Abstract

Abstract. We analyze the simulation results from a CMAQ model and GOME-2 NO2 retrievals over the United States for August 2009 to estimate the model-simulated biases of NOx concentrations over six geological regions (Pacific Coast = PC, Rocky Mountains = RM, Lower Middle = LM, Upper Middle = UM, Southeast = SE, Northeast = NE). By comparing GOME-2 NO2 columns to corresponding CMAQ NO2 columns, we produced satellite-adjusted NOx emission ("GOME2009") and compared baseline emission ("BASE2009") CMAQ simulations with GOME2009 CMAQ runs. We found that the latter exhibited decreases of −5.6%, −12.3%, −21.3%, and −15.9 % over the PC, RM, LM, and SE regions, respectively, and increases of +2.3% and +10.0% over the UM and NE regions. In addition, we found that changes in NOx emissions generally mitigate discrepancies between the surface NOx concentrations of baseline CMAQ and those of AQS at EPA AQS stations (mean bias of +19.8% to −13.7% over PC, −13.8% to −36.7% over RM, +149.7% to −1.8% over LM, +22.5% to −7.8% over UM, +31.3% to −7.9% over SE, and +11.6% to +0.7% over NE). The relatively high simulated NOx biases from baseline CMAQ over LM (+149.7%) are likely the results of over-predictions of simulated NOx emissions, which could shed light on those from global/regional Chemical Transport Models. We also perform more detailed investigations on surface NOx and O3 concentrations in two urban and outflow areas, PC (e.g., Los Angeles, South Pasadena, Anaheim, La Habra and Riverside) and LM (e.g., Houston, Beaumont and Sulphur). From two case studies, we found that the GOME2009 emissions decreased surface NOx concentrations significantly in the urban areas of PC (up to 30 ppbv) and in those of LM (up to 10 ppbv) during the daytime and that simulated NOx concentrations from CMAQ with GOME2009 compare well to those of in-situ AQS observations. A significant reduction in NOx concentrations resulted in a comparable increase in surface O3 concentrations in the urban areas of PC (up to 30 ppbv) and the resulting simulated O3 concentrations compare well with in-situ surface O3 observations over South Pasadena, Anaheim, and Riverside. Over Houston, Beaumont, and Sulphur, large reductions in NOx emissions from CMAQ with GOME2009 coincides with large reduced concentrations of simulated NOx. These concentrations are similar to those of the EPA AQS NOx observations. However, the resulting simulated increase in surface O3 at the urban stations in Houston and Sulphur exacerbated preexisting high O3 over-predictions of the baseline CMAQ. This study implies that simulated low O3 biases in the urban areas of PC are likely caused by simulated high NOx biases, but high O3 biases in the urban areas of LM cannot be explained by simulated high NOx biases over the region. This study also suggests that both in-situ surface NOx and O3 observations should be used simultaneously to resolve issues pertaining to simulated high/low O3 bias and that remote-sensing data could be used as a constraint for bottom-up emissions. In addition, we also found that daytime O3 reductions over the outflow regions of LM following large reductions in NOx emissions in the urban areas are significantly larger than they are over outflow regions of PC. These findings provide policymakers in the two regions with information critical to establishing strategies for mitigating air pollution.

Highlights

  • Nitrogen oxides (NOx = NO + NO2) are major O3 precursors that originate from fossil fuel combustion, lightning, soil, aircraft, and biomass burning

  • We used the remotely-sensed NO2 column density from the Global Ozone Monitoring Experiment-2 (GOME-2) sensor to measure the nadir at 09:30 local time (LT) with footprints of 40 × 80 km2, obtained the daily Global Ozone Monitoring Experiments (GOME)-2 NO2 column retrievals from http://www.temis.nl/airpollution, and used TM4NO2A version 2.1 for the GOME-2 NO2 column density

  • We found large reductions in NOx concentrations in CMAQ with GOME2009, at EPA AQS stations over LM, SE and PC (i.e., +149.7 to −1.8 % for LM and +19.8 to −13.7 % for PC), which resulted from large reductions in NOx emissions over the regions

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Summary

Introduction

Several previous studies pertaining to the NOx emissions inventory have focused on investigating changes in the number of NO2 columns resulting from either air pollution policy regulations over the eastern, western, and southern US (e.g., Kim et al, 2006, 2009; 2011; Choi et al, 2009, 2012; Russell et al, 2010) or over China (e.g., Zhao and Wang, 2009; Yang et al, 2011), or the occurrence of extreme weather conditions over coastal urban regions near the Gulf of Mexico (e.g., Yoshida et al, 2010) These studies have shown significant differences between the NO2 column densities of satellite instruments (e.g., OMI and SCIAMACHY) and WRF-Chem across the western United States (e.g., Kim et al, 2009). Details relating to the chemistry modules and the chemical boundary conditions for this study were described in the previous study by Choi et al (2012)

The global ozone monitoring experiment-2 NO2 column
In-situ observed ground-level NOx and O3
Comparison of the NO2 columns of CMAQ to those of GOME-2
The impact of GOME2009 on surface NOx over six geological regions
Conclusion and discussion
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