Sensitivity of modelled sulfate aerosol and its radiative effect on climate to ocean DMS concentration and air–sea flux

Dimethylsulfide (DMS) is a well-known marine trace gas that is emitted from the ocean and subsequently oxidizes to sulfate in the atmosphere. Sulfate aerosols in the atmosphere have direct and indirect effects on the amount of solar radiation reaching the Earth's surface. Thus, as a potentia...

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Main Authors: J.-E. Tesdal, J. R. Christian, A. H. Monahan, K. von Salzen
Format: Article
Language:English
Published: Copernicus Publications 2016-09-01
Series:Atmospheric Chemistry and Physics
Online Access:https://www.atmos-chem-phys.net/16/10847/2016/acp-16-10847-2016.pdf
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author J.-E. Tesdal
J.-E. Tesdal
J. R. Christian
J. R. Christian
A. H. Monahan
K. von Salzen
author_facet J.-E. Tesdal
J.-E. Tesdal
J. R. Christian
J. R. Christian
A. H. Monahan
K. von Salzen
author_sort J.-E. Tesdal
collection DOAJ
description Dimethylsulfide (DMS) is a well-known marine trace gas that is emitted from the ocean and subsequently oxidizes to sulfate in the atmosphere. Sulfate aerosols in the atmosphere have direct and indirect effects on the amount of solar radiation reaching the Earth's surface. Thus, as a potential source of sulfate, ocean efflux of DMS needs to be accounted for in climate studies. Seawater concentration of DMS is highly variable in space and time, which in turn leads to high spatial and temporal variability in ocean DMS emissions. Because of sparse sampling (in both space and time), large uncertainties remain regarding ocean DMS concentration. In this study, we use an atmospheric general circulation model with explicit aerosol chemistry (CanAM4.1) and several climatologies of surface ocean DMS concentration to assess uncertainties about the climate impact of ocean DMS efflux. Despite substantial variation in the spatial pattern and seasonal evolution of simulated DMS fluxes, the global-mean radiative effect of sulfate is approximately linearly proportional to the global-mean surface flux of DMS; the spatial and temporal distribution of ocean DMS efflux has only a minor effect on the global radiation budget. The effect of the spatial structure, however, generates statistically significant changes in the global-mean concentrations of some aerosol species. The effect of seasonality on the net radiative effect is larger than that of spatial distribution and is significant at global scale.
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spelling doaj.art-1a752a7a66e04bedb0def8fe8d1902cc2022-12-22T02:35:27ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242016-09-0116108471086410.5194/acp-16-10847-2016Sensitivity of modelled sulfate aerosol and its radiative effect on climate to ocean DMS concentration and air–sea fluxJ.-E. Tesdal0J.-E. Tesdal1J. R. Christian2J. R. Christian3A. H. Monahan4K. von Salzen5School of Earth and Ocean Sciences, University of Victoria, Victoria, British Columbia, Canadanow at: Lamont-Doherty Earth Observatory, Columbia University, Palisades, New York, USAFisheries and Oceans Canada, Sidney, British Columbia, CanadaCanadian Centre for Climate Modelling and Analysis, Environment Canada, Victoria, British Columbia, CanadaSchool of Earth and Ocean Sciences, University of Victoria, Victoria, British Columbia, CanadaCanadian Centre for Climate Modelling and Analysis, Environment Canada, Victoria, British Columbia, CanadaDimethylsulfide (DMS) is a well-known marine trace gas that is emitted from the ocean and subsequently oxidizes to sulfate in the atmosphere. Sulfate aerosols in the atmosphere have direct and indirect effects on the amount of solar radiation reaching the Earth's surface. Thus, as a potential source of sulfate, ocean efflux of DMS needs to be accounted for in climate studies. Seawater concentration of DMS is highly variable in space and time, which in turn leads to high spatial and temporal variability in ocean DMS emissions. Because of sparse sampling (in both space and time), large uncertainties remain regarding ocean DMS concentration. In this study, we use an atmospheric general circulation model with explicit aerosol chemistry (CanAM4.1) and several climatologies of surface ocean DMS concentration to assess uncertainties about the climate impact of ocean DMS efflux. Despite substantial variation in the spatial pattern and seasonal evolution of simulated DMS fluxes, the global-mean radiative effect of sulfate is approximately linearly proportional to the global-mean surface flux of DMS; the spatial and temporal distribution of ocean DMS efflux has only a minor effect on the global radiation budget. The effect of the spatial structure, however, generates statistically significant changes in the global-mean concentrations of some aerosol species. The effect of seasonality on the net radiative effect is larger than that of spatial distribution and is significant at global scale.https://www.atmos-chem-phys.net/16/10847/2016/acp-16-10847-2016.pdf
spellingShingle J.-E. Tesdal
J.-E. Tesdal
J. R. Christian
J. R. Christian
A. H. Monahan
K. von Salzen
Sensitivity of modelled sulfate aerosol and its radiative effect on climate to ocean DMS concentration and air–sea flux
Atmospheric Chemistry and Physics
title Sensitivity of modelled sulfate aerosol and its radiative effect on climate to ocean DMS concentration and air–sea flux
title_full Sensitivity of modelled sulfate aerosol and its radiative effect on climate to ocean DMS concentration and air–sea flux
title_fullStr Sensitivity of modelled sulfate aerosol and its radiative effect on climate to ocean DMS concentration and air–sea flux
title_full_unstemmed Sensitivity of modelled sulfate aerosol and its radiative effect on climate to ocean DMS concentration and air–sea flux
title_short Sensitivity of modelled sulfate aerosol and its radiative effect on climate to ocean DMS concentration and air–sea flux
title_sort sensitivity of modelled sulfate aerosol and its radiative effect on climate to ocean dms concentration and air sea flux
url https://www.atmos-chem-phys.net/16/10847/2016/acp-16-10847-2016.pdf
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