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Record W2031871453 · doi:10.1029/2001jd000697

Ozone production from Canadian wildfires during June and July of 1995

2002· article· en· W2031871453 on OpenAlexaboutno aff
S. A. McKeen, Gerhard Wotawa, D. D. Parrish, J. S. Holloway, M. P. Buhr, G. Hübler, F. C. Fehsenfeld, J. F. Meagher

Bibliographic record

VenueJournal of Geophysical Research Atmospheres · 2002
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicAtmospheric chemistry and aerosols
Canadian institutionsnot available
Fundersnot available
KeywordsEnvironmental scienceOzoneLatitudeAtmospheric sciencesStratosphereClimatologyMeteorologyGeographyGeology

Abstract

fetched live from OpenAlex

During the summer of 1995, especially between June and mid July, extensive wildfires occurred throughout Canada, primarily north of 55°N latitude. A previous report used aircraft and surface observations and tracer simulations to show these fires strongly influenced CO concentrations as far south as 35°N in the central and eastern United States [ Wotawa and Trainer , 2000 ]. This study extends those results by incorporating wildfire emissions estimates for CO, NO x , and nonmethane hydrocarbons into a three‐dimensional photochemical transport model specifically designed to simulate ozone photochemistry in the continental United States. The results of the model are compared to observations from four measurement platforms deployed during the time period of interest: National Oceanic and Atmospheric Administration WP‐3 aircraft observations collected during the 1995 Southern Oxidants Study (SOS‐95) field campaign; 12 eastern U.S. surface stations that measured ozone, CO, and NO y ; rural ozone measurements from the Aerometric Information Retrieval System network collected by the U.S. Environmental Protection Agency; and daily ozonesondes obtained near Nashville, Tennessee, during SOS‐95. Model performance, as determined by correlation and bias with observations from these four platforms, is significantly improved for both O 3 and CO when the Canadian fires are considered. Both observations and model results show enhanced O 3 from air transported from the Northwest Territory. The model results imply that during the period of strongest fire influence 10 to 30 ppbv enhancement of O 3 throughout a large region of the central and eastern United States was due to these fires. Modeled O 3 increases are sensitive to the NO x /CO emission ratio assumed for the fires, which is highly uncertain and variable. A molar NO x /CO ratio of 0.007 yields model comparisons that are most consistent for O 3 and ΔO 3 /ΔCO observations within aged fire plumes during SOS‐95, and is also consistent with previously observed NO x /CO ratios from boreal fires. For this NO x /CO emission ratio, and considering the entire eastern United States, most of the O 3 increase is associated with the NO x emitted directly by the fires and the photochemical O 3 formation that occurs before the plumes actually reach the United States. However, the in situ oxidation of CO from the Canadian fires with NO x emitted locally leads to significantly higher O 3 increases for high‐NO x ‐emitting regions that are limited by hydrocarbon availability. Thus O 3 in urban areas, or any other region modified by nearby NO x sources, is more sensitive to long‐range fires compared to less populated or polluted regions.

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 distilled prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesInsufficient payload (model declined to judge)
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.223
Threshold uncertainty score0.998

Codex and Gemma teacher scores by category

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 integrity0.0000.001
Insufficient payload (model declined to judge)0.0030.000

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 head0.026
GPT teacher head0.250
Teacher spread0.225 · 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 teacher head, not a consensus.

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".

Quick stats

Citations187
Published2002
Admission routes1
Has abstractyes

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