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 (