JpGU-AGU Joint Meeting 2020

Presentation information

[E] Oral

A (Atmospheric and Hydrospheric Sciences ) » A-AS Atmospheric Sciences, Meteorology & Atmospheric Environment

[A-AS11] Aerosol impacts on air quality, climate system, and our society

convener:Teppei J Yasunari(Arctic Research Center, Hokkaido University), Kyu-Myong Kim(NASA Goddard Space Flight Center), Hongbin Yu(NASA Goddard Space Flight Center), Toshihiko Takemura(Research Institute for Applied Mechanics, Kyushu University)

[AAS11-09] Dependency of surface air temperature change by sulfate aerosols on CO2 concentration

*Toshihiko Takemura1 (1.Research Institute for Applied Mechanics, Kyushu University)

Keywords:aerosols, climate change, temperature, greenhouse gases, climate model, feedback

Sulfate aerosols are estimated to mitigate global warming through aerosol-radiation interactions by scattering solar radiation and through aerosol-cloud interactions enhancing it by cloud droplets. Under the present situation in which emissions of anthropogenic SO2, a primary precursor of sulfate aerosol, are decreasing and, on the other hand, atmospheric CO2 concentrations are increasing, it is anxious about accelerating global warming. In the previous study, a change in surface air temperature with perturbed SO2 and black carbon emissions (factors of 0.0, 0.1, 0.3, 0.5, 0.8, 1.5, and 2.0 relative to present emissions) were analyzed using an atmosphere-ocean general circulation model coupled with an aerosol process model, MIROC-SPRINTARS (Takemura and Suzuki, 2019). In this study, extended experiments were performed with CO2 concentrations both of present (369 ppm, recorded in 2000) and double (738 ppm, close to SSP3-7.0 scenario for 2080) for each SO2 emission factor. The experimental results show that reducing SO2 emission at high CO2 concentration brings an enhanced increase in surface air temperature. The warming is especially strong over land at the mid- and high- latitudes in the Northern Hemisphere because of an larger increase in water vapor that is a greenhouse gas, a weaker increase in liquid water path, and stronger ice-albedo feedback under the higher CO2 concentration.

Reference: Takemura, T., and K. Suzuki, Sci. Rep., 9, 2019, doi:10.1038/s41598-019-41181-6.