Radiative forcing estimates in 2011 relative to 1750 and aggregated uncertainties for the main drivers of climate change
Metadata
-
Last upload:
- 09 Feb 2015
-
Temporal coverage:
- 1750 , 2011
-
Tags:
- climate change drivers , radiative forcing
-
Geographic coverage:
-
Rights:
- Unless otherwise stated, the information available on this website, including text, logos, graphics, maps, images, audio clips and electronic downloads is the property of the IPCC and is protected by intellectual property laws.
You may freely download and copy the material contained on this website for your personal, non-commercial use, without any right to resell, redistribute, compile or create derivative works therefrom, subject to more specific restrictions that may apply to specific materials.
Reproduction of a limited number of figures or short excerpts of IPCC material is authorized free of charge and without formal written permission provided that the original source is properly acknowledged, with mention of the name of the report, the publisher and the numbering of the page(s) or the figure(s). Permission can only be granted to use the material exactly as it is in the report. Please be aware that figures cannot be altered in any way, including the full legend.
Further information:
https://www.ipcc.ch/report/graphics/ -
Owners:
- Intergovernmental Panel on Climate Change (IPCC)
-
Figure type:
- Graph
Additional information
Values are global average radiative forcing (RF14), partitioned according to the emitted compounds or processes that result in a combination of drivers. The best estimates of the net radiative forcing are shown as black diamonds with corresponding uncertainty intervals; the numerical values are provided on the right of the figure, together with the confidence level in the net forcing (VH – very high, H – high, M – medium, L – low, VL – very low). Albedo forcing due to black carbon on snow and ice is included in the black carbon aerosol bar. Small forcings due to contrails (0.05 W m-2, including contrail induced cirrus), and HFCs, PFCs and SF6 (total 0.03 W m–2) are not shown. Concentration-based RFs for gases can be obtained by summing the like-coloured bars. Volcanic forcing is not included as its episodic nature makes is difficult to compare to other forcing mechanisms. Total anthropogenic radiative forcing is provided for three different years relative to 1750.
For further technical details, including uncertainty ranges associated with individual components and processes, see the Technical Summary Supplementary Material.
https://www.ipcc.ch/pdf/assessment-report/ar5/wg1/supplementary/WG1AR5_TSSM_FINAL.pdf
{8.5; Figures 8.14–8.18; Figures TS.6 and TS.7}
Permalinks
- Permalink to this version
- 61bb710bffa745dba238e4bc6f8367cc
- Permalink to latest version
- TNVOMCKD7S
For references, please go to https://www.eea.europa.eu/data-and-maps/figures/radiative-forcing-estimates-in-2011 or scan the QR code.
PDF generated on 21 Aug 2019, 06:17 AM
Document Actions
Share with others