Dust and water ice aerosols play a major role in the energy budget and circulation of the atmosphere of Mars and its climate. Dust affects the thermal structure and the dynamics of the atmosphere. Water ice clouds play an important part in the water cycle by altering the global transport of water vapor (Montmessin et al., 2004; Richardson & Wilson, 2002), by influencing the Martian climate radiatively (Madeleine et al., 2012; Wilson et al., 2008), and by changing the dust distribution through the scavenging of dust aerosols' particles due to the condensation of ice (Navarro et al., 2014; Pearl et al. 2001). Information on the aerosols physical properties is needed for a better understanding and modeling of Martian climate (
The ESA-Roscosmos ExoMars Trace Gas Orbiter (TGO) was launched on 14 March 2016 and was successfully inserted into Mars' orbit in November 2016. After several orbit maneuvers including a 12-month aerobraking phase it reached its final, 400-km altitude and near-circular orbit on
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