INFLUENCE OF THE AEROSOL-SIZE SPREAD ON DISSIPATIVE INSTABILITY OF AEROSOL FLOWS IN THE PLANETARY ATMOSPHERES.II. ATMOSPHERES OF MARS AND TITAN

摘要

The results on the aerosol-size spread influence on dissipative instability of aerosol flow in a cold weakly ionized collisional plasma, which were obtained in the first part of this paper [1], are used for the Mars (altitudes 70-100 km) and Titan (altitudes 900-1200 km) atmospheric conditions.The threshold charges and characteristic space-time instability scales are quantitatively estimated.