Articles | Volume 19, issue 4
https://doi.org/10.5194/acp-19-2405-2019
© Author(s) 2019. 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-19-2405-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
25 Feb 2019
Research article |
| 25 Feb 2019
| 25 Feb 2019
Variability, timescales, and nonlinearity in climate responses to black carbon emissions
Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, Washington, USA
Joint Global Change Research Institute, Pacific Northwest National Laboratory, College Park, Maryland, USA
Hailong Wang
Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, Washington, USA
Catrin M. Mills
Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, Washington, USA
Philip J. Rasch
Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, Washington, USA
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30 citations as recorded by crossref.
- Evaluating climate emulation: fundamental impulse testing of simple climate models A. Schwarber et al. 10.5194/esd-10-729-2019
- Simulated aging processes of black carbon and its impact during a severe winter haze event in the Beijing-Tianjin-Hebei region D. Chen et al. 10.1016/j.scitotenv.2020.142712
- Effective Radiative Forcings Due To Anthropogenic Emission Changes Under Covid‐19 and Post‐Pandemic Recovery Scenarios X. Yu et al. 10.1029/2021JD036251
- Impacts of black carbon on the formation of advection–radiation fog during a haze pollution episode in eastern China Q. Ding et al. 10.5194/acp-19-7759-2019
- Atmospheric Circulation Patterns Conducive to Severe Haze in Eastern China Have Shifted Under Climate Change Y. Yang et al. 10.1029/2021GL095011
- Mapping the dependence of black carbon radiative forcing on emission region and season P. Räisänen et al. 10.5194/acp-22-11579-2022
- FLEXPART v10.1 simulation of source contributions to Arctic black carbon C. Zhu et al. 10.5194/acp-20-1641-2020
- HIRM v1.0: a hybrid impulse response model for climate modeling and uncertainty analyses K. Dorheim et al. 10.5194/gmd-14-365-2021
- A Strong Anthropogenic Black Carbon Forcing Constrained by Pollution Trends Over China Y. Liu et al. 10.1029/2022GL098965
- Fast response of global monsoon area and precipitation to regional carbonaceous aerosols A. Asutosh et al. 10.1016/j.atmosres.2024.107354
- Comparing the Radiative Forcings of the Anthropogenic Aerosol Emissions From Chile and Mexico T. Miinalainen et al. 10.1029/2020JD033364
- Source attribution of Arctic black carbon and sulfate aerosols and associated Arctic surface warming during 1980–2018 L. Ren et al. 10.5194/acp-20-9067-2020
- Airmass Analysis of Size-Resolved Black Carbon Particles Observed in the Arctic Based on Cluster Analysis R. Cremer et al. 10.3390/atmos13050648
- Sulfur emissions from consumption by developed and developing countries produce comparable climate impacts J. Lin et al. 10.1038/s41561-022-00898-2
- Long-term variability, source apportionment and spectral properties of black carbon at an urban background site in Athens, Greece E. Liakakou et al. 10.1016/j.atmosenv.2019.117137
- Reduced light absorption of black carbon (BC) and its influence on BC-boundary-layer interactions during “APEC Blue” M. Gao et al. 10.5194/acp-21-11405-2021
- Black Carbon Increases Frequency of Extreme ENSO Events S. Lou et al. 10.1175/JCLI-D-19-0549.1
- Estimating Arctic Temperature Impacts From Select European Residential Heating Appliances and Mitigation Strategies B. Seay et al. 10.1029/2020EF001493
- Relationship between ambient black carbon and daily mortality in Tehran, Iran: a distributed lag nonlinear time series analysis M. Rahmatinia et al. 10.1007/s40201-021-00659-0
- Fast Climate Responses to Aerosol Emission Reductions During the COVID‐19 Pandemic Y. Yang et al. 10.1029/2020GL089788
- Radiative Effects of Residential Sector Emissions in China: Sensitivity to Uncertainty in Black Carbon Emissions S. Archer‐Nicholls et al. 10.1029/2018JD030120
- Climate effects of future aerosol reductions for achieving carbon neutrality in China Y. Yang et al. 10.1016/j.scib.2023.03.048
- Diagnosing uncertainties in global biomass burning emission inventories and their impact on modeled air pollutants W. Hua et al. 10.5194/acp-24-6787-2024
- Investigating the importance of sub-grid particle formation in point source plumes over eastern China using IAP-AACM v1.0 with a sub-grid parameterization Y. Wei et al. 10.5194/gmd-14-4411-2021
- Fast climate responses to emission reductions in aerosol and ozone precursors in China during 2013–2017 J. Gao et al. 10.5194/acp-22-7131-2022
- Aerosol transport pathways and source attribution in China during the COVID-19 outbreak L. Ren et al. 10.5194/acp-21-15431-2021
- Surface temperature response to regional black carbon emissions: do location and magnitude matter? M. Sand et al. 10.5194/acp-20-3079-2020
- Impact of methane and black carbon mitigation on forcing and temperature: a multi-model scenario analysis S. Smith et al. 10.1007/s10584-020-02794-3
- Space–Time Evaluation of Atmospheric Black Carbon in Chinese Urban Environment: Influence of Land Use and Air Pollution Policies A. Shaheen et al. 10.1007/s41748-024-00380-6
- Local and remote climate impacts of future African aerosol emissions C. Wells et al. 10.5194/acp-23-3575-2023
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Latest update: 20 Nov 2024
Short summary
Black carbon (BC) particles exert a potentially large warming influence on the
Earth system. We evaluate regional climate responses, non-linearity, and short-term transient responses to BC emission perturbations. We found that climate responses do not scale linearity with emissions and BC impacts temperature much faster than greenhouse gas forcing. Removing present-day BC emissions results in discernible surface temperature changes for only limited regions of the globe.
Black carbon (BC) particles exert a potentially large warming influence on the
Earth system. We...
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