期刊
GEOPHYSICAL RESEARCH LETTERS
卷 41, 期 7, 页码 2623-2630出版社
AMER GEOPHYSICAL UNION
DOI: 10.1002/2013GL059099
关键词
inverse modeling; radiative forcing; synthetic greenhouse gas
资金
- UK Natural Environment Research Council (NERC) [NE/I021365/1]
- NASA Upper Atmospheric Research Program in the U.S. [NNX11AF17G, NNX11AF15G, NNX11AF16G]
- NOAA
- UK Department of Food and Rural Affairs (DEFRA)
- Department for Energy and Climate Change (DECC) in the UK
- CSIRO
- Australian Government Bureau of Meteorology in Australia
- NERC [NE/L013088/1, NE/I021365/1] Funding Source: UKRI
- Natural Environment Research Council [NE/I021365/1, NE/L013088/1] Funding Source: researchfish
- NASA [NNX11AF15G, 146891, NNX11AF16G, 147009] Funding Source: Federal RePORTER
Atmospheric measurements show that emissions of hydrofluorocarbons (HFCs) and hydrochlorofluorocarbons are now the primary drivers of the positive growth in synthetic greenhouse gas (SGHG) radiative forcing. We infer recent SGHG emissions and examine the impact of future emissions scenarios, with a particular focus on proposals to reduce HFC use under the Montreal Protocol. If these proposals are implemented, overall SGHG radiative forcing could peak at around 355mWm(-2) in 2020, before declining by approximately 26% by 2050, despite continued growth of fully fluorinated greenhouse gas emissions. Compared to no HFC policy projections, this amounts to a reduction in radiative forcing of between 50 and 240mWm(-2) by 2050 or a cumulative emissions saving equivalent to 0.5 to 2.8years of CO2 emissions at current levels. However, more complete reporting of global HFC emissions is required, as less than half of global emissions are currently accounted for.
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