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Variations in Vertical O3 and SO2 Concentrations During Rainfall in a Boreal-temperate Forest

2025· preprint· W4417508182 on OpenAlexafffund
Jane Liu, Holly Croft, Ralf M. Staebler, Liming He, Alemu Gonsamo, Jing M. Chen

Bibliographic record

Venuenot available
Typepreprint
Language
FieldAgricultural and Biological Sciences
TopicPlant responses to elevated CO2
Canadian institutionsMcMaster UniversityEnvironment and Climate Change CanadaUniversity of Toronto
FundersEuropean Centre for Medium-Range Weather ForecastsEnvironment and Climate Change CanadaUniversity of Toronto
KeywordsTrace gasDeposition (geology)Mixing ratioDaytimeOzoneSulfur dioxideRelative humidityAtmosphere (unit)Spatial distributionAir pollution

Abstract

fetched live from OpenAlex

Ozone (O 3 ) and sulfur dioxide (SO 2 ) in the atmospheric boundary layer are air pollutants that pose significant threats to forest health. Rainfall can significantly modulate the concentrations of these trace gases. In forest ecosystems, it is essential to assess the extent to which rainfall impacts gas concentrations and to understand the underlying mechanisms driving such changes. Here, we explore how rainfall alters the vertical distribution of O 3 and SO 2 mixing ratios within and above a boreal-temperate forest canopy, drawing upon multi-year measurements (2009–2013) from a 42-meter tower. Based on 194 persistent rainfall events, comparisons of vertical O 3 and SO 2 mixing ratios between rain and non-rain conditions are made at matched height, hour, and month to minimize biases introduced by spatial and temporal background variations. In contrast to tropical forest observations where O 3 increases during rain, our results indicate a consistent decline in O 3 by 2–6 ppb (10–20%) during rainfall across all heights, from near the surface to above the canopy, except for during evening rainfall. Reductions in SO 2 are even more substantial, reaching 0.3–0.5 ppb (40–50%) throughout the profile. We further assess the role of four key processes of washout, photochemistry, deposition, and vertical transport in modulating O 3 and SO 2 vertical profiles during rainfall. The substantial reduction in SO 2 is mainly attributable to its high solubility, while O 3 reductions during the day are largely due to declined photochemical production. Rain-induced surface wetness modestly enhances non-stomatal deposition of both gases, observably at night, whereas the overall daytime O 3 deposition remains relatively stable, as the enhanced non-stomatal deposition is offset by the decreased stomatal deposition. Additionally, upward transport following the rainfall onset could contribute to the reduction of O 3 in the boundary layer, while downward transport after the rainfall peak could contribute to O 3 enhancement. This effect is most obvious at night, when photochemistry is absent. These findings provide new insights into how rainfall impacts air pollutants and underscore the role of the four processes in shaping O 3 and SO 2 vertical distributions in boreal-temperate forests, thereby advancing our understanding of atmosphere-biosphere interactions.

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

How this classification was reachedexpand

Full frame machine prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. The Gemma side is a direct model label for every work in the frame, read from the title-only record. The Codex side is a classifier learned from the 10,348 direct Codex labels and calibrated to design-weighted sample rates; fields without enough sample support carry no Codex call. Candidate is the union of the two sides; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.031
Threshold uncertainty score0.061

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0000.000

Machine scores (provisional)

The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

Opus teacher head0.016
GPT teacher head0.237
Teacher spread0.221 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it

Classification

machine, unvalidated

Machine predicted; a candidate call from one source (direct Gemma or distilled Codex), not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
Study designObservational
Domainnot available
GenreEmpirical

How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".

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Citations0
Published2025
Admission routes2
Has abstractyes

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