The Hohenpeissenberg aerosol formation experiment (HAFEX): a long-term study including size-resolved aerosol, H2SO4, OH, and monoterpenes measurements
[摘要] Ambient aerosol size distributions(>3 nm) and OH, H2SO4, and terpene concentrationswere measured from April 1998 to August 2000 at a rural continental site in southern Germany.New particle formation (NPF) events were detected on 18% of all days, typically during midday hours under sunny and dry conditions.The number of newly formed particles correlated significantly with solar irradiance and ambientlevels of H2SO4. A pronounced anti-correlatation of NPF events with the pre-existingparticle surface area was identified in the cold season, often associated withthe advection of dry and relatively clean air masses from southerly directions (Alps).Estimates of the particle formation rate based on observations were around1 cm-3 s-1, being in agreement with the predictions of ternaryhomogeneous H2SO4-NH3-H2O nucleation within a few orders of magnitude.The experimentally determined nucleation mode particle growth rates were on average2.6 nm h-1, with a fraction of 0.7 nm h-1 being attributed to the co-condensation ofH2SO4-H2O-NH3. The magnitude of nucleation mode particle growth was neither significantly correlated toH2SO4, nor to the observed particle formation rate. Turn-over rate calculations of measured monoterpenes and aromatic hydrocarbons suggestthat especially the oxidation products of monoterpenes have the capacity tocontribute to the growth of nucleation mode particles. Although a large number of precursor gases, aerosol and meteorological parameterswere measured, the ultimate key factors controlling the occurence of NPF eventscould not be identified.
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[效力级别] [学科分类] 大气科学
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