Preprints
https://doi.org/10.5194/egusphere-2023-1117
https://doi.org/10.5194/egusphere-2023-1117
16 Jun 2023
 | 16 Jun 2023

Understanding offshore high-ozone events during TRACER-AQ 2021 in Houston: Insights from WRF-CAMx photochemical modeling

Wei Li, Yuxuan Wang, Xueying Liu, Ehsan Soleimanian, Travis Griggs, James Flynn, and Paul Walter

Abstract. Mechanisms for high offshore ozone (O3) events in the Houston area have not been systematically examined due to limited O3 measurements over water. In this study, we used the datasets collected by three boats deployed in Galveston Bay and the Gulf of Mexico during the Tracking Aerosol Convection Interactions ExpeRiment/Air Quality (TRACER-AQ) field campaign period (September 2021) in combination with the Weather Research and Forecasting (WRF) coupled Comprehensive Air quality Model with Extensions (CAMx) modeling system (WRF-CAMx) to investigate the reasons for high offshore O3. The model can capture the spatiotemporal variability of daytime (10:00–18:00) O3 for the three boats (R > 0.7) but tends to overestimate O3 by ~10 ppb on clean days and underestimate O3 by ~3 ppb during high-O3 events. The process analysis tool in CAMx identifies O3 chemistry as the major process leading to high O3 concentrations. The region-wide increase of long-lived VOCs through advection not only leads to more O3 production under a NOx-limited regime but also fosters VOC-limited O3 formation along western Galveston Bay and the Gulf coast under high-NOx conditions brought by the northeasterly winds from the Houston Ship Channel. Two case studies illustrate that high offshore O3 events can develop under both large- and meso-scale circulations, indicating both the regional and local emissions need to be stringently controlled. Wind conditions are demonstrated to be important meteorological factors in such events, so they must be well represented in photochemical models to forecast air quality over the urban coastal regions accurately.

Journal article(s) based on this preprint

03 Nov 2023
Understanding offshore high-ozone events during TRACER-AQ 2021 in Houston: insights from WRF–CAMx photochemical modeling
Wei Li, Yuxuan Wang, Xueying Liu, Ehsan Soleimanian, Travis Griggs, James Flynn, and Paul Walter
Atmos. Chem. Phys., 23, 13685–13699, https://doi.org/10.5194/acp-23-13685-2023,https://doi.org/10.5194/acp-23-13685-2023, 2023
Short summary

Wei Li et al.

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2023-1117', Anonymous Referee #1, 15 Aug 2023
  • RC2: 'Comment on egusphere-2023-1117', Anonymous Referee #2, 16 Aug 2023
  • AC1: 'Comment on egusphere-2023-1117', Wei Li, 22 Sep 2023

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2023-1117', Anonymous Referee #1, 15 Aug 2023
  • RC2: 'Comment on egusphere-2023-1117', Anonymous Referee #2, 16 Aug 2023
  • AC1: 'Comment on egusphere-2023-1117', Wei Li, 22 Sep 2023

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Wei Li on behalf of the Authors (22 Sep 2023)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (27 Sep 2023) by Suvarna Fadnavis
AR by Wei Li on behalf of the Authors (27 Sep 2023)  Author's response   Manuscript 

Journal article(s) based on this preprint

03 Nov 2023
Understanding offshore high-ozone events during TRACER-AQ 2021 in Houston: insights from WRF–CAMx photochemical modeling
Wei Li, Yuxuan Wang, Xueying Liu, Ehsan Soleimanian, Travis Griggs, James Flynn, and Paul Walter
Atmos. Chem. Phys., 23, 13685–13699, https://doi.org/10.5194/acp-23-13685-2023,https://doi.org/10.5194/acp-23-13685-2023, 2023
Short summary

Wei Li et al.

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Short summary
This study examined high offshore ozone events in Galveston Bay and the Gulf of Mexico using boat data and WRF-CAMx modeling during the TRACER-AQ 2021 field campaign. On average, high ozone is caused by chemistry due to the regional transport of VOCs and downwind advection of NOx from the Ship Channel. Two case studies show advection of ozone can be another process leading to high ozone and an accurate wind prediction is crucial for air quality forecasting in coastal areas.