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Increase in CFC-11 emissions from eastern China based on atmospheric observations
Increased emissions of trichlorofluoromethane (CFC-11) from eastern China have been identified, contributing significantly to a global rise. This new production and use of CFC-11 is inconsistent with international agreements to phase out ozone-depleting substances.
Area of Science:
- Atmospheric chemistry and environmental science.
- Ozone layer protection and climate change mitigation.
Background:
- Stratospheric ozone layer recovery depends on decreasing ozone-depleting gases like chlorofluorocarbons (CFCs).
- Atmospheric concentrations of CFC-11, a major CFC, declined until recently, but a slowdown suggests increased global emissions.
- A rise in CFC-11 emissions from East Asia was noted, but the source region and scale remained unknown.
Purpose of the Study:
- To investigate and pinpoint the regional source and magnitude of increased CFC-11 emissions in East Asia.
- To determine the contribution of East Asian emissions to the global increase in CFC-11.
- To assess compliance with the Montreal Protocol regarding CFC production and use.
Main Methods:
- Utilized high-frequency atmospheric observations from South Korea and Japan.
- Integrated global monitoring data with atmospheric chemical transport model simulations.
- Analyzed CFC-11 emission changes between 2008-2012 and 2014-2017.
Main Results:
- Identified significant CFC-11 emissions from eastern mainland China, 7.0 ± 3.0 Gg/year higher in 2014-2017 than 2008-2012.
- Localized the emission increase primarily to the Shandong and Hebei provinces in northeastern China.
- Determined that these Chinese emissions accounted for 40-60% of the global CFC-11 emission rise.
- Found no evidence of significant CFC-11 emission increases from other East Asian countries or other monitored global regions.
Conclusions:
- The increase in CFC-11 emissions from eastern China is likely due to new production and usage.
- This finding contradicts the Montreal Protocol's phase-out of global CFC production by 2010.
- Further monitoring is needed to attribute the remaining global CFC-11 emission rise due to sparse data in potential source regions.
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