Preprints
https://doi.org/10.5194/egusphere-2026-5595
https://doi.org/10.5194/egusphere-2026-5595
22 Sep 2026
 | 22 Sep 2026
Status: this preprint is open for discussion and under review for Atmospheric Chemistry and Physics (ACP).

Airborne measurements and model evaluation of dimethyl sulfide over the Amazon rainforest and Pacific Ocean

Bianca E. Krumm, Matthias Kohl, Anna Martin, Joseph Byron, Alexandra Gutmann, Michael Hewson, Jos Lelieveld, Andrea Pozzer, and Jonathan Williams

Abstract. Dimethyl sulfide (DMS) is the primary natural source of reduced sulfur to the atmosphere and, as a precursor to sulfate aerosols, indirectly influences Earth’s climate. Despite its global significance, upper tropospheric DMS measurements, particularly in deep-convective outflows, remain limited. Here we present two airborne datasets of in-situ DMS observations spanning 0.3–14 km over the Amazon rainforest and eastern Indo-Pacific Ocean, obtained during the CAFE-Brazil and CAFE-Pacific campaigns. These measurements confirm an east-west decreasing concentration gradient in the Amazonian boundary layer and reveal frequent elevated DMS (up to 56 pptv) in marine upper tropospheric convective outflows. Model-observation comparisons were performed with the EMAC (ECHAM5/MESSy2 Atmospheric Chemistry) model using several marine and terrestrial emission inventories and three different convection parametrisations. The sole available global terrestrial inventory (Spiro et al., 1992) overestimates Amazonian DMS by approximately a factor of three. Among the marine DMS climatologies, the Hulswar et al. (2022) inventory provides the closest agreement with the measurements, although further refinements remain10 necessary. Of the convection schemes tested, the Tiedtke scheme with Nordeng closure best reproduces the observed vertical DMS profile. Our results highlight the need for improved DMS emission parametrisations and show that the choice of convection scheme strongly influences the representation of the atmospheric sulfur cycle in global models. The frequent occurrence of DMS in deep convective outflow underscores the importance of further investigations into its transport, oxidation at cold temperatures, and role in new particle formation in the upper troposphere and stratosphere.

Competing interests: At least one of the (co-)authors is a member of the editorial board of Atmospheric Chemistry and Physics.

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Bianca E. Krumm, Matthias Kohl, Anna Martin, Joseph Byron, Alexandra Gutmann, Michael Hewson, Jos Lelieveld, Andrea Pozzer, and Jonathan Williams

Status: open (until 03 Nov 2026)

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Bianca E. Krumm, Matthias Kohl, Anna Martin, Joseph Byron, Alexandra Gutmann, Michael Hewson, Jos Lelieveld, Andrea Pozzer, and Jonathan Williams
Bianca E. Krumm, Matthias Kohl, Anna Martin, Joseph Byron, Alexandra Gutmann, Michael Hewson, Jos Lelieveld, Andrea Pozzer, and Jonathan Williams
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Latest update: 22 Sep 2026
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Short summary
We present airborne DMS observations (0.3-14 km) over the Amazon rainforest and Pacific Ocean, revealing frequent high DMS in marine upper‑tropospheric convective outflows. EMAC model comparisons show the global terrestrial inventory overestimates Amazonian DMS threefold and convection parameterisations control the vertical distribution of DMS and its oxidation products. The results call for improved emission inventories and further research on the fate of lofted DMS in the upper troposphere.
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