula, Rita Van Dingenen

    Research output: Contribution to journalArticlepeer-review


    The microstructure of orographic clouds related to the aerosol present was studied during the second Aerosol Characterisation Experiment (ACE-2). Very high cloud droplet number concentrations (almost 3000 cm-3) were observed. These high concentrations occurred when clouds formed on a hill slope at Tenerife in polluted air masses originating in Europe that had transported the order of 1000 km over the Atlantic Ocean. The validity of the measured droplet number concentrations was investigated by comparing with measurements of the aerosol upstream of the cloud and cloud interstitial aerosol. Guided by distributions of the ratios between the measurements, three criteria of typically 30% in maximum deviation were applied to the measurements to test their validity. Agreement was found for 88% of the cases. The validated data set spans droplet number concentrations of 150-3000 cm-3. The updraught velocity during the cloud formation was estimated to 2.2 m s-1 by model calculations, which is typical of cumuliform clouds. The results of the present study are discussed in relation to cloud droplet number concentrations previously reported in the literature. The importance of promoting the mechanistic understanding of the aerosol/cloud interaction and the use of validation procedures of cloud microphysical parameters is stressed in relation to the assessment of the indirect climatic effect of aerosols.
    Original languageEnglish
    Pages (from-to)801-814
    Number of pages13
    JournalTellus, Series B: Chemical and Physical Meteorology
    Issue number2
    Publication statusPublished - Apr 2000


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