A simplified non-linear chemistry transport model for analyzing NO₂ column observations: STILT–NOx
Creators
Abstract
Satellites monitoring air pollutants (e.g., nitrogen oxides; NOx = NO + NO2) or greenhouse gases (GHGs) are widely utilized to understand the spatiotemporal variability in and evolution of emission characteristics, chemical transformations, and atmospheric transport over anthropogenic hotspots. Recently, the joint use of space-based long-lived GHGs (e.g., carbon dioxide; CO2) and short-lived pollutants has made it possible to improve our understanding of emission characteristics. Some previous studies, however, lack consideration of the non-linear NOx chemistry or complex atmospheric transport. Considering the increase in satellite data volume and the demand for emission monitoring at higher spatiotemporal scales, it is crucial to construct a local-scale emission optimization system that can handle both long-lived GHGs and short-lived pollutants in a coupled and effective manner. This need motivates us to develop a Lagrangian chemical transport model that accounts for NOx chemistry and fine-scale atmospheric transport (STILT–NOx) and to investigate how physical and chemical processes, anthropogenic emissions, and background may affect the interpretation of tropospheric NO2 columns (tNO2).
Interpreting emission signals from tNO2 commonly involves either an efficient statistical model or a sophisticated chemical transport model. To balance computational expenses and chemical complexity, we describe a simplified representation of the NOx chemistry that bypasses an explicit solution of individual chemical reactions while preserving the essential non-linearity that links NOx emissions to its concentrations. This NOx chemical parameterization is then incorporated into an existing Lagrangian modeling framework that is widely applied in the GHG community. We further quantify uncertainties associated with the wind field and chemical parameterization and evaluate modeled columns against retrieved columns from the TROPOspheric Monitoring Instrument (TROPOMI v2.1). Specifically, simulations with alternative model configurations of emissions, meteorology, chemistry, and inter-parcel mixing are carried out over three United States (US) power plants and two urban areas across seasons. Using the U.S. Environmental Protection Agency (EPA)-reported emissions for power plants with non-linear NOx chemistry improves the model–data alignment in tNO2 (a high bias of ≤ 10 % on an annual basis), compared to simulations using either the Emissions Database for Global Atmospheric Research (EDGAR) model or without chemistry (bias approaching 100 %). The largest model–data mismatches are associated with substantial biases in wind directions or conditions of slower atmospheric mixing and photochemistry. More importantly, our model development illustrates (1) how NOx chemistry affects the relationship between NOx and CO2 in terms of the spatial and seasonal variability and (2) how assimilating tNO2 can quantify systematic biases in modeled wind directions and emission distribution in prior inventories of NOx and CO2, which laid a foundation for a local-scale multi-tracer emission optimization system.
Copyright and License
© Author(s) 2023. This work is distributed under the Creative Commons Attribution 4.0 License. Published by Copernicus Publications on behalf of the European Geosciences Union.
Acknowledgement
The computations presented here were conducted in the Resnick High-Performance Computing Center, a facility supported by the Resnick Sustainability Institute at the California Institute of Technology. We acknowledge the use of the WRF-Chem preprocessor tool of mozbc, which was provided by the Atmospheric Chemistry Observations and Modeling Lab (ACOM) of the National Center for Atmospheric Research (NCAR). The authors acknowledge the National Oceanic and Atmospheric Administration (NOAA) Air Re45 sources Laboratory (ARL) for the provision of the GFS and HRRR meteorological files used in this publication, which were downloaded from the READY website (http://www.ready.noaa.gov, last access: 1 May 2018). The first author extends their appreciation to Kazuyuki Miyazaki (JPL) for discussions on NOx modeling and Rob Nelson and Annmarie Eldering (JPL) for the OCO-3 data. The authors thank the two anonymous referees for their careful reading of our paper and for their constructive suggestions that have helped improve our study.
Funding
The analysis has been supported by the National Aeronautics and Space Administration (NASA; grant no. 80NSSC21K1064). A portion of the research was carried out at the Jet Propulsion Laboratory, California Institute of Technology, under a contract with NASA (grant no. 80NM0018D0004).
Data Availability
TROPOMI is available at TROPOMI Level 2 Nitrogen Dioxidehttps://doi.org/10.5270/S5P-9bnp8q8 (ESA, 2021). OCO-3 Level 2 B10p4r XCO2 data are available at https://doi.org/10.5067/970BCC4DHH24 (OCO-2/OCO-3 Science Team et al., 2022). EDGARv6.1 emissions can be accessed from https://data.jrc.ec.europa.eu/dataset/df521e05-6a3b-461c-965a-b703fb62313e (Monforti Ferrario et al., 2022) and have been preprocessed. The STILT–NOx v1 model is built on previous efforts of the X-STILT model in modeling NO2. The exact version used in the paper is archived on Zenodo at https://doi.org/10.5281/zenodo.8057850 (Wu, 2023). The GFS and HRRR meteorological files are available from the READY website (https://www.ready.noaa.gov/archives.php, Rolph et al., 2017).
Supplemental Material
The supplement related to this article is available online at: https://doi.org/10.5194/gmd-16-6161-2023-supplement.
Additional Information
This paper was edited by Jason Williams and reviewed by two anonymous referees.
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Additional details
Funding
- National Aeronautics and Space Administration
- 80NSSC21K1064
- National Aeronautics and Space Administration
- 80NM0018D0004
Dates
- Accepted
-
2023-09-04