4.5 Article

Properties of Saharan Dust Versus Local Urban Dust-A Case Study

Journal

EARTH AND SPACE SCIENCE
Volume 8, Issue 12, Pages -

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1029/2021EA001816

Keywords

lidar; mineral dust; aerosol; urban dust; particles; agro dust

Funding

  1. uropean Space Agency (ESA) project POLIMOS [4000119961/16/NL/FF/mg]
  2. European Cooperation in Science and Technology (COST) project InDust [CA16202]
  3. Deutsche Forschungsgemeinschaft (DFG) project IcePolCKa [HA 3314/9-1]
  4. European Commission [262254, 654109, 739530]
  5. Leibniz Institute of Tropospheric Research (TROPOS) in the Polish Foundation of Science and Technology [519/FNITP/115/2010]
  6. AERONET-PHOTONS at University of Lille

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On June 29-30, 2019, a huge amount of mineral dust from North Africa was forecasted to be transported to Poland, resulting in a unique dust event observed by lidar in Warsaw. The analyses conducted on the dust properties evolution revealed different characteristics of fine and coarse mode dust particles during the event, providing valuable data for future research and comparative studies.
On June 29-30, 2019, the Barcelona Dust Forecast Center with Non-hydrostatic Multiscale Model (NMMB/BSC-Dust) and the Navy Aerosol Analysis and Prediction System forecasted huge amounts of mineral dust over Poland. The Hybrid Single Particle Lagrangian Integrated Trajectory model confirmed uniquely fast (120 hr) long-range air-mass transport form North Africa to Poland. This remarkable dust event was observed using lidar at the Aerosol, Clouds and Trace Gases Research InfraStructure site in Warsaw, Central Poland; the only site equipped with Raman-Mie polarization water vapor lidar in East-Central Europe. The excellent capabilities of PollyXT lidar allowed to obtain an impressive number of 31 full sets of aerosol optical properties profiles, which enabled study of dust properties evolution on a rare hourly scale. The analyses were completed with the separation of fine and coarse mode dust particles form non-dust particles using the POlarization-LIdar PHOtometer Networking algorithm. Huge amount of an exceptionally pure mineral dust from Sahara measured in the free troposphere was characterized by a gradually decreasing coarse dust fraction (76%-21%) with a peak of fine dust fraction (67%) and particle linear depolarization ratio (26%) in the middle of the event. Within the boundary layer, a local urban dust mixed with pollution was observed with fine mode dust particles dominating (44%) and lower particle linear depolarization ratio (7.4%). The influx of pure mineral dust has been unique to this geographical region and will therefore be a reference point for future research and comparative studies.

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