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In-situ observations and modeling of nitric acid-containing particles in a cirrus cloud formation region

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Fig. 1. Backscatter ratios and aerosol depolarization at a wavelength of 532 nm measured during a Geophysica flight on 17 February 2005
Fig. 5. Thermodynamic equilibrium properties of STS aerosol particles containing 0.1 ppb H 2 SO 4 as a function of the ice saturation ratio S i for various combinations of the HNO 3 partial pressure p n and T prevailing during the TROCCINOX observations
Fig. 6. Steady-state molar HNO 3 /H 2 O ratios µ in ice (curves) versus normalized ice crystal spherical radius r i /r
Fig. 8. As Fig. 6, but resulting from a one-dimensional cloud-resolving simulation in which STS aerosols can dissolve HNO 3 and H 2 O kinetically and freeze homogeneously, and the growth, sedimentation, and HNO 3 uptake of individual ice particles are trac

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