Articles | Volume 12, issue 3
https://doi.org/10.5194/essd-12-1649-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/essd-12-1649-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Data description paper
| 
16 Jul 2020
Data description paper |
| 16 Jul 2020
| 16 Jul 2020
Radiative forcing of climate change from the Copernicus reanalysis of atmospheric composition
Nicolas Bellouin
CORRESPONDING AUTHOR
Department of Meteorology, University of Reading, Reading, RG6 6BB,
UK
Will Davies
Department of Meteorology, University of Reading, Reading, RG6 6BB,
UK
Keith P. Shine
Department of Meteorology, University of Reading, Reading, RG6 6BB,
UK
Johannes Quaas
Institute for Meteorology, Universität Leipzig, 04103 Leipzig,
Germany
Johannes Mülmenstädt
Institute for Meteorology, Universität Leipzig, 04103 Leipzig,
Germany
now at: Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, Washington, USA
Piers M. Forster
Priestley International Centre for Climate, University of Leeds, Leeds, LS2 9JT, UK
Chris Smith
Priestley International Centre for Climate, University of Leeds, Leeds, LS2 9JT, UK
Lindsay Lee
Institute for Climate and Atmospheric Science, University of Leeds,
Leeds, LS2 9JT, UK
now at: Department of Engineering and Mathematics, Sheffield Hallam
University, Sheffield, S1 1WB, UK
Leighton Regayre
Institute for Climate and Atmospheric Science, University of Leeds,
Leeds, LS2 9JT, UK
Guy Brasseur
Max Planck Institute for Meteorology, 20146 Hamburg, Germany
Natalia Sudarchikova
Max Planck Institute for Meteorology, 20146 Hamburg, Germany
Idir Bouarar
Max Planck Institute for Meteorology, 20146 Hamburg, Germany
Olivier Boucher
Institut Pierre-Simon Laplace, Sorbonne Université/CNRS, Paris
75252, France
Gunnar Myhre
Center for International Climate and Environmental Research Oslo
(CICERO), 0318 Oslo, Norway
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- Changes in Clear‐Sky Shortwave Aerosol Direct Radiative Effects Since 2002 N. Loeb et al. 10.1029/2020JD034090
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- Ionic Distribution of an Unequal Electrolyte Near an Air/Water Surface C. Phan et al. 10.5650/jos.ess23140
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- Comprehensive study of aerosols properties over various terrain types N. Srivastava & M. Kumar 10.1007/s10661-022-10536-4
- Climatology of aerosol component concentrations derived from multi-angular polarimetric POLDER-3 observations using GRASP algorithm L. Li et al. 10.5194/essd-14-3439-2022
- Global spatiotemporal completion of daily high-resolution TCCO from TROPOMI over land using a swath-based local ensemble learning method Y. Wang et al. 10.1016/j.isprsjprs.2022.10.012
- The effect of climate change on the dynamics of a modified surface energy balance-mass balance model of Cryosphere under the frame of a non-local operator A. Chakraborty et al. 10.1016/j.rinp.2023.107031
- The role of direct air capture and negative emissions technologies in the shared socioeconomic pathways towards +1.5 °C and +2 °C futures J. Fuhrman et al. 10.1088/1748-9326/ac2db0
- Causes of increased pollen exposure during Saharan-Sahel dust intrusions J. Rojo et al. 10.1016/j.envpol.2021.117441
- An assessment of four decades atmospheric PM2.5 trends in urban locations over Southern Africa using MERRA-2 reanalysis M. Nyasulu et al. 10.1007/s11869-023-01392-3
- Constraining the Twomey effect from satellite observations: issues and perspectives J. Quaas et al. 10.5194/acp-20-15079-2020
- Estimates of Variations in Radiative Forcing of Methane in the Past and in the Future S. Akishina et al. 10.1134/S1024856024010020
Latest update: 23 Apr 2024
Short summary
Quantifying the imbalance in the Earth's energy budget caused by human activities is important to understand and predict climate changes. This study presents new estimates of the imbalance caused by changes in atmospheric concentrations of carbon dioxide, methane, ozone, and particles of pollution. Over the period 2003–2017, the overall imbalance has been positive, indicating that the climate system has gained energy and will warm further.
Quantifying the imbalance in the Earth's energy budget caused by human activities is important...
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