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Impacts of changing U.S. NOx emissions on ozone pollution: Insights from satellites, ground-based measurements and air quality models Arlene M. Fiore ExxonMobil Research and Engineering NOx Controls Workshop Bridgewater, NJ January 12, 2016
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Attaining the U.S. National Ambient Air Quality Standards (NAAQS) for ozone remains a challenge
One or more NAAQS 142.2 Ozone (8-hour) 133.2 PM2.5 (annual/24-hr) 28.2 PM10 (24-hr) PM10 (24hr) 16.1 SO2 (1-hr) 15.1 Lead (3-month) 8.1 NO2 (annual/1-hr) 2012 CO (8-hr) Millions of people living in counties with air quality concentrations above the level of the U.S. National Ambient Air Quality Standards EPA, 2014:
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Today’s topics Introduction to atmospheric chemistry of ozone formation and destruction Influence of U.S. NOx controls on ozone air quality Overview of air quality modeling Current research directions and challenges -- Role of natural NOx sources -- Accuracy of emission inventories -- Source attribution for ozone (anthropogenic, biogenic, background components) -- Changing climate
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Introduction to ozone pollution chemistry
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Ground-level O3 is produced photochemically in the atmosphere, from both natural and anthropogenic sources Raises background ozone levels CH4 NMVOC + Fuel local-to-regional ozone pollution episodes NOx O3 Observed surface ozone includes background plus any ozone produced from local-to-regional emissions
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Tropospheric O3 formation & “Background” contributions
stratosphere lightning “Background” ozone Natural sources Continent X hn intercontinental transport NO2 NO OH HO2 VOC, CH4, CO Human activity Fires Land Biosphere (NMVOC, NOx) Ocean Continent
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Regional average loss pathways for ozone in (polluted) U. S
Regional average loss pathways for ozone in (polluted) U.S. boundary layer Percentage (%) of total ozone (Ox) lost via each pathway, estimated with the GEOS-Chem chemical transport model for summer 1995 Fiore et al., Journal of Geophysical Research, 2002 deposition dominates O3 photolysis followed by OH production and O3 + HOx also important In high NOx settings (urban, power plant plumes) O3 titration by NO also occurs
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Regional average loss pathways for ozone in (polluted) U. S
Regional average loss pathways for ozone in (polluted) U.S. boundary layer Percentage (%) of total ozone (Ox) lost via each pathway, estimated with the GEOS-Chem chemical transport model for summer 1995 WESTERN U.S.A. EASTERN U.S.A. Based on Table 4 from Fiore et al., Journal of Geophysical Research, 2002 Deposition dominates, with O3 photolysis followed by OH production and O3 reaction with odd hydrogen radicals (OH, HO2) also important (relatively moreso in humid eastern U.S.A.) In high NOx settings (urban, power plant plumes) O3 titration by NO also occurs
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OZONE CONCENTRATIONS vs
OZONE CONCENTRATIONS vs. NOx AND VOC EMISSIONS Air pollution model calculation for a typical urban airshed NOx-limited Ridge NOx- saturated
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Influence of U.S. NOx controls on ozone air quality
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Cleaner U.S. air is visible from space
Satellite (OMI) tropospheric NO2 columns c/o Lok Lamsal & Bryan Duncan, NASA GSFC New OMI NO2 website: airquality.gsfc.nasa.gov
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Consistent trends derived from satellite (OMI) vs
Consistent trends derived from satellite (OMI) vs. ground-based (AQS) measurements c/o Bryan Duncan & Lok Lamsal, NASA GSFC
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Satellite (OMI NO2) data indicate 20-40% decreases from 2005 to 2014 over most of the U.S.A.
c/o Bryan Duncan & Lok Lamsal, NASA GSFC
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Trends in summer daytime (11am-4pm) 95% ozone at rural U. S
Trends in summer daytime (11am-4pm) 95% ozone at rural U.S. monitoring sites (CASTNet): 1990 to 2010 significant not significant Cooper et al., JGR, 2012 Decreases in EUS attributed in observations and models to NOx emission controls [e.g., Frost et al., 2006; Hudman et al., 2007; van der A. et al., 2008; Stavrakou et al., 2008; Bloomer et al., 2009, 2010; Fang et al., 2010]
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CASTNet site: Penn Station, PA
Extreme value theory methods enable derivation of “return levels” for JJA MDA8 O3 within a given time period (from GPD fit) Return level = Probability of observing a value x (level) within a time window T (period) CASTNet site: Penn Station, PA Sharp decline in return levels between early and later periods (NOx SIP call) Consistent with prior work [e.g., Frost et al., 2006; Bloomer et al., 2009, 2010] Translates air pollution changes into probabilistic language Apply methods to all EUS CASTNet sites to derive 1-year and 5-year return levels Rieder et al., ERL 2013
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Highest ozone events decrease over EUS following NOx emission controls
1-year Return Levels for Summertime MDA8 Ozone 1-yr return level decreases by 2-16 ppb 1-year levels remain above the NAAQS ozone level (70 ppb) across much of EUS Rieder et al., ERL 2013
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Can we exploit weekday-weekend patterns in NOx emissions (e. g
Can we exploit weekday-weekend patterns in NOx emissions (e.g., diesel) to assess impact of NOx reductions on ozone? WEEKDAY WEEKEND Satellite (OMI) Tropospheric NO2 columns Mid-2000s NO2 columns decline on weekends; following NOx controls, weekday tropospheric NO2 columns look like past weekends Early 2010s Luke Valin LDEO, in prep.
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Implies regional NOx-sensitive ozone production
Similar patterns occur in surface ozone 90th% summer afternoon surface ozone (U.S. EPA AQS) WEEKDAY WEEKEND Mid- 2000s Early 2010s Luke Valin LDEO, in prep. Additional diesel NOx controls would lower weekday surface ozone (and tropospheric NO2 columns) Implies regional NOx-sensitive ozone production
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What is an air quality model?
See accompanying animation c/o Lee Murray (LDEO/NASA GISS)
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CMAQ Overview Biogenic Emissions Anthropogenic Emissions (LADCO)
Aerosol Thermodynamics Dispersion, Advection Meteorology (WRF) Other Processes eularian grid-based model Takes in my inputs Processes them with these things 36km grid, 112 rows, 148 columns, 27 layers, 500k grid boxes (If I were to decrease resolution to 12km number of grid boxes increases by more than 70 times) Cloud- Aqueous Processes Gas-phase chemistry Boundary Conditions (MOZART) c/o Alex Karambelas, U Wisconsin-Madison
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Current research directions and ongoing challenges
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Natural vs. anthropogenic sources: Nitrogen oxides (NOx)
Relative importance varies by day, season, year! Approx ~43 Tg N year in 2010. NOx = NO + NO2 (Precursor to tropospheric O3)
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Summertime NOx Sources over Contiguous U.S.A.
Estimates from Table 1 of Hudman et al., J. Geophys Res. Atmos., 2004 for July 1 – August
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Uncertainties exist in the sectoral breakdown of U. S
Uncertainties exist in the sectoral breakdown of U.S. anthropogenic NOx NOy (NOx + oxidation products) too high, as is NOy/CO Power plant NOx is well known (CEMS) Implies mobile sources are overestimated (by >50%) in the most recent U.S. EPA inventory (NEI2011) Modeled (CMAQ) using U.S. EPA NEI2011 inventory observed Anderson et al., Atmos. Environ., 2014 Figure c/o Russ Dickerson (U MD)
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How important are ‘natural’ NOx sources?
Model estimates of soil and lightning NOx influence on monthly mean maximum daily 8-hour (MDA8) average surface ozone Soil NOx June June 2006 Hudman et al., Atmos. Chem. Phys., 2010 Lightning NOx July 2004 Lightning and soil NOx vary daily, seasonally, and inter-annually. Their impacts on ozone are not well quantified, but are typically smaller than those from U.S. anthropogenic NOx Fang et al., J. Geophys. Res., 2010 [ppbv]
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Wildfires are a ‘hot’ topic: How much ozone do they produce?
Example (July )of how satellite, in situ measurements and models can be combined to detect and attribute exceptional events Fiore et al., EM 2014 (NASA AQAST special issue; Figures c/o R. Dickerson (U MD) excerpted from Taubman et al., 2004; Colarco et al., 2004) Ongoing research strives to understand the impact of fire effluents on high ozone levels
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An air quality mgmt challenge: SOURCE ATTRIBUTION How much is transported? Background? International? GEOS-Chem model “zero-out” simulations: one day during 2012 EUS heat wave
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c/o Kelly Chance, Harvard SAO, AQAST7 Meeting, June 2014
New insights into mid-latitude pollution expected from instruments aboard geostationary platforms with hourly, continuous coverage (~ launch dates) c/o Kelly Chance, Harvard SAO, AQAST7 Meeting, June 2014
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Figure 6a of Fiore, Naik, Leibensperger, JAWMA, 2015
An Air Quality Management Challenge: CLIMATE CHANGE Will warmer temperatures worsen O3 pollution? Observations at U.S. EPA CASTNet site Penn State, PA 41N, 78W, 378m July mean MDA8 O3 and July mean daily maximum temperature G. Milly Figure 6a of Fiore, Naik, Leibensperger, JAWMA, 2015 Co-variance between ozone and temperature implies that climate warming will degrade air quality in polluted regions (well established, e.g. see Jacob & Winner Atmos. Environ. review, 2009) Downward ozone trend as EUS NOx emission controls are implemented
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Decreasing NOx emissions reduces sensitivity of O3 to temperature; helps to guard against any “climate penalty” [e.g., Bloomer et al., 2009; Rasmussen et al., 2012; Brown-Steiner et al., 2015] : 4.1 ppb/C : 2.4 ppb/C July mean MDA8 ozone (ppb) G. Milly July mean maximum daily temperature (°C) Figure 6b of Fiore, Naik, Leibensperger, JAWMA, 2015
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Our Team at Lamont-Doherty Earth Observatory of Columbia University
Luke Valin EPA) Arlene Fiore (PI) George Milly Lee Murray Dan Westervelt Gus Correa Olivia Clifton Jean Guo Xiaomeng Jin Nora Mascioli Not shown but contributed to NASA AQAST projects: Yuxing Ma (CU, Masters), Cynthia Zucker (Barnard ugrad), Melissa Seto (CU ugrad), Jacob Oberman (U WI ugrad)
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