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An atmospheric perspective on North American carbon dioxide exchange: CarbonTrackerNatural and anthropogenic variations in methane sources during the past two millennia.The global atmospheric environment for the next generation.Regional atmospheric CO2 inversion reveals seasonal and geographic differences in Amazon net biome exchange.The determination of nitrogen dioxide in ambient air with free hanging filters as passive samplers, and a new calibration method using fritted bubblers.Small interannual variability of global atmospheric hydroxyl.Ozone and carbon monoxide budgets over the Eastern Mediterranean.Observational evidence for interhemispheric hydroxyl-radical parity.Iconic CO2 time series at risk.Nitrogen and sulfur deposition on regional and global scales: A multimodel evaluationGlobal inverse modeling of CH<sub>4</sub> sources and sinks: an overview of methodsSatellite chartography of atmospheric methane from SCIAMACHY on board ENVISAT: 2. Evaluation based on inverse model simulationsOn the use of satellite-derived CH<sub>4</sub> : CO<sub>2</sub> columns in a joint inversion of CH<sub>4</sub> and CO<sub>2</sub> fluxesThe effect of stratospheric sulfur from Mount Pinatubo on tropospheric oxidizing capacity and methaneA multi-year methane inversion using SCIAMACHY, accounting for systematic errors using TCCON measurementsAnalysis of global methane changes after the 1991 Pinatubo volcanic eruptionAtmospheric constraints on global emissions of methane from plantsOn the variation of regional CO2exchange over temperate and boreal North AmericaApplication of the CALIOP layer product to evaluate the vertical distribution of aerosols estimated by global models: AeroCom phase I resultsEvaluation of black carbon estimations in global aerosol modelsThe effect of harmonized emissions on aerosol properties in global models – an AeroCom experimentAn AeroCom initial assessment – optical properties in aerosol component modules of global modelsAnalysis and quantification of the diversities of aerosol life cycles within AeroComChange in global aerosol composition since preindustrial timesCan we explain the observed methane variability after the Mount Pinatubo eruption?Inverse modeling of GOSAT-retrieved ratios of total column CH<sub>4</sub> and CO<sub>2</sub> for 2009 and 2010Isotopic evidence for biogenic molecular hydrogen production in the Atlantic OceanEvaluation of the boundary layer dynamics of the TM5 model over EuropeOff-line algorithm for calculation of vertical tracer transport in the troposphere due to deep convectionAtmospheric CH4in the first decade of the 21st century: Inverse modeling analysis using SCIAMACHY satellite retrievals and NOAA surface measurementsTracing the origin and ages of interlaced atmospheric pollution events over the tropical Atlantic Ocean with in situ measurements, satellites, trajectories, emission inventories, and global modelsOrigin of anthropogenic hydrocarbons and halocarbons measured in the summertime european outflow (on Crete in 2001)Modeling the surface–atmosphere exchange of ammoniaInverse modeling of European CH4emissions 2001–2006Impact of transport model errors on the global and regional methane emissions estimated by inverse modellingTransCom model simulations of methane: Comparison of vertical profiles with aircraft measurementsTransCom model simulations of CH<sub>4</sub> and related species: linking transport, surface flux and chemical loss with CH<sub>4</sub> variability in the troposphere and lower stratosphereCan the variability in tropospheric OH be deduced from measurements of 1,1,1-trichloroethane (methyl chloroform)?Reply [to “Comment on “Global OH trend inferred from methylchloroform measurements” by Maarten Krol et al.”]Identification of an El Niño-Southern Oscillation signal in a multiyear global simulation of tropospheric ozone
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0000-0002-3506-2477