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Bibliographical noteFunding Information:
This work was supported by the National Key Research and Development Program of China (Grant No. 2019YFC0214500). We are thankful for the stations personnel who have supported the in situ measurements and daily or weekly canister sampling at SDZ, WLG, LAN, LFS, XGL, JGJ, XGF, AKD, JSA. This work has benefited from the technical expertise of and assistance by the AGAGE (Advanced Global Atmospheric Gases Experiment) network including the Medusa GC/MS system technology, calibrations of CH2Cl2 measurements and network operation, as well as Dr. Martin Vollmer from Swiss Federal Laboratories for Materials Science and Technology. We acknowledge the support from members of Atmospheric Chemistry Research Group at University of Bristol. Measurements at the Mace Head, Trinidad Head, Ragged Point, Cape Matatula, and Cape Grim AGAGE stations are supported by the National Aeronautics and Space Administration (NASA) (grants NNX-16AC98G to MIT, and NNX16AC97G and NNX16AC96G to SIO). Support also comes from the UK Department for Business, Energy & Industrial Strategy (BEIS, Contract 1537/06/2018 to the University of Bristol) for Mace Head, the National Oceanic and Atmospheric Administration (NOAA, Contract RA-133-R15-CN-0008 and 1305M319CNRMJ0028 to the University of Bristol) for Ragged Point, and the Commonwealth Scientific and Industrial Research Organization (CSIRO) and the Bureau of Meteorology (Australia) for Cape Grim. R.H. is supported by a NERC Independent Research Fellowship (NE/N014375/1) and the NERC ISHOC project (NE/R004927/1). L.M.W. and M.R. received funding from NERC grants NE/ M014851/1, NE/N016548/1 and NE/S004211/1, and L.M.W. received funding from the European Union’s Horizon 2020 research and innovation programme under the Marie Skłodowska-Curie grant agreement No 101030750. A.L.G. was supported by U.K. Natural Environment Research Council (NERC) Independent Research Fellowship (NE/ L010992/1).
© 2021, The Author(s).
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