Author
Listed:
- Valerio Ferracci
(Cranfield University
National Physical Laboratory)
- James Weber
(University of Sheffield
University of Reading)
- Conor G. Bolas
(University of Cambridge
ITOPF)
- Andrew D. Robinson
(University of Cambridge
Schlumberger Cambridge Research)
- Fiona Tummon
(Swiss Federal Office for Meteorology and Climatology MeteoSwiss)
- Pablo Rodríguez-Ros
(Institut de Ciències del Mar (ICM-CSIC)
Bisbe Perelló)
- Pau Cortés-Greus
(Institut de Ciències del Mar (ICM-CSIC))
- Andrea Baccarini
(École Polytechnique Fédérale de Lausanne
École Polytechnique Fédérale de Lausanne)
- Roderic L. Jones
(University of Cambridge)
- Martí Galí
(Institut de Ciències del Mar (ICM-CSIC))
- Rafel Simó
(Institut de Ciències del Mar (ICM-CSIC))
- Julia Schmale
(École Polytechnique Fédérale de Lausanne)
- Neil. R. P. Harris
(Cranfield University)
Abstract
Isoprene is a key trace component of the atmosphere emitted by vegetation and other organisms. It is highly reactive and can impact atmospheric composition and climate by affecting the greenhouse gases ozone and methane and secondary organic aerosol formation. Marine fluxes are poorly constrained due to the paucity of long-term measurements; this in turn limits our understanding of isoprene cycling in the ocean. Here we present the analysis of isoprene concentrations in the atmosphere measured across the Southern Ocean over 4 months in the summertime. Some of the highest concentrations ( >500 ppt) originated from the marginal ice zone in the Ross and Amundsen seas, indicating the marginal ice zone is a significant source of isoprene at high latitudes. Using the United Kingdom Earth System Model we show that current estimates of sea-to-air isoprene fluxes underestimate observed isoprene by a factor >20. A daytime source of isoprene is required to reconcile models with observations. The model presented here suggests such an increase in isoprene emissions would lead to >8% decrease in the hydroxyl radical in regions of the Southern Ocean, with implications for our understanding of atmospheric oxidation and composition in remote environments, often used as proxies for the pre-industrial atmosphere.
Suggested Citation
Valerio Ferracci & James Weber & Conor G. Bolas & Andrew D. Robinson & Fiona Tummon & Pablo Rodríguez-Ros & Pau Cortés-Greus & Andrea Baccarini & Roderic L. Jones & Martí Galí & Rafel Simó & Julia Sch, 2024.
"Atmospheric isoprene measurements reveal larger-than-expected Southern Ocean emissions,"
Nature Communications, Nature, vol. 15(1), pages 1-11, December.
Handle:
RePEc:nat:natcom:v:15:y:2024:i:1:d:10.1038_s41467-024-46744-4
DOI: 10.1038/s41467-024-46744-4
Download full text from publisher
References listed on IDEAS
- Martin Brüggemann & Nathalie Hayeck & Christian George, 2018.
"Interfacial photochemistry at the ocean surface is a global source of organic vapors and aerosols,"
Nature Communications, Nature, vol. 9(1), pages 1-8, December.
- Martin Brüggemann & Nathalie Hayeck & Christian George, 2018.
"Author Correction: Interfacial photochemistry at the ocean surface is a global source of organic vapors and aerosols,"
Nature Communications, Nature, vol. 9(1), pages 1-1, December.
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