Changes in global DMS production driven by increased CO2 levels and its impact on radiative forcing

Abstract Our study highlights the importance of understanding the future changes in dimethyl-sulfide (DMS), the largest natural sulfur source, in the context of ocean acidification driven by elevated CO2 levels. We found a strong negative correlation (R 2 = 0.89) between the partial pressure of carb...

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Main Authors: Junri Zhao, Yan Zhang, Shujun Bie, Kelsey R. Bilsback, Jeffrey R. Pierce, Ying Chen
Format: Article
Language:English
Published: Nature Portfolio 2024-01-01
Series:npj Climate and Atmospheric Science
Online Access:https://doi.org/10.1038/s41612-024-00563-y
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author Junri Zhao
Yan Zhang
Shujun Bie
Kelsey R. Bilsback
Jeffrey R. Pierce
Ying Chen
author_facet Junri Zhao
Yan Zhang
Shujun Bie
Kelsey R. Bilsback
Jeffrey R. Pierce
Ying Chen
author_sort Junri Zhao
collection DOAJ
description Abstract Our study highlights the importance of understanding the future changes in dimethyl-sulfide (DMS), the largest natural sulfur source, in the context of ocean acidification driven by elevated CO2 levels. We found a strong negative correlation (R 2 = 0.89) between the partial pressure of carbon dioxide (pCO2) and sea-surface DMS concentrations based on global observational datasets, not adequately captured by the Coupled Model Intercomparison Project Phase 6 (CMIP6) Earth System Models (ESMs). Using this relationship, we refined projections of future sea-surface DMS concentrations in CMIP6 ESMs. Our study reveals a decrease in global sea-surface DMS concentrations and the associated aerosol radiative forcing compared to ESMs’ results. These reductions represent ~9.5% and 11.1% of the radiative forcings resulting from aerosol radiation and cloud interactions in 2100 reported by the Intergovernmental Panel on Climate Change Sixth Assessment Report. Thus, future climate projections should account for the climate implications of changes in DMS production due to ocean acidification.
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spelling doaj.art-983d67c4bdd7450ea625d15e730bfdce2024-01-14T12:17:34ZengNature Portfolionpj Climate and Atmospheric Science2397-37222024-01-01711810.1038/s41612-024-00563-yChanges in global DMS production driven by increased CO2 levels and its impact on radiative forcingJunri Zhao0Yan Zhang1Shujun Bie2Kelsey R. Bilsback3Jeffrey R. Pierce4Ying Chen5Shanghai Key Laboratory of Atmospheric Particle Pollution and Prevention (LAP3), National Observations and Research Station for Wetland Ecosystems of the Yangtze Estuary, Department of Environmental Science and Engineering, Fudan UniversityShanghai Key Laboratory of Atmospheric Particle Pollution and Prevention (LAP3), National Observations and Research Station for Wetland Ecosystems of the Yangtze Estuary, Department of Environmental Science and Engineering, Fudan UniversityShanghai Key Laboratory of Atmospheric Particle Pollution and Prevention (LAP3), National Observations and Research Station for Wetland Ecosystems of the Yangtze Estuary, Department of Environmental Science and Engineering, Fudan UniversityDepartment of Atmospheric Science, Colorado State UniversityDepartment of Atmospheric Science, Colorado State UniversityShanghai Key Laboratory of Atmospheric Particle Pollution and Prevention (LAP3), National Observations and Research Station for Wetland Ecosystems of the Yangtze Estuary, Department of Environmental Science and Engineering, Fudan UniversityAbstract Our study highlights the importance of understanding the future changes in dimethyl-sulfide (DMS), the largest natural sulfur source, in the context of ocean acidification driven by elevated CO2 levels. We found a strong negative correlation (R 2 = 0.89) between the partial pressure of carbon dioxide (pCO2) and sea-surface DMS concentrations based on global observational datasets, not adequately captured by the Coupled Model Intercomparison Project Phase 6 (CMIP6) Earth System Models (ESMs). Using this relationship, we refined projections of future sea-surface DMS concentrations in CMIP6 ESMs. Our study reveals a decrease in global sea-surface DMS concentrations and the associated aerosol radiative forcing compared to ESMs’ results. These reductions represent ~9.5% and 11.1% of the radiative forcings resulting from aerosol radiation and cloud interactions in 2100 reported by the Intergovernmental Panel on Climate Change Sixth Assessment Report. Thus, future climate projections should account for the climate implications of changes in DMS production due to ocean acidification.https://doi.org/10.1038/s41612-024-00563-y
spellingShingle Junri Zhao
Yan Zhang
Shujun Bie
Kelsey R. Bilsback
Jeffrey R. Pierce
Ying Chen
Changes in global DMS production driven by increased CO2 levels and its impact on radiative forcing
npj Climate and Atmospheric Science
title Changes in global DMS production driven by increased CO2 levels and its impact on radiative forcing
title_full Changes in global DMS production driven by increased CO2 levels and its impact on radiative forcing
title_fullStr Changes in global DMS production driven by increased CO2 levels and its impact on radiative forcing
title_full_unstemmed Changes in global DMS production driven by increased CO2 levels and its impact on radiative forcing
title_short Changes in global DMS production driven by increased CO2 levels and its impact on radiative forcing
title_sort changes in global dms production driven by increased co2 levels and its impact on radiative forcing
url https://doi.org/10.1038/s41612-024-00563-y
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AT shujunbie changesinglobaldmsproductiondrivenbyincreasedco2levelsanditsimpactonradiativeforcing
AT kelseyrbilsback changesinglobaldmsproductiondrivenbyincreasedco2levelsanditsimpactonradiativeforcing
AT jeffreyrpierce changesinglobaldmsproductiondrivenbyincreasedco2levelsanditsimpactonradiativeforcing
AT yingchen changesinglobaldmsproductiondrivenbyincreasedco2levelsanditsimpactonradiativeforcing