Titlebook: Atmospheric Chemistry in the Mediterranean Region; Volume 2 - From Air Fran?ois Dulac,Stéphane Sauvage,Eric Hamonou Book 2022 The Editor(s

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https://doi.org/10.1007/b138024verse of the OH radical lifetime. Since OH is the main atmospheric oxidant during daytime, measuring the total OH reactivity represents an estimate of the total loading of reactive molecules in the atmosphere. This chapter presents the measurement principle of total OH reactivity and then results fr

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https://doi.org/10.1007/b138024o the process of condensation onto pre-existing particles), observed in a variety of environments. The processes of nucleation and early growth lead to the occurrence of new particle formation (NPF) in the atmosphere. NPF has frequently been observed in the Mediterranean basin, and a full overview o

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,Unbeschr?nkte Operatoren in Hilbertr?umen, gas phases normalized by the mass of aerosol. It is determined by the thermodynamic equilibrium between the particle (aerosol) and gas phase. This equilibrium is thought to be dominated by absorption phenomena. However, the validity of the instantaneous equilibrium between both phases and the predo

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