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Significant changes have occurred in the anthropogenic emissions of many compounds related to the Kyoto and Montreal Protocols within the past 20 years and many of their atmospheric abundances have responded dramatically. Additionally, there are a number of related natural compounds with underdetermined source or sink budgets. A new instrument, Medusa, was developed to make the high frequency in situ measurements required for the determination of the atmospheric lifetimes and emissions of these compounds. This automated system measures a wide range of halocarbons, hydrocarbons, and sulfur compounds involved in ozone depletion and/or climate forcing, from the very volatile perfluorocarbons (PFCs, e.g., CF(4) and CH(3)CF(3)) and hydrofluorocarbons (HFCs, e.g., CH(3)CF(3)) to the higher-boiling point solvents (such as CH(3)Cl(3) and CCl(2)=CCl(2)) and CHBr(3). A network of Medusa systems worldwide provides 12 in situ ambient air measurements per day of more than 38 compounds of part per trillion mole fractions and precisions up to 0.1% RSD at the five remote field stations operated by the Advanced Global Atmospheric Gases Experiment (AGAGE). This custom system couples gas chromatography/mass spectrometry (GC/MSD) with a novel scheme for cryogen-free low-temperature preconcentration (-165 degrees C) of analytes from 2 L samples in a two-trap process using HayeSep D adsorbent.
Abstract. We present the organization, instrumentation, datasets, data interpretation, modeling, and accomplishments of the multinational global atmospheric measurement program AGAGE (Advanced Global Atmospheric Gases Experiment). AGAGE is distinguished by its capability to measure globally, at high frequency, and at multiple sites all the important species in the Montreal Protocol and all the important non-carbon-dioxide (non-CO 2 ) gases assessed by the Intergovernmental Panel on Climate Change (CO 2 is also measured at several sites). The scientific objectives of AGAGE are important in furthering our understanding of global chemical and climatic phenomena. They are the following: (1) to accurately measure the temporal and spatial distributions of anthropogenic gases that contribute the majority of reactive halogen to the stratosphere and/or are strong infrared absorbers (chlorocarbons, chlorofluorocarbons – CFCs, bromocarbons, hydrochlorofluorocarbons – HCFCs, hydrofluorocarbons – HFCs and polyfluorinated compounds (perfluorocarbons – PFCs), nitrogen trifluoride – NF 3 , sulfuryl fluoride – SO 2 F 2 , and sulfur hexafluoride – SF 6 ) and use these measurements to determine the global rates of their emission and/or destruction (i.e., lifetimes); (2) to accurately measure the global distributions and temporal behaviors and determine the sources and sinks of non-CO 2 biogenic–anthropogenic gases important to climate change and/or ozone depletion (methane – CH 4 , nitrous oxide – N 2 O, carbon monoxide – CO, molecular hydrogen – H 2 , methyl chloride – CH 3 Cl, and methyl bromide – CH 3 Br); (3) to identify new long-lived greenhouse and ozone-depleting gases (e.g., SO 2 F 2 , NF 3 , heavy PFCs (C 4 F 10 , C 5 F 12 , C 6 F 14 , C 7 F 16 , and C 8 F 18 ) and hydrofluoroolefins (HFOs; e.g., CH 2 = CFCF 3 ) have been identified in AGAGE), initiate the real-time monitoring of these new gases, and reconstruct their past histories from AGAGE, air archive, and firn air measurements; (4) to determine the average concentrations and trends of tropospheric hydroxyl radicals (OH) from the rates of destruction of atmospheric trichloroethane (CH 3 CCl 3 ), HFCs, and HCFCs and estimates of their emissions; (5) to determine from atmospheric observations and estimates of their destruction rates the magnitudes and distributions by region of surface sources and sinks of all measured gases; (6) to provide accurate data on the global accumulation of many of these trace gases that are used to test the synoptic-, regional-, and global-scale circulations predicted by three-dimensional models; and (7) to provide global and regional measurements of methane, carbon monoxide, and molecular hydrogen and estimates of hydroxyl levels to test primary atmospheric oxidation pathways at midlatitudes and the tropics. Network Information and Data Repository: http://agage.mit.edu/data or http://cdiac.ess-dive.lbl.gov/ndps/alegage.html ( https://doi.org/10.3334/CDIAC/atg.db1001 ).
[1
]State Key Joint Laboratory for Environmental Simulation and Pollution Control, College
of Environmental Sciences and Engineering, Peking University, Beijing 100871, China
[2
]School of Chemistry, University of Bristol, Bristol BS8 1TS, U.K.
[3
]Beijing Huanaco Innovation Co., Ltd., Beijing 102400, China
[4
]Institute of Urban Meteorology, China Meteorological Administration, Beijing 100089,
China
[5
]Global Monitoring Laboratory, National Oceanic and Atmospheric Administration, Boulder,
Colorado 80305, United States
[6
]School of Geographical Sciences, University of Bristol, Bristol BS8 1SS, U.K.
[7
]Department of Atmospheric and Oceanic Sciences & Institute of Atmospheric Sciences,
Fudan University, Shanghai 200438, China
[8
]Meteorological Observation Centre of China Meteorological Administration (MOC/CMA),
Beijing 100081, China
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