Insights Into Summertime Surface Ozone Formation From Diurnal Variations in Formaldehyde and Nitrogen Dioxide Along a Transect Through New York City
Name
JGR Atmospheres - 2025 - Tao - Insights Into Summertime Surface Ozone Formation From Diurnal Variations in Formaldehyde and.pdf
Description
Published version
Size
4.42 MB
Format
Adobe PDF
Checksum (MD5)
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Author(s)
Tao, Madankui
Fiore, Arlene M
Karambelas, Alexandra
Miller, Paul J
Valin, Lukas C
Judd, Laura M
Tzortziou, Maria
Whitehill, Andrew
Teora, Amanda
Tian, Yuhong
Date Issued
May 12, 2025
Journal
Journal of Geophysical Research: Atmospheres
Publisher
Wiley
Citation
Tao, M., Fiore, A. M., Karambelas, A., Miller, P. J., Valin, L. C., Judd, L. M., et al. (2025). Insights into summertime surface ozone formation from diurnal variations in formaldehyde and nitrogen dioxide along a transect through New York City. Journal of Geophysical Research: Atmospheres, 130, e2024JD040922.
Version
Final published version
Abstract
Estimating tropospheric ozone (O3) production from observations is challenging but possible given the close coupling of O3 with formaldehyde (HCHO) and nitrogen dioxide (NO2), two remotely sensed air pollutants. The previous reliance on once-daily satellite overpasses highlights the need to study diurnal changes and surface-column relationships. Using surface observations, Pandora spectrometer retrievals, and a high-resolution (1.33 km) air quality model (WRF-CMAQ), we characterize diurnal patterns of HCHO and NO2 at seven locations along an upwind-downwind pathway through New York City during June–August 2018. Diurnal patterns of limited surface HCHO measurements suggest biogenic emission influence, while a bimodal surface NO2 pattern indicates the impact of local anthropogenic nitrogen oxides emissions. Details of these patterns vary by site: an afternoon NO2 spike at New Haven (CT) indicates traffic emissions, while a delayed daily HCHO peak at Westport (CT) relative to other sites likely reflects sea breeze dynamics. Peak column concentrations generally lag surface peaks by about four hours, occurring at 9–10 a.m. for morning NO2 (from Pandora and WRF-CMAQ) and around 4 p.m. for midday HCHO (from WRF-CMAQ). TROPOMI overpass time at 1:30 p.m. misses peak column HCHO and NO2 concentrations. A box model (F0AM) constrained with site-level observations and WRF-CMAQ fields indicates 1–9 ppb hr−1 higher noontime local O3 production rates on three sets of paired high- versus mid-to-low-O3 days. F0AM sensitivity analyses on these six days suggest a predominantly transitional O3 formation regime at urban and downwind sites, differing at some sites from the NOx-saturated regime diagnosed for summertime average conditions via the weekday-weekend effect.
MIT Department
Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Terms of Use
Creative Commons Attribution-Noncommercial
Persistent DSpace Link
DOI of Published Version
https://doi.org/10.1029/2024JD040922
