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Ground-Based Atmospheric Measurements of CO:CO2 Ratios in Eastern Highland Rim Using a CO Tracer Technique
journal contribution
posted on 2020-03-18, 20:45 authored by Lahiru
P. Gamage, Elijah G. Hix, Wilson K. GichuhiWe present ground-based atmospheric
measurements of ratios between
anthropogenic carbon monoxide (COan) and carbon dioxide
(CO2an) (β–1 ratios) in Cookeville,
Tennessee (36.1628° N, 85.5016° W), a medium-sized city
located within the Eastern Highland Rim region of the United States,
obtained using a continuous wavelength-scanned cavity ring-down spectrometer
(CRDS). In contrast to the summer season, the winter and spring β–1 values are reasonably high, where a tight correlation
between the above-background mole fractions of CO and CO2 is exhibited (as given by the high R2 value). The winter season is characterized by relatively high COan than biospheric CO2 signals (CO2Bio) due to fossil fuel heating sources and reduced biospheric uptake
of CO2. The lowest estimated seasonal background CO2 and CO mole fractions during the study period are 407.1 ±
11.3 ppm and 144.9 ± 2.1 ppb, respectively. During the summer,
the biogenic CO source from isoprene oxidation collocates with direct
anthropogenic CO sources, leading to uncertainties in the calculated
summertime β–1 values. For 2017, β–1 values (ppb:ppm) of 9.7 ± 0.4, 5.3 ± 0.4,
and 2.0 ± 0.2 were obtained for the winter, spring and summer
seasons, respectively. In 2018, a similar seasonal variability in
the β–1 ratios was obtained with values of
8.7 ± 0.5, 7.4 ± 0.7, and 2.6 ± 0.5 for winter, spring,
and summer seasons, respectively. While the estimated percentage contribution
of the oxidation reaction between the OH radical and isoprene (CH2C(CH3)–CHCH2 +
OH) to the total summertime CO budget is less than 50%, the relative
amounts may be significant enough to imply that any future study based
on the CO as a tracer of combustion emission should account for its
photochemical production through biogenic volatile organic compounds
in the summertime.
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Keywords
anthropogenic CO sourcessummertime CO budgetsummer seasonsOHbackground CO 2Eastern Highland Rim regionR 2 valueCO 2 Biowavelength-scanned cavity ring-down spectrometerCO 2Ground-Based Atmospheric MeasurementsCO mole fractionsEastern Highland RimCO Tracer Techniquefuel heating sourcesbiospheric CO 2 signalsCHisoprene oxidation collocatesabove-background mole fractionsanthropogenic carbon monoxideCRDSbiogenic CO source
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