EGU25-15896, updated on 15 Mar 2025
https://doi.org/10.5194/egusphere-egu25-15896
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Friday, 02 May, 08:30–10:15 (CEST), Display time Friday, 02 May, 08:30–12:30
 
Hall X5, X5.188
Vertical distribution of the concentrations of multiple aerosol types derived from the multiwavelength spaceborne lidar of the future Atmosphere Observing System 
Fazzal Qayyum1, Juan Cuesta1, Abou Bakr Merdji1, Anton Lopatin2, Oleg Dubovik3, Durgesh Nandan Piyush4, Laaziz El Amraoui5, and Richard Ferrare6
Fazzal Qayyum et al.
  • 1Univ Paris Est Creteil and Université Paris Cité, CNRS, LISA, F-94010 Créteil, France
  • 2GRASP SAS, Lezennes, 59260, France
  • 3Laboratoire d’Optique Atmospherique, UMR 8518, Villeneuve d’Ascq, 59650, France
  • 4National Center for Medium Range Weather Forecast, Ministry of Earth Sciences, NOIDA, INDIA, 201309
  • 5CNRM, Université de Toulouse, Météo-France, CNRS, 42 Avenue Gaspard Coriolis, 31057 Toulouse, France
  • 6NASA Langley Research Center, Hampton, VA, USA

Atmospheric aerosols play a key role in influencing the Earth's radiation budget. Still, their impacts remain poorly quantified due to the complex mechanisms involved in the interaction between aerosols and clouds. Indeed, aerosols act as ice-nucleating particles and cloud condensation nuclei, significantly altering the formation of precipitation and clouds. These environmental impacts of aerosols are strongly dependent on their composition, origin, and types. Moreover, high concentrations of aerosols in the atmosphere degrade air quality, posing large health risks which are also highly dependent on their composition (which is related to their types).

In recent decades, a space-borne lidar called the cloud–aerosol lidar with orthogonal polarization (CALIOP) onboard cloud–aerosol lidar and infrared pathfinder satellite observation (CALIPSO) satellite was providing aerosol vertical distribution from space using two wavelengths, namely 532 nm which provides attenuated backscatter and depolarization profiles and 1064 nm which deliver attenuated backscatter profile. Combining its 3 channels, CALIOP measurements provide a purely qualitative aerosol typing detection, indicating the presence or absence of a single aerosol type at each altitude of the atmosphere. To provide a more detailed and quantitative characterization of aerosols and to gain new insights into the interactions between aerosols, clouds, convective processes and precipitation, the upcoming mission called Atmosphere Observing System (AOS), which includes contributions from the space agencies NASA (United States), CNES (France), ASI (Italy), JAXA (Japan) and CSA (Canada) is currently in preparation for launching in a horizon near 2030. AOS payload will include an advanced high-energy 3-wavelength lidar with Raman capabilities during nighttime, called CALIGOLA.

In our present work, we examine the potential of CALIGOLA lidar during the daytime (three wavelength attenuated backscatter and depolarization measurements) and nighttime (one additional Raman channel in the UV which is suitable for nighttime measurements) flying in a polar orbit. By utilizing our newly developed retrieval approach, we quantitatively discriminate the concentration vertical profiles of five distinct aerosol types, such as smoke, continental, oceanic, dust and urban polluted. The development and first implementation of the method were performed using the pseudo-reality simulations obtained from the chemistry-transport model called Modèle de Chimie Atmosphérique de Grande Echelle (MOCAGE). In addition, the first tests of our innovative retrieval approach are planned using real lidar measurements from the High Spectral Resolution Lidar-2 (HSRL-2) airborne lidar from NASA Langley Research Center (LaRC).

How to cite: Qayyum, F., Cuesta, J., Merdji, A. B., Lopatin, A., Dubovik, O., Nandan Piyush, D., El Amraoui, L., and Ferrare, R.: Vertical distribution of the concentrations of multiple aerosol types derived from the multiwavelength spaceborne lidar of the future Atmosphere Observing System , EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-15896, https://doi.org/10.5194/egusphere-egu25-15896, 2025.