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• W3112788071 abstract "Abstract It is generally believed that anthropogenic aerosols cool the atmosphere; therefore, they offset the global warming resulting from greenhouse gases to some extent. Reduction in sulphate, a primary anthropogenic aerosol, is necessary for mitigating air pollution, which causes atmospheric warming. Here, the changes in the surface air temperature under various anthropogenic emission amounts of sulphur dioxide (SO 2 ), which is a precursor of sulphate aerosol, are simulated under both present and doubled carbon dioxide (CO 2 ) concentrations with a climate model. No previous studies have conducted explicit experiments to estimate the temperature changes due to individual short-lived climate forcers (SLCFs) in different climate states with atmosphere–ocean coupled models. The simulation results clearly show that reducing SO 2 emissions at high CO 2 concentrations will significantly enhance atmospheric warming in comparison with that under the present CO 2 concentration. In the high latitudes of the Northern Hemisphere, the temperature change that will occur when fuel SO 2 emissions reach zero under a doubled CO 2 concentration will be approximately 1.0 °C, while this value will be approximately 0.5 °C under the present state. This considerable difference can affect the discussion of the 1.5 °C/2 °C target in the Paris Agreement." @default.
• W3112788071 created "2020-12-21" @default.
• W3112788071 creator A5017098610 @default.
• W3112788071 date "2020-12-10" @default.
• W3112788071 modified "2023-09-27" @default.
• W3112788071 title "Return to different climate states by reducing sulphate aerosols under future CO2 concentrations" @default.
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• W3112788071 doi "https://doi.org/10.1038/s41598-020-78805-1" @default.
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