Chris Cantrell
Senior Scientist
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Project Summary:
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The fast photochemical processes taking place in the troposphere are central to understanding the removal of trace gases. One important pathway is the reaction of free radicals with hydrocarbons, sulfur- and nitrogen-containing compounds, carbon monoxide and other species. Our research focuses on the development, improvement and deployment of mass spectrometric-based instrumentation for measurement of hydroxyl (OH), hydroperoxy (HO2) and organic peroxy radicals (RO2) (and other species), and interpretation of the data from those deployments. In early 2006, we deployed our instrumentation during the Megacities Impact on Regional & Global Environment (MIRAGE, Mexico - movie clips from Dirk Richter, EOL) and the Intercontinental Chemical Transport Experiment (INTEX-B, northeast US) campaigns. In the summer of 2007, we made measurements near Christmas Island as part of Pacific Atmospheric Sulfur Experiment (PASE - UCAR Staff Notes, Christmas in August).
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Additional Photos from INTEX-B from Dirk Richter, EOL. The data from the 2006 campaigns has been fully processed, quality assured and submitted to the corresponding archives. We have made significant progress toward understanding the role of free radicals in the oxidation chemistry of the Mexico City urban plume with particular attention to the formation of ozone and the comparisons between observed radical concentrations those estimated from constrained photochemical box models. One major finding is the systematic and dramatic under-prediction of peroxy radical amounts by models at higher amounts of NOx (NO+NO2). This is shown in Figure 1 where measured and modeled mixing ratios of HO2+RO2, HO2 and RO2 versus NOx mixing ratios are shown. The data have been binned by the NOx. Note that for NOx amounts less than about 1000 pptv, the agreements between the observations and the model estimates are reasonable (within the 35% measurement and 40% model uncertainty). At larger NOx amounts, the measurement-model differences increase. The measured values are more than a factor of 10 greater than the model values at the NOx. These differences cannot be explained by measurement and model uncertainties, and point to processes that are not represented in the model.
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Analysis will continue on the data from MIRAGE and INTEX-B campaigns as we also prepare the data from PASE study and submit it to data archive in the required format. Preparation of documentation for a potential future campaign continued this year. The Deep Convective Clouds & Chemistry Experiment (DC3 - dee-cee three) study is designed to improve understanding of the role of deep convection in modifying the composition of upper troposphere and lower stratosphere. The PI team consists of Mary Barth (MMM/ACD), Chris Cantrell (ACD), Bill Brune (Pennsylvania State), and Steve Rutledge (Colorado State) who, along with a scientific steering committee composed of university and national laboratory scientists, are leading the planning of a community-wide comprehensive study that will utilize ground-based radars, mesonets, fully configured aircraft platforms and satellite data to address several important scientific questions. An important upcoming step in this process is the submittal of the Scientific and Experimental Overview documents to the National Science Foundation.
Windows to the Universe Postcards from the Field from Chris Cantrell: |
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Community Service:
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Presentations:
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TIIMES External Collaborators: Joan Alexander, NorthWest Research Associates |
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