4.7 Article

Ambient aerosol properties in the remote atmosphere from global-scale in situ measurements

Journal

ATMOSPHERIC CHEMISTRY AND PHYSICS
Volume 21, Issue 19, Pages 15023-15063

Publisher

COPERNICUS GESELLSCHAFT MBH
DOI: 10.5194/acp-21-15023-2021

Keywords

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Funding

  1. National Aeronautics and Space Administration [NNH15AB12I, NNX15AJ23G, NNX15AH33A, NNH13ZDA001N, NNX15AT90G, 80NSSC19K0124, 80NSSC18K0630]
  2. Austrian Science Fund FWF's Erwin Schrodinger Fellowship [J-3613]
  3. European Research Council under the European Union's Horizon 2020 framework [640458]
  4. US National Oceanic and Atmospheric Administration's Atmospheric Chemistry, Carbon Cycle, and Climate Program
  5. University of Vienna
  6. European Research Council (ERC) [640458] Funding Source: European Research Council (ERC)

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In situ measurements of aerosol microphysical, chemical, and optical properties were conducted during global-scale flights from 2016-2018 as part of the Atmospheric Tomography Mission (ATom). The data obtained were used to estimate aerosol hygroscopicity, size distributions, and other intensive and extensive aerosol properties, providing valuable insights into atmospheric aerosols and their behavior. By comparing different measurements and calculations, the study showed no substantial bias in the results, demonstrating the reliability and accuracy of the methodology.
In situ measurements of aerosol microphysical, chemical, and optical properties were made during globalscale flights from 2016-2018 as part of the Atmospheric Tomography Mission (ATom). The NASA DC-8 aircraft flew from similar to 84 degrees N to similar to 86 degrees S latitude over the Pacific, Atlantic, Arctic, and Southern oceans while profiling nearly continuously between altitudes of similar to 160m and similar to 12 km. These global circuits were made once each season. Particle size distributions measured in the aircraft cabin at dry conditions and with an underwing probe at ambient conditions were combined with bulk and single-particle composition observations and measurements of water vapor, pressure, and temperature to estimate aerosol hygroscopicity and hygroscopic growth factors and calculate size distributions at ambient relative humidity. These reconstructed, composition-resolved ambient size distributions were used to estimate intensive and extensive aerosol properties, including single-scatter albedo, the asymmetry parameter, extinction, absorption, Angstrom exponents, and aerosol optical depth (AOD) at several wavelengths, as well as cloud condensation nuclei (CCN) concentrations at fixed supersaturations and lognormal fits to four modes. Dry extinction and absorption were compared with direct in situ measurements, and AOD derived from the extinction profiles was compared with remotely sensed AOD measurements from the ground-based Aerosol Robotic Network (AERONET); this comparison showed no substantial bias.

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