Model calculations for the formation of aerosols and the interaction b
etween themselves and with exhaust gases in plumes of cruising airline
rs are presented. A subset of in situ-nucleated H2SO4/H2O aerosols tha
t stay liquid can transform into an almost pure HNO3/H2O mode because
of enhanced uptake of HNO3. Soot embedded in a liquid coating containi
ng H2SO4 and HNO3 triggers heterogeneous freezing of water ice and lea
ds to visible contrails. At low temperatures and high fuel sulfur leve
ls homogeneous freezing increases the ice mass. The ice particles may
acquire a HNO3 . 3 H2O (NAT) coating upon evaporation of H2O, which ca
n potentially lead to a lengthening of their lifetime. If future plume
sampling experiments confirm these results, they would have important
Implications for ozone-related heterogeneous plume chemistry.