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DOI | 10.1029/2017GB005862 |
Impacts of Shifts in Phytoplankton Community on Clouds and Climate via the Sulfur Cycle | |
Wang S.; Maltrud M.E.; Burrows S.M.; Elliott S.M.; Cameron-Smith P. | |
发表日期 | 2018 |
ISSN | 0886-6236 |
EISSN | 1944-9224 |
起始页码 | 1005 |
结束页码 | 1026 |
卷号 | 32期号:6 |
英文摘要 | Dimethyl sulfide (DMS), primarily produced by marine organisms, contributes significantly to sulfate aerosol loading over the ocean after being oxidized in the atmosphere. In addition to exerting a direct radiative effect, the resulting aerosol particles act as cloud condensation nuclei, modulating cloud properties and extent, with impacts on atmospheric radiative transfer and climate. Thus, changes in pelagic ecosystems, such as phytoplankton physiology and community structure, may influence organosulfur production, and subsequently affect climate via the sulfur cycle. A fully coupled Earth system model, including explicit marine ecosystems and the sulfur cycle, is used here to investigate the impacts of changes associated with individual phytoplankton groups on DMS emissions and climate. Simulations show that changes in phytoplankton community structure, DMS production efficiency, and interactions of multielement biogeochemical cycles can all lead to significant differences in DMS transfer to the atmosphere. Subsequent changes in sulfate aerosol burden, cloud condensation nuclei number, and radiative effect are examined. We find the global annual mean cloud radiative effect shifts up to 0.21 W/m2, and the mean surface temperature increases up to 0.1 °C due to DMS production changes associated with individual phytoplankton group in simulations with radiative effects at the 2,100 levels under an 8.5 scenario. However, changes in DMS emissions, radiative effect, and surface temperature are more intensive on regional scales. Hence, we speculate that major uncertainties associated with future marine sulfur cycling will involve strong region-to-region climate shifts. Further understanding of marine ecosystems and the relevant phytoplankton-aerosol-climate linkage are needed for improving climate projections. ©2018. The Authors. |
英文关键词 | climate impact; community composition change; dimethyl sulfide; phytoplankton |
语种 | 英语 |
scopus关键词 | aerosol; climate effect; cloud; cloud condensation nucleus; cloud radiative forcing; community composition; dimethylsulfide; phytoplankton; sulfide; sulfur cycle; surface temperature; uncertainty analysis |
来源期刊 | Global Biogeochemical Cycles
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/129819 |
作者单位 | The Climate Ocean and Sea Ice Modeling Group, Los Alamos National Laboratory, Los Alamos, NM, United States; Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, WA, United States; Atmospheric, Earth and Energy Division, Lawrence Livermore National Laboratory, Livermore, CA, United States |
推荐引用方式 GB/T 7714 | Wang S.,Maltrud M.E.,Burrows S.M.,et al. Impacts of Shifts in Phytoplankton Community on Clouds and Climate via the Sulfur Cycle[J],2018,32(6). |
APA | Wang S.,Maltrud M.E.,Burrows S.M.,Elliott S.M.,&Cameron-Smith P..(2018).Impacts of Shifts in Phytoplankton Community on Clouds and Climate via the Sulfur Cycle.Global Biogeochemical Cycles,32(6). |
MLA | Wang S.,et al."Impacts of Shifts in Phytoplankton Community on Clouds and Climate via the Sulfur Cycle".Global Biogeochemical Cycles 32.6(2018). |
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