Simulation of cloud formation in the atmosphere of Titan

Physics

Scientific paper

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Scientific paper

For understanding the cloud formation, a detailed microphysical model is modified to simulate nucleation, condensation and coagulation processes occurring in the atmosphere of Titan. The model is validated by laboratory results that synthesize particle formation in Titan-like environment. Model results show that the model could reproduce well the laboratory experiment results including time evolution of total pressures, number concentration and composition. Applying the model to a mimic Titan atmosphere, cloud layers could be formed at altitudes between 10-30 km depending on the strength of vertical transport. These particles could be produced by the N2-CH4 binary nucleation mechanism and be more effective than the falling tholin particle mechanism assumed in many current models.

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