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Glenn M. Wolfe

Researcher at University of Maryland, Baltimore County

Publications -  98
Citations -  4863

Glenn M. Wolfe is an academic researcher from University of Maryland, Baltimore County. The author has contributed to research in topics: NOx & Troposphere. The author has an hindex of 36, co-authored 86 publications receiving 3818 citations. Previous affiliations of Glenn M. Wolfe include University of Washington & Goddard Space Flight Center.

Papers
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A large atomic chlorine source inferred from mid-continental reactive nitrogen chemistry

TL;DR: Comparison of these findings to model predictions based on aerosol and precipitation composition data from long-term monitoring networks suggests nitryl chloride production in the contiguous USA alone is at a level similar to previous global estimates for coastal and marine regions and that a significant fraction of tropospheric chlorine atoms may arise directly from anthropogenic pollutants.
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Rapid deposition of oxidized biogenic compounds to a temperate forest

TL;DR: The chemically speciated fluxes presented here comprise a unique and novel dataset that quantifies the dry deposition velocities for a variety of trace gases in a typical forested ecosystem, and suggests that dry deposition is the dominant daytime sink for small, saturated oxygenates.
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Airborne measurements of western U.S. wildfire emissions: Comparison with prescribed burning and air quality implications

Xiaoxi Liu, +54 more
TL;DR: In this paper, an extensive set of emission factors (EFs) for over 80 gases and 5 components of submicron particulate matter (PM_1) from three wildfires in the western U.S. were measured from aircraft during the Studies of Emissions and Atmospheric Composition, Clouds and Climate Coupling by Regional Surveys (SEAC^4RS) and the Biomass Burning Observation Project (BBOP).
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The effect of varying levels of surfactant on the reactive uptake of N 2 O 5 to aqueous aerosol

TL;DR: In this article, the authors studied the effect of varying levels of surfactant on gas-aerosol reaction rates and found that the presence of 3.5wt% SDS in the aerosol, which corresponds to a monolayer surface coverage of 2×1014 molecules cm-2, suppresses the N2O5 reaction probability by approximately a factor of ten, independent of relative humidity.