Top‐down estimate of methane emissions in California using a mesoscale inverse modeling technique: The South Coast Air Basin. Issue 13 (14th July 2015)

• Record Type: Journal Article
• Authors: Cui, Yu Yan; Brioude, Jerome; McKeen, Stuart A.; Angevine, Wayne M.; Kim, Si‐Wan; Frost, Gregory J.; Ahmadov, Ravan; Peischl, Jeff; Bousserez, Nicolas; Liu, Zhen; Ryerson, Thomas B.; Wofsy, Steve C.; Santoni, Gregory W.; Kort, Eric A.; Fischer, Marc L.; Trainer, Michael
• Is Part Of: Journal of geophysical research. Volume 120:Issue 13(2015:Jul.)
• Page Start: 6698
• Page End: 6711
• Publication Date: 2015-07-14
• Subjects: Atmospheric physics -- Periodicals; Geophysics -- Periodicals; 551.5
• DOI: 10.1002/2014JD023002
• Languages: English
• ISSNs: 2169-897X

Abstract

<abstract abstract-type="main" id="jgrd52271-abs-0001"> <title>Abstract</title> <p id="jgrd52271-para-0001">Methane (CH<sub>4</sub>) is the primary component of natural gas and has a larger global warming potential than CO<sub>2</sub>. Recent top‐down studies based on observations showed CH<sub>4</sub> emissions in California's South Coast Air Basin (SoCAB) were greater than those expected from population‐apportioned bottom‐up state inventories. In this study, we quantify CH<sub>4</sub> emissions with an advanced mesoscale inverse modeling system at a resolution of 8 km × 8 km, using aircraft measurements in the SoCAB during the 2010 Nexus of Air Quality and Climate Change campaign to constrain the inversion. To simulate atmospheric transport, we use the FLEXible PARTicle‐Weather Research and Forecasting (FLEXPART‐WRF) Lagrangian particle dispersion model driven by three configurations of the Weather Research and Forecasting (WRF) mesoscale model. We determine surface fluxes of CH<sub>4</sub> using a Bayesian least squares method in a four‐dimensional inversion. Simulated CH<sub>4</sub> concentrations with the posterior emission inventory achieve much better correlations with the measurements (<italic>R</italic><sup>2</sup> = 0.7) than using the prior inventory (U.S. Environmental Protection Agency's National Emission Inventory 2005, <italic>R</italic><sup>2</sup> = 0.5). The emission estimates for CH<sub>4</sub> in the posterior, 46.3 ± 9.2 Mg CH<sub>4</sub>/h, are consistent with published observation‐based estimates. Changes in the spatial distribution of CH<sub>4</sub> emissions in the SoCAB between the prior and posterior inventories are discussed. Missing or underestimated emissions from dairies, the oil/gas system, and landfills in the SoCAB seem to explain the differences between the prior and posterior inventories. We estimate that dairies contributed 5.9 ± 1.7 Mg CH<sub>4</sub>/h and the two sectors of oil and gas industries (production and downstream) and landfills together contributed 39.6 ± 8.1 Mg CH<sub>4</sub>/h in the SoCAB.</p> </abstract>