Articles | Volume 26, issue 7
https://doi.org/10.5194/acp-26-4917-2026
© Author(s) 2026. This work is distributed under the Creative Commons Attribution 4.0 License.
Novel insights on causes of disproportionate trends between particulate NO3− and NOx emissions in Canadian urban atmospheres
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- Final revised paper (published on 14 Apr 2026)
- Supplement to the final revised paper
- Preprint (discussion started on 15 Dec 2025)
- Supplement to the preprint
Interactive discussion
Status: closed
Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor
| : Report abuse
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CC1: 'Comment on egusphere-2025-6080', Nima Zafarmomen, 02 Jan 2026
- AC1: 'Reply on CC1', Leiming Zhang, 26 Feb 2026
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RC1: 'Comment on egusphere-2025-6080', Anonymous Referee #1, 05 Jan 2026
- AC2: 'Reply to RC1', Leiming Zhang, 26 Feb 2026
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RC2: 'Comment on egusphere-2025-6080', Anonymous Referee #2, 14 Jan 2026
- AC3: 'Reply to RC2', Leiming Zhang, 26 Feb 2026
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
AR by Leiming Zhang on behalf of the Authors (26 Feb 2026)
Author's response
EF by Katja Gänger (02 Mar 2026)
Manuscript
Author's tracked changes
ED: Publish as is (23 Mar 2026) by Qi Chen
AR by Leiming Zhang on behalf of the Authors (26 Mar 2026)
Manuscript
This study presents a comprehensive long-term (1990–2019) analysis of fine- and coarse-mode particulate nitrate (f-NO₃⁻ and c-NO₃⁻) in seven Canadian urban atmospheres using NAPS observations. The authors identify systematic, disproportionate trends between particulate nitrate concentrations and NOₓ emission reductions, particularly in cold-climate cities. Despite modest declines in provincial NOₓ emissions (typically 10–30%), f-NO₃⁻ concentrations decreased by up to ~60–70% in recent decades, while c-NO₃⁻ remained largely insensitive to NOₓ controls.
Primary f-NO₃⁻ emissions hypothesis: The explanation is physically plausible and well-argued, but remains indirect. The manuscript would benefit from clearer discussion of how future studies (e.g., near-source plume measurements or isotopic constraints) could directly validate this mechanism.
HNO₃* measurements: The clarification that denuder-based HNO₃ represents an upper bound (HNO₃ + N₂O₅) is important and appropriately handled. Consider briefly discussing how this uncertainty might bias wintertime interpretations (even qualitatively).
Given the study’s emphasis on spatial inhomogeneity and the impact of localized urban sources (as discussed in Category ii uncertainties, Section 3.6), it is essential to contextualize these findings within the broader framework of high-resolution urban monitoring.
I strongly suggest citing the following paper to bolster the discussion on how localized traffic and industrial emissions create complex urban aerosol patterns that traditional stationary sites might struggle to represent: Comprehensive spatiotemporal analysis of long-term mobile monitoring for traffic-related particles in a complex urban environment. > DOI: 10.1016/j.apr.2025.102870