Articles | Volume 19, issue 13
https://doi.org/10.5194/acp-19-8547-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-19-8547-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
05 Jul 2019
Research article |
| 05 Jul 2019
| 05 Jul 2019
An improved estimate for the δ13C and δ18O signatures of carbon monoxide produced from atmospheric oxidation of volatile organic compounds
Isaac J. Vimont
CORRESPONDING AUTHOR
Institute of Arctic and Alpine Research, University of Colorado, Boulder, CO, USA
National Oceanic and Atmospheric Administration, Global Monitoring
Division, Boulder, CO, USA
CIRES, University of Colorado, Boulder, CO, USA
Jocelyn C. Turnbull
CIRES, University of Colorado, Boulder, CO, USA
GNS Science, Lower Hutt, New Zealand
Vasilii V. Petrenko
Earth and Environmental Science Department, University of Rochester,
Rochester, NY, USA
Philip F. Place
Earth and Environmental Science Department, University of Rochester,
Rochester, NY, USA
Colm Sweeney
National Oceanic and Atmospheric Administration, Global Monitoring
Division, Boulder, CO, USA
Natasha Miles
Department of Meteorology and Atmospheric Science, Pennsylvania State University, College Station, PA, USA
Scott Richardson
Department of Meteorology and Atmospheric Science, Pennsylvania State University, College Station, PA, USA
Bruce H. Vaughn
Institute of Arctic and Alpine Research, University of Colorado, Boulder, CO, USA
James W. C. White
Institute of Arctic and Alpine Research, University of Colorado, Boulder, CO, USA
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Cited
12 citations as recorded by crossref.
- Efficacy of the CO Tracer Technique in Partitioning Biogenic and Anthropogenic Atmospheric CO2 Signals in the Humid Subtropical Eastern Highland Rim City of Cookeville, Tennessee W. Gichuhi & L. Gamage 10.3390/atmos14020208
- The use of δ 13C in CO to determine removal of CH4 by Cl radicals in the atmosphere * T. Röckmann et al. 10.1088/1748-9326/ad4375
- Isotopic source signatures of stratospheric CO inferred from in situ vertical profiles J. Hooghiem et al. 10.1038/s41612-025-00986-1
- High‐Resolution Lagrangian Inverse Modeling of CO2 Emissions Over the Paris Region During the First 2020 Lockdown Period K. Nalini et al. 10.1029/2021JD036032
- Observing Anthropogenic and Biogenic CO2 Emissions in Los Angeles Using a Dense Sensor Network J. Kim et al. 10.1021/acs.est.4c11392
- Quantification of fossil fuel CO2 from combined CO, δ13CO2 and Δ14CO2 observations J. Kim et al. 10.5194/acp-23-14425-2023
- Observational Evidence of Large Contribution from Primary Sources for Carbon Monoxide in the South Asian Outflow S. Dasari et al. 10.1021/acs.est.1c05486
- Wildfire smoke in the lower stratosphere identified by in situ CO observations J. Hooghiem et al. 10.5194/acp-20-13985-2020
- Observed decade-long improvement of combustion efficiency in the Yangtze River Delta region in China J. Zhao et al. 10.1088/1748-9326/ad521e
- Urban flask measurements of CO2ff and CO to identify emission sources at different site types in Auckland, New Zealand H. Young et al. 10.1098/rsta.2022.0204
- Diagenetic evolution of Early Eocene Chorgali Formation in the Upper Indus Basin of Pakistan: outcrop, petrographic and geochemical signatures M. Ibrar et al. 10.1007/s13146-025-01061-9
- Uncertainty in continuous ΔCO-based ΔffCO2 estimates derived from 14C flask and bottom-up ΔCO ∕ ΔffCO2 ratios F. Maier et al. 10.5194/acp-24-8205-2024
12 citations as recorded by crossref.
- Efficacy of the CO Tracer Technique in Partitioning Biogenic and Anthropogenic Atmospheric CO2 Signals in the Humid Subtropical Eastern Highland Rim City of Cookeville, Tennessee W. Gichuhi & L. Gamage 10.3390/atmos14020208
- The use of δ 13C in CO to determine removal of CH4 by Cl radicals in the atmosphere * T. Röckmann et al. 10.1088/1748-9326/ad4375
- Isotopic source signatures of stratospheric CO inferred from in situ vertical profiles J. Hooghiem et al. 10.1038/s41612-025-00986-1
- High‐Resolution Lagrangian Inverse Modeling of CO2 Emissions Over the Paris Region During the First 2020 Lockdown Period K. Nalini et al. 10.1029/2021JD036032
- Observing Anthropogenic and Biogenic CO2 Emissions in Los Angeles Using a Dense Sensor Network J. Kim et al. 10.1021/acs.est.4c11392
- Quantification of fossil fuel CO2 from combined CO, δ13CO2 and Δ14CO2 observations J. Kim et al. 10.5194/acp-23-14425-2023
- Observational Evidence of Large Contribution from Primary Sources for Carbon Monoxide in the South Asian Outflow S. Dasari et al. 10.1021/acs.est.1c05486
- Wildfire smoke in the lower stratosphere identified by in situ CO observations J. Hooghiem et al. 10.5194/acp-20-13985-2020
- Observed decade-long improvement of combustion efficiency in the Yangtze River Delta region in China J. Zhao et al. 10.1088/1748-9326/ad521e
- Urban flask measurements of CO2ff and CO to identify emission sources at different site types in Auckland, New Zealand H. Young et al. 10.1098/rsta.2022.0204
- Diagenetic evolution of Early Eocene Chorgali Formation in the Upper Indus Basin of Pakistan: outcrop, petrographic and geochemical signatures M. Ibrar et al. 10.1007/s13146-025-01061-9
- Uncertainty in continuous ΔCO-based ΔffCO2 estimates derived from 14C flask and bottom-up ΔCO ∕ ΔffCO2 ratios F. Maier et al. 10.5194/acp-24-8205-2024
Latest update: 30 May 2025
Short summary
Stable isotopes of Carbon Monoxide (CO) and radiocarbon carbon dioxide were measured over three summers at Indianapolis, Indiana, US, and for 1 year at a site thought to be strongly influenced by CO from oxidized volatile organic compounds (VOCs) in South Carolina, US. The Indianapolis results were used to provide an estimate of the carbon and oxygen isotopic signatures of CO produced from oxidized VOCs. This updated estimate agrees well with the data from South Carolina during the summer.
Stable isotopes of Carbon Monoxide (CO) and radiocarbon carbon dioxide were measured over three...
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