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February 19, 2026Elementa Science of the Anthropocene0 citationsOpen Access

The biogenic sulfur cycle in the coupled ocean–sea ice–atmosphere system

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SISakiko IshinoMWMegan D. WillisHAHélène Angot

Key Points

  • The research aims to clarify the role of biogenic sulfur compounds in the polar climate system and improve their representation in models.
  • Synthesize existing literature on biogenic volatile methylated sulfur (VMS) compounds in polar regions.
  • Identify factors affecting VMS production and emissions in sea ice habitats.
  • Examine atmospheric oxidation processes of VMS and their impact on cloud properties.
  • Recommend priority research areas for improved model representation and observational strategies.
  • Polar oceans are significant sources of VMS compounds like DMS and MeSH, affecting atmospheric processes.
  • There are critical gaps in numerical models concerning VMS emissions and their climate impacts.
  • Certain physical features of sea ice influence VMS production and atmospheric oxidation rates.
  • Episodic VMS emissions during sea ice breakup may significantly affect the cloud condensation nuclei budget.

Abstract

Polar oceans and sea-ice regions are global hot spots for the production of biogenic volatile methylated sulfur (VMS) compounds: dimethyl sulfide (DMS) and methanethiol (MeSH). VMS compounds make important contributions to atmospheric particle formation and cloud property modulation, especially when polar atmospheres are pristine. As a result, the polar biogenic sulfur cycle may induce significant climate feedback in response to ongoing sea ice decline. However, polar VMS production, emission, and atmospheric oxidation processes remain poorly represented in current numerical models, hampering assessments of their radiative impacts and, in turn, implementation of targeted observations necessary for providing predictive understanding of changes in the ocean–sea ice–atmosphere (OIA) system. We synthesize current knowledge of the polar biogenic sulfur cycle and its representation in models. To untangle the existing gaps and provide a roadmap toward predictive understanding, we identify key features of sea ice habitats for biological VMS production, sea ice physical features that enhance or suppress VMS emissions, and atmospheric VMS oxidation at low temperatures that controls the contribution of oxidation products to particle formation or growth. These features are tightly coupled, emphasizing the need for coordinated efforts across disciplines that span the OIA interface, and among observational, experimental, and modeling communities. We recommend 4 priority research areas: (1) model representation of biological VMS production at the sea ice bottom and surface; (2) improved quantification of cloud condensation nuclei (CCN) sensitivity to VMS emissions with updated gas phase and multiphase oxidation chemistry at low temperatures; (3) better spatial and seasonal quantification of MeSH abundance and its biological and chemical controls in sea-ice environments; and (4) assessment of the contribution of episodic extreme VMS emissions during sea ice breakup for the polar CCN budget.

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Cite This Study

Ishino et al. (2026) studied this question.

synapsesocial.com/papers/6996a8c7ecb39a600b3efe34https://doi.org/10.1525/elementa.2025.00067
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