2018
DOI: 10.5194/acp-2017-1171
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Inverse modelling of CF<sub>4</sub> and NF<sub>3</sub> emissions in East Asia

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Cited by 2 publications
(4 citation statements)
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“…20,000 particles per hour were transported backward in time for 30 days in NAME in a domain bounded at 5°S and 74°N and 55°E and 192°E. When particles are within the lowest m of the atmosphere, it was assumed that they interacted with the surface and could intercept emissions sources 17,23 . The NAME-HB framework uses a climatological a priori estimate of the mole fraction at the boundary of the domain from the NASA 3D GEOS Chemistry Climate Model 27 .…”
Section: Regional Atmospheric Chemical Transport Modelsmentioning
confidence: 99%
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“…20,000 particles per hour were transported backward in time for 30 days in NAME in a domain bounded at 5°S and 74°N and 55°E and 192°E. When particles are within the lowest m of the atmosphere, it was assumed that they interacted with the surface and could intercept emissions sources 17,23 . The NAME-HB framework uses a climatological a priori estimate of the mole fraction at the boundary of the domain from the NASA 3D GEOS Chemistry Climate Model 27 .…”
Section: Regional Atmospheric Chemical Transport Modelsmentioning
confidence: 99%
“…Output from NAME was also used with the InTEM inversion framework (NAME-InTEM) 17 . Emissions and uncertainties were averaged across the 24 individual inversions thereby assuming 100% correlation between uncertainties in these separate inversions.…”
Section: Regional Inversion Frameworkmentioning
confidence: 99%
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