the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
| 26 Feb 2025
Observations of tropospheric HONO are incompatible with understanding of atmospheric chemistry
Abstract. Recent observations of nitrous acid (HONO) in the remote troposphere found much higher concentrations than can be explained through known sources, with important implications for air quality and climate. Laboratory evidence and modelling of field observations suggests that nitrate aerosol photolysis is the likely mechanism providing the additional HONO, offering a rapid route for recycling of NOx from nitric acid (HNO3). Previous studies of the global impact of this chemistry have used either very restricted HONO data or a “top-down” approach to parameterize the HONO source by reconciling simulated and observed NOx concentrations. Here, we use multiple, independent tropospheric HONO observations from different locations to parameterize nitrate photolysis, and evaluate its impacts on global atmospheric chemistry using GEOS-Chem. The simulations improve agreement between modelled and observed HONO concentrations relative to previous studies, decreasing the model bias by 5–20 %. The remaining (and large) underestimate of HONO in the model is due predominantly to an underestimate of total nitrate aerosol (-95 %) and is reduced to 20 % when accounting for low model nitrate. Despite the low bias in the model HONO, we find that nitrate aerosol photolysis leads to substantial global increases in NOx, O3 and OH concentrations, likely beyond the observational constraints. The additional source of NOx (~48 Tg N yr-1 globally) is comparable to total NOx emissions from all sources (~55 Tg yr-1). These HONO observations in the remote troposphere, thus imply a large uncertainty in the NOx budget and an incomplete understanding of atmospheric chemistry.
Competing interests: At least one of the (co-)authors is a member of the editorial board of Atmospheric Chemistry and Physics.
Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this preprint. The responsibility to include appropriate place names lies with the authors.- Preprint
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Status: open (until 09 Apr 2025)
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RC1: 'Comment on egusphere-2025-830', Anonymous Referee #1, 20 Mar 2025
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Rowlinson et al. present a new parameterization of particulate nitrate photolysis to explain high HONO concentrations observed in recent field campaigns conducted in less polluted regions. They include this parameterization in the GEOS-Chem model and compare simulations against HONO observations from additional campaigns, finding improved agreement compared to simulations without this source. However, including this new HONO source leads to large changes in the global NOx source and the O3 and OH burdens in the model, which are inconsistent with observational constraints. The authors, therefore, conclude that these HONO measurements highlight a gap in our current understanding of atmospheric chemistry.
The study addresses an important issue: photolysis of HONO is a source of NOx and HOx, both key species in tropospheric chemistry. Observations in remote areas have reported unexpectedly high HONO concentrations, suggesting an unidentified source that could significantly influence NOx and HOx cycling. Some prior studies have suggested particulate nitrate photolysis as this source and have derived photolysis rates based on the inferred HONO source. This study expands on that approach using a broader observational dataset and evaluates its global implications.
Although the results are potentially impactful, there are some major issues to be addressed:
i) The study adopts a narrow framing of uncertainties surrounding HONO sources, assuming particulate nitrate photolysis as the sole explanation for observed HONO (cf. Eq. 1), without adequate justification. Notably, the role of heterogeneous NO2 reactions on aerosols is not discussed, although this process is included in GEOS-Chem. What is the uncertainty associated with it? What other mechanisms have been proposed in the literature, and why are they insufficient to explain the observed HONO? Addressing these questions is necessary to substantiate the study’s conclusion that the HONO observations point to a fundamental gap in our understanding.
ii) The key result supporting this conclusion is the large effect of the proposed HONO source on the modeled burdens of O3 and OH, which is pushed beyond observational bounds. This occurs even though the model underestimates particulate nitrate concentrations and potentially also the HONO source. The issue again is that the study assumes that the missing HONO source is only from particulate nitrate photolysis. If the missing reaction producing HONO consumes NOx (and HOx), then the impact on O3 and OH would be smaller. Li et al. (2014; doi: 10.1126/science.1248999) hypothesized such a mechanism, and recent laboratory work by Song et al. (2023; doi: 10.1038/s41612-023-00357-8) provides empirical evidence for another such reaction. This alternative explanation seems more plausible and should be considered.
iii) The physical interpretation of the parameterization for HONO production from particulate nitrate photolysis is unclear.
From Eqs. 1–4, the HONO production rate is given by:
P(HONO) = (2/3) × J(HNO3) × EF × [pNO3]
where EF = C1 / (1 + C2 × [pNO3]). At atmospherically relevant [pNO3], C2 × [pNO3] >> 1, which reduces the EF to:
EF ≈ (C1 / C2) / [pNO3]
and thus,
P(HONO) ≈ (2/3) × J(HNO3) × (C1 / C2)
This implies that the HONO production rate is effectively independent of [pNO3], which is difficult to interpret physically if particulate nitrate photolysis is the missing HONO source.Citation: https://doi.org/10.5194/egusphere-2025-830-RC1
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