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

Charles A. Brock (Corresponding author), Karl D. Froyd, Maximilian Dollner, Christina J. Williamson, Gregory Schill, Daniel M. Murphy, Nicholas J. Wagner, Agnieszka Kupc, Jose L. Jimenez, Pedro Campuzano-Jost, Benjamin A. Nault, Jason C. Schroder, Douglas A. Day, Derek J. Price, Bernadett Weinzierl, Joshua P. Schwarz, Joseph M. Katich, Siyuan Wang, Linghan Zeng, Rodney WeberJack Dibb, Eric Scheuer, Glenn S. Diskin, Joshua P. DiGangi, ThaoPaul Bui, Jonathan M. Dean-Day, Chelsea R. Thompson, Jeff Peischl, Thomas B. Ryerson, Ilann Bourgeois, Bruce C. Daube, Roisin Commane, Steven C. Wofsy

Publications: Contribution to journalArticlePeer Reviewed

Abstract

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.
Original languageEnglish
Pages (from-to)15023-15063
Number of pages41
JournalAtmospheric Chemistry and Physics
Volume21
Issue number19
DOIs
Publication statusPublished - 8 Oct 2021

Funding

This research has been supported by the National Aeronautics and Space Administration (award nos. NNH15AB12I, NNX15AJ23G, NNX15AH33A, NNH13ZDA001N, NNX15AT90G, 80NSSC19K0124, and 80NSSC18K0630), the Austrian Science Fund FWF's Erwin Schrodinger Fellowship (grant no. J-3613), and the European Research Council under the European Union's Horizon 2020 framework (grant no. 640458). Additional support was provided by the US National Oceanic and Atmospheric Administration's Atmospheric Chemistry, Carbon Cycle, and Climate Program, and by the University of Vienna.

Austrian Fields of Science 2012

  • 103037 Environmental physics
  • 103039 Aerosol physics
  • 105206 Meteorology

Keywords

  • SOUTHEASTERN UNITED-STATES
  • CLOUD CONDENSATION NUCLEI
  • BROWN CARBON ABSORPTION
  • OPTICAL-PROPERTIES
  • BLACK CARBON
  • COMPREHENSIVE CHARACTERIZATION
  • SATELLITE-OBSERVATIONS
  • AIRCRAFT INSTRUMENT
  • SIZE DISTRIBUTIONS
  • HYGROSCOPIC GROWTH

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