11 results on '"Ensberg, J J"'
Search Results
2. Impacts of electronically photo-excited NO2 on air pollution in the South Coast Air Basin of California
- Author
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Ensberg, J. J, Carreras-Sospedra, M., and Dabdub, D.
- Subjects
sensitivity-analysis ,chemical mechanism ,ozone ,quality ,uncertainty ,rethinking ,emissions ,weekday - Abstract
A new path for hydroxyl radical formation via photo-excitation of nitrogen dioxide (NO2) and the reaction of photo-excited NO2 with water is evaluated using the UCI-CIT model for the South Coast Air Basin of California (SoCAB). Two separate studies predict different reaction rates, which differ by nearly an order of magnitude, for the reaction of photo-excited NO2 with water. Impacts of this new chemical mechanism on ozone and particulate matter formation, while utilizing both reaction rates, are quantified by simulating two summer episodes. First, sensitivity simulations are conducted to evaluate the uncertainty in the rate of reaction of photo-excited NO2 with water reported in the literature. Results indicate that the addition of photo-excited NO2 chemistry increases peak 8-h average ozone and particulate matter concentrations. The importance of this new chemistry is then evaluated in the context of pollution control strategies. A series of simulations are conducted to generate isopleths for ozone and particulate matter concentrations, varying baseline nitrogen oxides (NOx) and volatile organic compounds (VOC) emissions. Isopleths are obtained using 1987 emissions, to represent past conditions, and 2005, to represent current conditions in the SoCAB. Results show that the sensitivity of modeled pollutant control strategies due to photoexcitation decreases with the decrease in baseline emissions from 1987 to 2005. Results show that including NO2 photo-excitation, increases the sensitivity of ozone concentration with respect to changes in NOx emissions for both years. In particular, decreasing NOx emissions in 2005 when NO2 photo-excitation is included, while utilizing the higher reaction rate, leads to ozone relative reduction factors that are 15% lower than in a case without photo-excited NO2. This implies that photoexcitation increases the effectiveness in reducing ozone through NOx emissions reductions alone, which has implications for the assessment of future emission control strategies. However, there is still disagreement with respect to the reaction rate constant for the formation of OH. Therefore, further studies are required to reduce the uncertainty in the reaction rate constant before this new mechanism is fully implemented in regulatory applications.
- Published
- 2010
3. Inorganic and black carbon aerosols in the Los Angeles Basin during CalNex
- Author
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Ensberg, J. J., Craven, J. S., Metcalf, A. R., Allan, J. D., Angevine, W. M., Bahreini, R., Brioude, J., Cai, C., Coe, H., De Gouw, J. A., Ellis, R. A., Flynn, J. H., Haman, C. L., Hayes, P. L., Jimenez, J. L., Lefer, B. L., Middlebrook, A. M., Murphy, J. G., Neuman, J. A., Nowak, J. B., Roberts, J. M., Stutz, J., Taylor, J. W., Veres, P. R., Walker, J. M., and Seinfeld, J. H.
- Subjects
particulate matter ,mexico-city ,Atmospheric Science ,inorganic ,modeling ,source apportionment ,thermodynamic-equilibrium ,mass-spectrometry ,calnex ,black carbon ,los angeles ,pittsburgh supersite ,Geophysics ,southern california ,Space and Planetary Science ,Earth and Planetary Sciences (miscellaneous) ,single-particle analysis ,chemical-composition ,california air-quality - Abstract
We evaluate predictions from the Community Multiscale Air Quality (CMAQ version 4.7.1) model against a suite of airborne and ground-based meteorological measurements, gas- and aerosol-phase inorganic measurements, and black carbon (BC) measurements over Southern California during the CalNex field campaign in May/June 2010. Ground-based measurements are from the CalNex Pasadena ground site, and airborne measurements took place onboard the Center for Interdisciplinary Remotely-Piloted Aircraft Studies (CIRPAS) Navy Twin Otter and the NOAA WP-3D aircraft. BC predictions are in general agreement with observations at the Pasadena ground site and onboard the WP-3D, but are consistently overpredicted when compared to Twin Otter measurements. Adjustments to predicted inorganic mass concentrations, based on predicted aerosol size distributions and the AMS transmission efficiency, are shown to be significant. Owing to recent shipping emission reductions, the dominant source of sulfate in the L.A. Basin may now be long-range transport. Sensitivity studies suggest that severely underestimated ammonia emissions, and not the exclusion of crustal species (Ca2 +, K+, and Mg2 +), are the single largest contributor to measurement/model disagreement in the eastern part of the L.A. Basin. Despite overstated NOx emissions, total nitrate concentrations are underpredicted, which suggests a missing source of HNO 3 and/or overprediction of deposition rates. Adding gas-phase NH 3 measurements and size-resolved measurements, up to 10 μm, of nitrate and various cations (e.g. Na+, Ca2 +, K +) to routine monitoring stations in the L.A. Basin would greatly facilitate interpreting day-to-day fluctuations in fine and coarse inorganic aerosol. Key pointsWe measured inorganic gas- and aerosol-phase species during CalNexWe compare ground-based and airborne measurements to CMAQ predictionsMeasure/model agreement varies depending on the species and location © 2012. American Geophysical Union. All Rights Reserved.
- Published
- 2013
- Full Text
- View/download PDF
4. Black carbon aerosol over the Los Angeles Basin during CalNex
- Author
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Metcalf, A. R., Craven, J. S., Ensberg, J. J., Brioude, J., Angevine, W., Sorooshian, A., Duong, H. T., Jonsson, H. H., Flagan, R. C., and Seinfeld, J. H.
- Abstract
Refractory black carbon (rBC) mass and number concentrations were quantified by a Single Particle Soot Photometer (SP2) in the CalNex 2010 field study on board the Center for Interdisciplinary Remotely-Piloted Aircraft Studies (CIRPAS) Twin Otter in the Los Angeles (LA) Basin in May, 2010. The mass concentrations of rBC in the LA Basin ranged from 0.002–0.530 μg m^(−3), with an average of 0.172 μg m^(−3). Lower concentrations were measured in the Basin outflow regions and above the inversion layer. The SP2 afforded a quantification of the mixing state of rBC aerosols through modeling the scattering cross-section with a core-and-shell Mie model to determine coating thickness. The rBC particles above the inversion layer were more thickly coated by a light-scattering substance than those below, indicating a more aged aerosol in the free troposphere. Near the surface, as the LA plume is advected from west to east with the sea breeze, a coating of scattering material grows on rBC particles, coincident with a clear growth of ammonium nitrate within the LA Basin and the persistence of water-soluble organic compounds as the plume travels through the outflow regions. Detailed analysis of the rBC mixing state reveals two modes of coated rBC particles; a mode with smaller rBC core diameters (∼90 nm) but thick (>200 nm) coating diameters and a mode with larger rBC cores (∼145 nm) with a thin (
- Published
- 2012
5. Black Carbon Aerosol over the Los Angeles Basin during CalNex
- Author
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NAVAL POSTGRADUATE SCHOOL MONTEREY CA, Metcalf, A R, Craven, J S, Ensberg, J J, Brioude, J, Angevine, W, Sorooshian, A, Duong, H T, Jonsson, H H, Flagan, R C, Seinfeld, J H, NAVAL POSTGRADUATE SCHOOL MONTEREY CA, Metcalf, A R, Craven, J S, Ensberg, J J, Brioude, J, Angevine, W, Sorooshian, A, Duong, H T, Jonsson, H H, Flagan, R C, and Seinfeld, J H
- Abstract
Refractory black carbon (rBC) mass and number concentrations were quantified by a Single Particle Soot Photometer (SP2) in the CalNex 2010 field study on board the Center for Interdisciplinary Remotely-Piloted Aircraft Studies (CIRPAS) Twin Otter in the Los Angeles (LA) Basin in May, 2010. The mass concentrations of rBC in the LA Basin ranged from 0.002 0.530 micro g m(expn -3), with an average of 0.172 micro g m(expn -3). Lower concentrations were measured in the Basin outflow regions and above the inversion layer. The SP2 afforded a quantification of the mixing state of rBC aerosols through modeling the scattering cross-section with a core-and-shell Mie model to determine coating thickness. The rBC particles above the inversion layer were more thickly coated by a light-scattering substance than those below, indicating a more aged aerosol in the free troposphere. Near the surface, as the LA plume is advected from west to east with the sea breeze, a coating of scattering material grows on rBC particles, coincident with a clear growth of ammonium nitrate within the LA Basin and the persistence of water-soluble organic compounds as the plume travels through the outflow regions. Detailed analysis of the rBC mixing state reveals two modes of coated rBC particles; a mode with smaller rBC core diameters (90 nm) but thick (200 nm) coating diameters and a mode with larger rBC cores (145 nm) with a thin (75 nm) coating. The weekend effect in the LA Basin results in more thickly coated rBC particles, coinciding with more secondary formation of aerosol., Published in the Journal of Geophysical Research, v117 article ID D00V13, 20 Apr 2012. Prepared in cooperation with the Division of Engineering and Applied Science, California Institute of Technology, Pasadena, the Division of Chemistry and Chemical Engineering, California Institute of Technology, Pasadena, the Chemical Sciences Division, NOAA Earth System Research Laboratory, Boulder, CO, the Department of Chemical and Environmental Engineering, University of Arizona, Tucson, and the Department of Atmospheric Sciences, University of Arizona, Tucson.
- Published
- 2012
6. Emission factor ratios, SOA mass yields, and the impact of vehicular emissions on SOA formation
- Author
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Ensberg, J. J., primary, Hayes, P. L., additional, Jimenez, J. L., additional, Gilman, J. B., additional, Kuster, W. C., additional, de Gouw, J. A., additional, Holloway, J. S., additional, Gordon, T. D., additional, Jathar, S., additional, Robinson, A. L., additional, and Seinfeld, J. H., additional
- Published
- 2014
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7. Emission factor ratios, SOA mass yields, and the impact of vehicular emissions on SOA formation
- Author
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Ensberg, J. J., primary, Hayes, P. L., additional, Jimenez, J. L., additional, Gilman, J. B., additional, Kuster, W. C., additional, de Gouw, J. A., additional, Holloway, J. S., additional, and Seinfeld, J. H., additional
- Published
- 2013
- Full Text
- View/download PDF
8. Inorganic and black carbon aerosols in the Los Angeles Basin during CalNex
- Author
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Ensberg, J. J., primary, Craven, J. S., additional, Metcalf, A. R., additional, Allan, J. D., additional, Angevine, W. M., additional, Bahreini, R., additional, Brioude, J., additional, Cai, C., additional, Coe, H., additional, de Gouw, J. A., additional, Ellis, R. A., additional, Flynn, J. H., additional, Haman, C. L., additional, Hayes, P. L., additional, Jimenez, J. L., additional, Lefer, B. L., additional, Middlebrook, A. M., additional, Murphy, J. G., additional, Neuman, J. A., additional, Nowak, J. B., additional, Roberts, J. M., additional, Stutz, J., additional, Taylor, J. W., additional, Veres, P. R., additional, Walker, J. M., additional, and Seinfeld, J. H., additional
- Published
- 2013
- Full Text
- View/download PDF
9. Black carbon aerosol over the Los Angeles Basin during CalNex
- Author
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Metcalf, A. R., primary, Craven, J. S., additional, Ensberg, J. J., additional, Brioude, J., additional, Angevine, W., additional, Sorooshian, A., additional, Duong, H. T., additional, Jonsson, H. H., additional, Flagan, R. C., additional, and Seinfeld, J. H., additional
- Published
- 2012
- Full Text
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10. Impacts of electronically photo-excited NO<sub>2</sub> on air pollution control strategies in the South Coast Air Basin of California
- Author
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Ensberg, J. J., primary, Carreras-Sospedra, M., additional, and Dabdub, D., additional
- Published
- 2009
- Full Text
- View/download PDF
11. Emission factor ratios, SOA mass yields, and the impact of vehicular emissions on SOA formation.
- Author
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Ensberg, J. J., Hayes, P. L., Jimenez, J. L., Gilman, J. B., Kuster, W. C., de Gouw, J. A., Holloway, J. S., and Seinfeld, J. H.
- Abstract
The underprediction of ambient secondary organic aerosol (SOA) levels by atmospheric models in urban areas is well established, yet the cause of this underprediction remains elusive. Likewise, the relative contribution of emissions from gasoline- and diesel-fueled vehicles to the formation of SOA is generally unresolved. Here we address these two issues using data from the 2010 CalNex experiment carried out in the Los Angeles basin (Ryerson et al., 2013). We use gas-phase organic mass (GPOM) and CO emission factors in conjunction with measured enhancements in oxygenated organic aerosol (OOA) relative to CO to investigate the relative importance of gasoline vs. diesel emissions to organic aerosol formation. Two possible conclusions emerge from the analysis to yield consistency with the ambient data: (1) vehicular emissions are not a dominant source of anthropogenic fossil SOA in the Los Angeles basin, or (2) ambient SOA mass yields are substantially higher than those derived from laboratory chamber studies. [ABSTRACT FROM AUTHOR]
- Published
- 2013
- Full Text
- View/download PDF
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