A166-03
Source and Chemistry of Hydroxymethanesulfonate (HMS) in Fairbanks, Alaska

Monday, 14 December 2020: 17:38
Virtual
James Campbell1, Michael Battaglia Jr2, Meeta Cesler-Maloney1, Jason Michael St Clair3,4, Thomas F Hanisco3, William R Simpson5, Rodney J Weber2 and Jingqiu Mao1, (1)University of Alaska Fairbanks, Geophysical Institute and Department of Chemistry and Biochemistry, Fairbanks, AK, United States, (2)Georgia Institute of Technology, School of Earth and Atmospheric Sciences, Atlanta, GA, United States, (3)NASA Goddard Space Flight Center, Atmospheric Chemistry and Dynamics Lab, Greenbelt, MD, United States, (4)University of Maryland Baltimore County, Baltimore, MD, United States, (5)University of Alaska Fairbanks, Department of Chemistry and Biochemistry & Geophysical Institute, Fairbanks, AK, United States
Abstract:
Fairbanks, Alaska is a subarctic city that often has high levels of fine particle pollution during the winter, resulting from trapping by strong atmospheric inversions and local emissions and chemistry under cold and dark conditions. Aerosol particle samples collected on filters in winters 2018-2019 and 2019-2020 confirm the existence of abundant hydroxymethanesulfonate (HMS) in these conditions. HMS is an adduct of dissolved SO2 and formaldehyde (HCHO), and may undergo further chemistry to produce particulate sulfate. During January-March of 2020, we deployed an online Particle into Liquid Sampler coupled to Ion Chromatography (PILS-IC) for quantification of HMS and inorganic sulfate in particle phase and a Laser Induced Fluorescence (LIF) instrument for HCHO in gas phase, along with ancillary measurements. We find that HMS serves as an important sulfur reservoir in the particle phase under cold conditions (T < -30 °C), with concentrations comparable to that of inorganic sulfate. We also find that HMS is correlated with inorganic sulfate during pollution events. The formation mechanism of HMS and its possible fate are further investigated with a multi-phase chemical box (0D) model constrained by ambient measurements. These observations and modeling of HMS formation under cold and dark conditions should improve our understanding of the relationship between secondary sulfur particulate species (HMS and sulfate) and precursor emissions (SO2 and HCHO), providing the basis for improved regulations aimed at reducing these pollution events.