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Overview of the Po valley fog experiment 1994 (CHEMDROP)

S. FuzziCNR Istituto per le Tecnologie Applicate ai Beni Culturali (CNR-ITABC)Paolo LajCNR Istituto per le Tecnologie Applicate ai Beni Culturali (CNR-ITABC)Loretta RicciCNR Istituto per le Tecnologie Applicate ai Beni Culturali (CNR-ITABC)G. OrsiCNR Istituto per le Tecnologie Applicate ai Beni Culturali (CNR-ITABC)Jost HeintzenbergLeibniz Institute for Tropospheric Research (TROPOS)Manfred WendischLeibniz Institute for Tropospheric Research (TROPOS)B. YuskiewiczLeibniz Institute for Tropospheric Research (TROPOS)Stephan MertesLeibniz Institute for Tropospheric Research (TROPOS)D. OrsiniLeibniz Institute for Tropospheric Research (TROPOS)Marina SchwanzLeibniz Institute for Tropospheric Research (TROPOS)Alfred WiedensohlerLeibniz Institute for Tropospheric Research (TROPOS)Frank StratmannLeibniz Institute for Tropospheric Research (TROPOS)Olle H. BergLund UniversityErik SwietlickiNuclear physicsG. P. FrankNuclear physicsBengt G. MartinssonNuclear physicsArmin GüntherGoethe-University,Jens Peter DierssenGoethe-Institute United KingdomD. SchellGoethe UniversityW. JaeschkeGoethe-University,A. BernerUniv of ViennaUlrike DusekUniv of ViennaZ. GalambosUniv of ViennaC. KruiszUniv of ViennaNigatu S. MesfinUniv of ViennaWolfram WobrockBlaise Pascal UniversityBeate Arends[Energy research Centre of the Netherlands]H.M. ten Brink[Energy research Centre of the Netherlands]
ABI

Abstract

The paper presents an outline of the CHEMDROP field experiment, carried out in November 1994 at the field station of S. Pietro Capofiume in the Po Valley, Italy. The main objective of the project was to address the issue of the size-dependent chemical composition of fog droplets, by experimentally investigating the following processes, which are expected to affect (or be affected by) the chemical composition of fog droplets as a function of size: a) the connection of the size-dependent chemical composition of CCN to the size-dependent composition of fog droplets; b) the gas/liquid partitioning of the gaseous species NH3, SO2, HCHO, HNO3 in fog; c) the Fe(II)/Fe(III) redox cycle in fog water. Some general results and overall conclusions of the experiment are reported in this paper, while more specific scientific questions are discussed in other companion papers in this issue. CHEMDROP results show that several processes concur in determining the size-dependence of fog droplets chemical composition: nucleation scavenging of pre-existing CCN, fog dynamical evolution and gas/liquid exchange between interstitial air and fog droplets. Chemical transformations in the liquid phase can cause further changes in the chemical composition of the droplets. Only by taking into account the combination of all these processes, is it possible to explain the inhomogeneities in fog droplet chemical composition.

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