Constraints on the Loss of Hydroperoxymethyl Thioformate (HPMTF) to Marine Clouds Using Aircraft Observations

Abstract The photochemical oxidation of dimethyl sulfide (DMS) by the hydroxyl radical (OH) contributes to the production and growth of particles and cloud condensation nuclei in the marine boundary layer (MBL). DMS oxidized by OH can go on to form a stable intermediate, hydroperoxymethyl thioformate (HPMTF), which is both globally ubiquitous and efficiently lost to multiphase processes in the marine atmosphere. Recent work has shown that clouds act as a significant and irreversible loss path for HPMTF, sequestering sulfur and greatly reducing the production of long-lived, climate-relevant species (e.g., SO2 and OCS). Until recently, there have been few observational constraints on the role of clouds in the spatiotemporal distribution of HPMTF and other soluble molecules in the MBL. Using a steady-state approximation, we determine a reactive uptake and first-order aqueous loss rate constant of HPMTF to cloud droplets of 1.2 (0.9–1.9) × 10–2 and 1.4 (0.4–2.2) × 10–1 s–1, respectively. The results suggest that hydrolysis and ozonolysis are significant within cloud droplets, and their competition likely impacts the distribution of sulfate and organic acids in the marine environment.

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Journal
ACS ES&T Air
Published
2026-09-29
DOI
https://doi.org/10.1021/acsestair.6c00199
Primary Topic
Atmospheric chemistry and aerosols
Type
article
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article

Constraints on the Loss of Hydroperoxymethyl Thioformate (HPMTF) to Marine Clouds Using Aircraft Observations

Lu Xu, C. Warneke, J. Kazil, Birger Bohn et al.
ACS ES&T Air
Atmospheric chemistry and aerosols
article

Constraints on the Loss of Hydroperoxymethyl Thioformate (HPMTF) to Marine Clouds Using Aircraft Observations

Lu Xu, C. Warneke, J. Kazil, Birger Bohn, Michelle Färber, C. A. Brock, Michael A. Robinson, Chelsea E. Stockwell, Adam T. Ahern, Kelvin H. Bates, Gordon A. Novak, Matthew Mitchell Coggon, Kristen Zuraski, Wyndom S. Chace, Kevin A. Wokosin, Han N. Huynh, Nell B. Schafer, Jeff Peischl, Hendrik Fuchs, Zachary Finewax, Anna Novelli, Timothy H. Bertram, Andrew W. Rollins, Ming Lyu, Patrick R. Veres, Steven S. S Brown, Georgios I. Gkatzelis, Christopher M. Jernigan, Eleanor M. Waxman, Katherine Ball, Bernadett Weinzierl, Aaron Stainsby, Maximilian Dollner, Siyuan Wang, Osinachi Ajoku
article en

Abstract

Abstract The photochemical oxidation of dimethyl sulfide (DMS) by the hydroxyl radical (OH) contributes to the production and growth of particles and cloud condensation nuclei in the marine boundary layer (MBL). DMS oxidized by OH can go on to form a stable intermediate, hydroperoxymethyl thioformate (HPMTF), which is both globally ubiquitous and efficiently lost to multiphase processes in the marine atmosphere. Recent work has shown that clouds act as a significant and irreversible loss path for HPMTF, sequestering sulfur and greatly reducing the production of long-lived, climate-relevant species (e.g., SO2 and OCS). Until recently, there have been few observational constraints on the role of clouds in the spatiotemporal distribution of HPMTF and other soluble molecules in the MBL. Using a steady-state approximation, we determine a reactive uptake and first-order aqueous loss rate constant of HPMTF to cloud droplets of 1.2 (0.9–1.9) × 10–2 and 1.4 (0.4–2.2) × 10–1 s–1, respectively. The results suggest that hydrolysis and ozonolysis are significant within cloud droplets, and their competition likely impacts the distribution of sulfate and organic acids in the marine environment.

ACS ES&T Air
California Institute of Technology (US), University of Vienna (AT), National Oceanic and Atmospheric Administration (US), University of Wisconsin–Madison (US), Howard University (US), Forschungszentrum Jülich (DE), University of Cologne (DE), University of Colorado Boulder (US), National Centre for Earth Observation (GB), NOAA Chemical Sciences Laboratory (US)
Life below water
Openalex Percentile: Top 16%
Atmospheric chemistry and aerosols
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