Articles | Volume 21, issue 24
https://doi.org/10.5194/acp-21-18499-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-21-18499-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
21 Dec 2021
Research article |
| 21 Dec 2021
| 21 Dec 2021
Anthropogenic aerosol effects on tropospheric circulation and sea surface temperature (1980–2020): separating the role of zonally asymmetric forcings
Chenrui Diao
Department of Atmospheric Sciences, Texas A&M University, College Station, TX 77843, USA
Department of Atmospheric Sciences, Texas A&M University, College Station, TX 77843, USA
Shang-Ping Xie
Scripps Institution of Oceanography, University of California, San
Diego, La Jolla, CA 92093, USA
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Cited
22 citations as recorded by crossref.
- Possible shift in controls of the tropical Pacific surface warming pattern M. Watanabe et al. 10.1038/s41586-024-07452-7
- East Asian summer monsoon response to anthropogenic aerosols redistribution: contrasting 1950–1980 and 1980–2010 to understand the role of non-Asian forcing Z. Shao et al. 10.1007/s00382-023-07016-x
- Impacts of reducing scattering and absorbing aerosols on the temporal extent and intensity of South Asian summer monsoon and East Asian summer monsoon C. Fang et al. 10.5194/acp-23-8341-2023
- Interhemispheric Contrasts of Ocean Heat Content Change Reveals Distinct Fingerprints of Anthropogenic Climate Forcings J. Shi et al. 10.1029/2023GL102741
- Amplified Interhemispheric Rainfall Contrast in Boreal Summer Due To Reduction in Anthropogenic Emissions Under COVID‐MIP Green Economic‐Recovery Scenarios X. Yu et al. 10.1029/2023EF003743
- Large-scale climate response to regionally confined extratropical cooling: effect of ocean dynamics J. Kim et al. 10.1007/s00382-022-06500-0
- Strong control of effective radiative forcing by the spatial pattern of absorbing aerosol A. Williams et al. 10.1038/s41558-022-01415-4
- The Contribution of Climate Change to Increasing Extreme Ocean Warming Around Japan M. Hayashi et al. 10.1029/2022GL100785
- Subsurface Ocean Temperature Responses to the Anthropogenic Aerosol Forcing in the North Pacific J. Shi et al. 10.1029/2022GL101035
- Evaluating uncertainty in aerosol forcing of tropical precipitation shifts A. Peace et al. 10.5194/esd-13-1215-2022
- Scenario Dependence of Future Precipitation Changes across Japan in CMIP6 M. Hayashi et al. 10.2151/sola.2024-028
- Dust storm induced severe cooling in the northern Arabian Sea during winter 2022 S. Nukapothula et al. 10.1016/j.dsr.2023.104047
- Two Distinct Modes of Climate Responses to the Anthropogenic Aerosol Forcing Changes J. Shi et al. 10.1175/JCLI-D-21-0656.1
- The competition between anthropogenic aerosol and greenhouse gas climate forcing is revealed by North Pacific water-mass changes J. Shi et al. 10.1126/sciadv.adh7746
- Seasonal delay of Sahelian rainfall driven by an east–west contrast in radiative forcing in idealized CESM experiments H. Dong et al. 10.1007/s00382-024-07452-3
- Distributions and Trends of the Aerosol Direct Radiative Effect in the 21st Century: Aerosol and Environmental Contributions Q. Yu & Y. Huang 10.1029/2022JD037716
- Increased Asian aerosols drive a slowdown of Atlantic Meridional Overturning Circulation F. Liu et al. 10.1038/s41467-023-44597-x
- A comparative analysis of the attribution of extreme summer precipitation in south and north parts of the East China monsoon region—with the year 2020 as an example R. Li et al. 10.1002/joc.8260
- Aerosol Induced Changes in Sea Surface Temperature Over the Bay of Bengal Due to COVID-19 Lockdown T. Sarin et al. 10.3389/fmars.2021.648566
- Little Influence of Asian Anthropogenic Aerosols on Summer Temperature in Central East Asia Since 1960 W. Hua et al. 10.1029/2022GL097946
- Reduction in European anthropogenic aerosols and the weather conditions conducive to PM2.5 pollution in North China: a potential global teleconnection pathway Z. Wang et al. 10.1088/1748-9326/ac269d
- Modelling human–natural systems interactions with implications for twenty-first-century warming V. Ramanathan et al. 10.1038/s41893-021-00826-z
18 citations as recorded by crossref.
- Possible shift in controls of the tropical Pacific surface warming pattern M. Watanabe et al. 10.1038/s41586-024-07452-7
- East Asian summer monsoon response to anthropogenic aerosols redistribution: contrasting 1950–1980 and 1980–2010 to understand the role of non-Asian forcing Z. Shao et al. 10.1007/s00382-023-07016-x
- Impacts of reducing scattering and absorbing aerosols on the temporal extent and intensity of South Asian summer monsoon and East Asian summer monsoon C. Fang et al. 10.5194/acp-23-8341-2023
- Interhemispheric Contrasts of Ocean Heat Content Change Reveals Distinct Fingerprints of Anthropogenic Climate Forcings J. Shi et al. 10.1029/2023GL102741
- Amplified Interhemispheric Rainfall Contrast in Boreal Summer Due To Reduction in Anthropogenic Emissions Under COVID‐MIP Green Economic‐Recovery Scenarios X. Yu et al. 10.1029/2023EF003743
- Large-scale climate response to regionally confined extratropical cooling: effect of ocean dynamics J. Kim et al. 10.1007/s00382-022-06500-0
- Strong control of effective radiative forcing by the spatial pattern of absorbing aerosol A. Williams et al. 10.1038/s41558-022-01415-4
- The Contribution of Climate Change to Increasing Extreme Ocean Warming Around Japan M. Hayashi et al. 10.1029/2022GL100785
- Subsurface Ocean Temperature Responses to the Anthropogenic Aerosol Forcing in the North Pacific J. Shi et al. 10.1029/2022GL101035
- Evaluating uncertainty in aerosol forcing of tropical precipitation shifts A. Peace et al. 10.5194/esd-13-1215-2022
- Scenario Dependence of Future Precipitation Changes across Japan in CMIP6 M. Hayashi et al. 10.2151/sola.2024-028
- Dust storm induced severe cooling in the northern Arabian Sea during winter 2022 S. Nukapothula et al. 10.1016/j.dsr.2023.104047
- Two Distinct Modes of Climate Responses to the Anthropogenic Aerosol Forcing Changes J. Shi et al. 10.1175/JCLI-D-21-0656.1
- The competition between anthropogenic aerosol and greenhouse gas climate forcing is revealed by North Pacific water-mass changes J. Shi et al. 10.1126/sciadv.adh7746
- Seasonal delay of Sahelian rainfall driven by an east–west contrast in radiative forcing in idealized CESM experiments H. Dong et al. 10.1007/s00382-024-07452-3
- Distributions and Trends of the Aerosol Direct Radiative Effect in the 21st Century: Aerosol and Environmental Contributions Q. Yu & Y. Huang 10.1029/2022JD037716
- Increased Asian aerosols drive a slowdown of Atlantic Meridional Overturning Circulation F. Liu et al. 10.1038/s41467-023-44597-x
- A comparative analysis of the attribution of extreme summer precipitation in south and north parts of the East China monsoon region—with the year 2020 as an example R. Li et al. 10.1002/joc.8260
4 citations as recorded by crossref.
- Aerosol Induced Changes in Sea Surface Temperature Over the Bay of Bengal Due to COVID-19 Lockdown T. Sarin et al. 10.3389/fmars.2021.648566
- Little Influence of Asian Anthropogenic Aerosols on Summer Temperature in Central East Asia Since 1960 W. Hua et al. 10.1029/2022GL097946
- Reduction in European anthropogenic aerosols and the weather conditions conducive to PM2.5 pollution in North China: a potential global teleconnection pathway Z. Wang et al. 10.1088/1748-9326/ac269d
- Modelling human–natural systems interactions with implications for twenty-first-century warming V. Ramanathan et al. 10.1038/s41893-021-00826-z
Latest update: 13 Dec 2024
Short summary
Anthropogenic aerosol (AA) emission has shown a zonal redistribution since the 1980s, with a decline in the Western Hemisphere (WH) high latitudes and an increase in the Eastern Hemisphere (EH) low latitudes. This study compares the role of zonally asymmetric forcings affecting the climate. The WH aerosol reduction dominates the poleward shift of the Hadley cell and the North Pacific warming, while the EH AA forcing is largely confined to the emission domain and induces local cooling responses.
Anthropogenic aerosol (AA) emission has shown a zonal redistribution since the 1980s, with a...
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