ArticleAtmospheric chemistry and physics2020
Constraining remote oxidation capacity with ATom observations.
Article in Atmospheric chemistry and physics, 2020. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 7 papers.
What it found
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The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.
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Who cites it
7 citing papers in PubMed, 91 citations in OpenAlex.
- Preliminary Evidence of Exogenous Hydrogen Peroxide Formation via Plant Transpiration: Toward a Nature-Based Solution for Air Quality and Climate Mitigation.Bioengineering (Basel, Switzerland) · 2025Article
- Atmospheric isoprene measurements reveal larger-than-expected Southern Ocean emissions.Nature communications · 2024Article
- An observation-based, reduced-form model for oxidation in the remote marine troposphere.Proceedings of the National Academy of Sciences of the United States of America · 2023Article
- Seven-year monitoring of mercury in wet precipitation and atmosphere at the Amsterdam Island GMOS station.Heliyon · 2023Article
- Extensive field evidence for the release of HONO from the photolysis of nitrate aerosols.Science advances · 2023Article
- HCOOH in the remote atmosphere: Constraints from Atmospheric Tomography (ATom) airborne observations.ACS earth & space chemistry · 2021Article
- Chemical Interactions Between Ship-Originated Air Pollutants and Ocean-Emitted Halogens.Journal of geophysical research. Atmospheres : JGR · 2021Article
Corrections and comments
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Authors and funding
32 authors at 16 institutions in 3 countries.
Funding
Abstract
The global oxidation capacity, defined as the tropospheric mean concentration of the hydroxyl radical (OH), controls the lifetime of reactive trace gases in the atmosphere such as methane and carbon monoxide (CO). Models tend to underestimate the methane lifetime and CO concentrations throughout the troposphere, which is consistent with excessive OH. Approximately half of the oxidation of methane and non-methane volatile organic compounds (VOCs) is thought to occur over the oceans where oxidant chemistry has received little validation due to a lack of observational constraints. We use observations from the first two deployments of the NASA ATom aircraft campaign during July-August 2016 and January-February 2017 to evaluate the oxidation capacity over the remote oceans and its representation by the GEOS-Chem chemical transport model. The model successfully simulates the magnitude and vertical profile of remote OH within the measurement uncertainties. Comparisons against the drivers of OH production (water vapor, ozone, and NO
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Registered trials
Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.