Non-equilibrium evolution of HNO3/H2SO4/H2O stratospheric particles under multi-component diffusive condensation/evaporation regime

A box model is used to study the evolution of stratospheric HNO3/H2SO4/H2O solution particles along temperature variations, which force the droplet en semble far from the thermodynamic equilibrium. In the case of rapid tempera ture fluctuations, i.e. orographically forced lee waves, the model shows th at the micron-sized droplets meet the conditions to become precursors of so lid particles, mainly constituted of nitric acid hydrates. This paper exami nes how the particle size distributions and compositions are influenced by the presence of rapid temperature fluctuations, comparing model calculation s along prescribed thermal histories. There results a remarkable dependence of the particle physical status (solid and/or liquid) on the presence of w ave-like perturbations in the former thermal history of the air mass.