G
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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Journal ArticleDOI
A large atomic chlorine source inferred from mid-continental reactive nitrogen chemistry
Joel A. Thornton,James P. Kercher,Theran P. Riedel,Nicholas L. Wagner,J. Cozic,John S. Holloway,William P. Dubé,Glenn M. Wolfe,Patricia K. Quinn,Ann M. Middlebrook,Becky Alexander,Steven S. Brown +11 more
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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Insights into hydroxyl measurements and atmospheric oxidation in a California forest
Jingqiu Mao,Jingqiu Mao,Xinrong Ren,Ling Zhang,D. M. Van Duin,Ronald C. Cohen,Jeong-Hoo Park,Allen H. Goldstein,Fabien Paulot,Fabien Paulot,M. R. Beaver,M. R. Beaver,John D. Crounse,Paul O. Wennberg,Joshua P. DiGangi,Joshua P. DiGangi,S. B. Henry,Frank N. Keutsch,Chiwook Park,Chiwook Park,Gunnar W. Schade,Glenn M. Wolfe,Glenn M. Wolfe,Joel A. Thornton,William H. Brune +24 more
TL;DR: In this paper, a new chemical removal method was used to measure hydroxyl (OH) in a California forest environment using laser-induced fluorescence in low pressure detection chambers (called Fluorescence Assay with Gas Expansion (FAGE)) using the Penn State Ground-based Tropospheric Hydrogen Oxides Sensor (GTHOS).
Journal ArticleDOI
Rapid deposition of oxidized biogenic compounds to a temperate forest
Tran B. Nguyen,John D. Crounse,Alex P. Teng,Jason M. St. Clair,Fabien Paulot,Fabien Paulot,Glenn M. Wolfe,Glenn M. Wolfe,Paul O. Wennberg +8 more
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.
Journal ArticleDOI
Airborne measurements of western U.S. wildfire emissions: Comparison with prescribed burning and air quality implications
Xiaoxi Liu,Xiaoxi Liu,Xiaoxi Liu,L. Gregory Huey,Robert J. Yokelson,Vanessa Selimovic,Isobel J. Simpson,Markus Müller,Markus Müller,Jose L. Jimenez,Jose L. Jimenez,Pedro Campuzano-Jost,Pedro Campuzano-Jost,Andreas J. Beyersdorf,Andreas J. Beyersdorf,Donald R. Blake,Zachary Butterfield,Zachary Butterfield,Yonghoon Choi,John D. Crounse,Douglas A. Day,Douglas A. Day,Glenn S. Diskin,Manvendra K. Dubey,Edward C. Fortner,Thomas F. Hanisco,Weiwei Hu,Weiwei Hu,L. King,Lawrence I. Kleinman,Simone Meinardi,Tomas Mikoviny,Timothy B. Onasch,Brett B. Palm,Brett B. Palm,Jeff Peischl,Jeff Peischl,Ilana B. Pollack,Ilana B. Pollack,Ilana B. Pollack,Thomas B. Ryerson,Glen W. Sachse,Arthur J. Sedlacek,John E. Shilling,Stephen R. Springston,Jason M. St. Clair,Jason M. St. Clair,Jason M. St. Clair,David J. Tanner,Alex P. Teng,Paul O. Wennberg,Armin Wisthaler,Armin Wisthaler,Glenn M. Wolfe,Glenn M. Wolfe +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).
Journal ArticleDOI
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.