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Title: Reconciliation of asynchronous satellite-based $$\mathrm{NO_2}$$ and $$\mathrm{XCO_2}$$ enhancements with mesoscale modeling over two urban landscapes

Abstract

Fossil fuel carbon dioxide (CO2ff), the main driver of global warming and climate change, is often co-emitted with nitrogen oxides (NOx) and precursors to ground-level ozone from anthropogenic sources like power plants or vehicles. In urban and suburban areas, satellite-based NO2 can be used as a proxy to track the emissions of CO2ff. Because of NO2’s shorter lifetime, urban NO2 plumes are more distinguishable from backgrounds and more sensitive to variations in emissions. However, the combination of these two gases is limited by the asynchrony among NO2 and CO2 monitoring satellites. We used CO2ff simulated by the Weather Research and Forecasting model coupled with Chemistry (WRF-Chem) model to reconcile the tropospheric NO2 vertical column density (VCD) from the Tropospheric Monitoring Instrument (TROPOMI) and column-averaged dry-air mole fractions of carbon dioxide enhancements (ΔXCO2) from Orbiting Carbon Observatory 3 (OCO-3) Snapshot Area Maps (SAMs) over a multicity area, Washington D.C.-Baltimore (DC-Balt), and a basin city, Mexico City. NO2/CO2ff ratios over DC-Balt are smaller than Mexico City, indicative of stricter emission restrictions, a more combustion-efficient vehicle fleet, and higher combustion efficiency due to lower altitude in DC-Balt. For single-track cases, the spatial correlations between NO2 and ΔXCO2 over Mexico City are stronger thanmore » DC-Balt because the NO2 and CO2 are mostly trapped in the valley of Mexico City, while DC-Balt is severely affected by distant sources (i.e., US East Coast cities). Using multi-track averaging, spatial correlation coefficients increase with the number of days used for averaging. The correlations reached a maximum when averaging >12 continuous images for DC-Balt and > 10 continuous images for Mexico City. This finding indicates that multi-track averaging using modeled CO2ff as a proxy is helpful to filter the noise in single-track images, to cancel the interference from distant sources, and to magnify correlations between NO2 and CO2ff. Mexico City showed stronger spatial correlations but weaker temporal correlations than DC-Balt due to biomass burning hot spots and large transport errors caused by the trapping effects of the surrounding mountains. Tracking the 20-day moving average of CO2ff emissions using TROPOMI NO2 seems technically feasible, considering the relationship between correlation coefficients and the number of available satellite images.« less

Authors:
 [1];  [2];  [3];  [3];  [3];  [4];  [4];  [4];  [5]
  1. Pennsylvania State University, University Park, PA (United States); Johns Hopkins University, Baltimore, MD (United States)
  2. Pennsylvania State University, University Park, PA (United States); Pacific Northwest National Laboratory (PNNL), Richland, WA (United States)
  3. University Paris-Saclay, Gif-sur-Yvette (France)
  4. University Nacional Autonoma de Mexico (UNAM), Mexico City (Mexico)
  5. University Paris-Saclay, Gif-sur-Yvette (France); University of Reims-Champagne Ardenne, Reims (France)
Publication Date:
Research Org.:
Pacific Northwest National Lab. (PNNL), Richland, WA (United States)
Sponsoring Org.:
USDOE; National Aeronautics and Space Administration; National Council of Science and Technology (CONACYT); Mexico City's Regional Carbon Impacts (MERCI-CO2); Dirección General de Asuntos del Personal Académico, Universidad Nacional Autónoma de México (DGAPA-UNAM)
OSTI Identifier:
1893830
Report Number(s):
PNNL-SA-176357
Journal ID: ISSN 0034-4257
Grant/Contract Number:  
AC05-76RL01830; 80NSSC18K1313; 80NSSC19k0093; 80HQTR21T0070; 290589; ANR-17-CE04-0013-01
Resource Type:
Accepted Manuscript
Journal Name:
Remote Sensing of Environment
Additional Journal Information:
Journal Volume: 281; Journal ID: ISSN 0034-4257
Publisher:
Elsevier
Country of Publication:
United States
Language:
English
Subject:
54 ENVIRONMENTAL SCIENCES; OCO-3 SAMs; TROPOMI; WRF-Chem; Washington D.C.-Baltimore; Mexico City

Citation Formats

Lei, Ruixue, Feng, Sha, Xu, Yang, Tran, Sophie, Ramonet, Michel, Grutter, Michel, Garcia, Agustin, Campos-Pineda, Mixtli, and Lauvaux, Thomas. Reconciliation of asynchronous satellite-based $\mathrm{NO_2}$ and $\mathrm{XCO_2}$ enhancements with mesoscale modeling over two urban landscapes. United States: N. p., 2022. Web. doi:10.1016/j.rse.2022.113241.
Lei, Ruixue, Feng, Sha, Xu, Yang, Tran, Sophie, Ramonet, Michel, Grutter, Michel, Garcia, Agustin, Campos-Pineda, Mixtli, & Lauvaux, Thomas. Reconciliation of asynchronous satellite-based $\mathrm{NO_2}$ and $\mathrm{XCO_2}$ enhancements with mesoscale modeling over two urban landscapes. United States. https://doi.org/10.1016/j.rse.2022.113241
Lei, Ruixue, Feng, Sha, Xu, Yang, Tran, Sophie, Ramonet, Michel, Grutter, Michel, Garcia, Agustin, Campos-Pineda, Mixtli, and Lauvaux, Thomas. Tue . "Reconciliation of asynchronous satellite-based $\mathrm{NO_2}$ and $\mathrm{XCO_2}$ enhancements with mesoscale modeling over two urban landscapes". United States. https://doi.org/10.1016/j.rse.2022.113241. https://www.osti.gov/servlets/purl/1893830.
@article{osti_1893830,
title = {Reconciliation of asynchronous satellite-based $\mathrm{NO_2}$ and $\mathrm{XCO_2}$ enhancements with mesoscale modeling over two urban landscapes},
author = {Lei, Ruixue and Feng, Sha and Xu, Yang and Tran, Sophie and Ramonet, Michel and Grutter, Michel and Garcia, Agustin and Campos-Pineda, Mixtli and Lauvaux, Thomas},
abstractNote = {Fossil fuel carbon dioxide (CO2ff), the main driver of global warming and climate change, is often co-emitted with nitrogen oxides (NOx) and precursors to ground-level ozone from anthropogenic sources like power plants or vehicles. In urban and suburban areas, satellite-based NO2 can be used as a proxy to track the emissions of CO2ff. Because of NO2’s shorter lifetime, urban NO2 plumes are more distinguishable from backgrounds and more sensitive to variations in emissions. However, the combination of these two gases is limited by the asynchrony among NO2 and CO2 monitoring satellites. We used CO2ff simulated by the Weather Research and Forecasting model coupled with Chemistry (WRF-Chem) model to reconcile the tropospheric NO2 vertical column density (VCD) from the Tropospheric Monitoring Instrument (TROPOMI) and column-averaged dry-air mole fractions of carbon dioxide enhancements (ΔXCO2) from Orbiting Carbon Observatory 3 (OCO-3) Snapshot Area Maps (SAMs) over a multicity area, Washington D.C.-Baltimore (DC-Balt), and a basin city, Mexico City. NO2/CO2ff ratios over DC-Balt are smaller than Mexico City, indicative of stricter emission restrictions, a more combustion-efficient vehicle fleet, and higher combustion efficiency due to lower altitude in DC-Balt. For single-track cases, the spatial correlations between NO2 and ΔXCO2 over Mexico City are stronger than DC-Balt because the NO2 and CO2 are mostly trapped in the valley of Mexico City, while DC-Balt is severely affected by distant sources (i.e., US East Coast cities). Using multi-track averaging, spatial correlation coefficients increase with the number of days used for averaging. The correlations reached a maximum when averaging >12 continuous images for DC-Balt and > 10 continuous images for Mexico City. This finding indicates that multi-track averaging using modeled CO2ff as a proxy is helpful to filter the noise in single-track images, to cancel the interference from distant sources, and to magnify correlations between NO2 and CO2ff. Mexico City showed stronger spatial correlations but weaker temporal correlations than DC-Balt due to biomass burning hot spots and large transport errors caused by the trapping effects of the surrounding mountains. Tracking the 20-day moving average of CO2ff emissions using TROPOMI NO2 seems technically feasible, considering the relationship between correlation coefficients and the number of available satellite images.},
doi = {10.1016/j.rse.2022.113241},
journal = {Remote Sensing of Environment},
number = ,
volume = 281,
place = {United States},
year = {Tue Sep 13 00:00:00 EDT 2022},
month = {Tue Sep 13 00:00:00 EDT 2022}
}

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