Publikationsdatum:
2016-10-04
Beschreibung:
We report continuous surface observations of carbon dioxide (CO2) and methane (CH4) from the Los Angeles (LA) Megacity Carbon Project during 2015. We devised a calibration strategy, methods for selection of background air masses, calculation of urban enhancements, and a detailed algorithm for estimating uncertainties in urban scale CO2 and CH4 measurements. These methods are essential for understanding carbon fluxes from the LA megacity and other complex urban environments globally. We estimate background mole fractions entering LA using observations from four "extra-urban" sites including: two "coastal/marine" sites, one "continental" site in the high desert northeast of LA, and one "continental/mid-troposphere" site located in the San Gabriel Mountains. We find that a local marine background can be established to within roughly 1 ppm CO2 and 10 ppb CH4 using these local measurement sites. We also show that continental sites may not be relevant for selecting background observations during summer months due to the prevalence of onshore flow, which could transport CO2 and CH4 from the LA Basin to relatively remote sites. Overall, atmospheric carbon dioxide and methane levels are highly variable across Los Angeles. "Urban" and "suburban" sites show moderate to large CO2 and CH4 enhancements relative to a marine background to estimate. An urban site near Downtown LA has a median enhancement of roughly 20 ppm CO2 and 150 ppb CH4 during all hours, and roughly 15 ppm CO2 and 80 ppb ΔCH4 during midday hours (roughly 12–16:00 LT, local time), which is the typical period of focus for flux inversions. The estimated measurement uncertainty is typically better than 0.1 ppm CO2 and 1 ppb CH4 based on the repeated standard gas measurements from the LA sites during the last 1–2 years, similar to Andrews et al. (2014). The largest component of the measurement uncertainty is due to the observations being elevated relative to the single-point calibration method; however the uncertainty in the background mole fraction is much larger than the measurement uncertainty. The approach to identifying background mole fractions described here results in uncertainty ranging from roughly 5 and 15 % of the enhancement near downtown LA for CO2 and CH4, respectively, during afternoon hours. Overall, analytical and background uncertainties are small relative to the local CO2 and CH4 enhancements, however, our results suggest that reducing the uncertainty to less than 5 % of the enhancement will require detailed assessment of the impact of meteorology on background conditions.
Digitale ISSN:
1680-7375
Thema:
Geologie und Paläontologie
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