Top-down estimate of methane emissions in California using a mesoscale inverse modeling technique: The South Coast Air Basin
- National Oceanic and Atmospheric Administration (NOAA), Boulder, CO (United States); Univ. of Colorado Boulder, CO (United States)
- National Oceanic and Atmospheric Administration (NOAA), Boulder, CO (United States); Univ. of Colorado Boulder, CO (United States); National Centre for Scientific Research-Mixed Organizations (CNRS-UMR), Paris (France)
- National Oceanic and Atmospheric Administration (NOAA), Boulder, CO (United States). Earth System Research Lab.; Univ. of Colorado Boulder, CO (United States)
- National Oceanic and Atmospheric Administration (NOAA), Boulder, CO (United States; Univ. of Colorado Boulder, CO (United States)
- Univ. of Colorado, Boulder, CO (United States)
- Sandia National Lab. (SNL-CA), Livermore, CA (United States); Now at Ramboll Environ US Corporation, Novato, CA (United States)
- National Oceanic and Atmospheric Administration (NOAA), Boulder, CO (United States)
- Harvard Univ., Cambridge, MA (United States)
- Univ. of Michigan, Ann Arbor, MI (United States)
- Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States)
Methane (CH4) is the primary component of natural gas and has a larger global warming potential than CO2. Some recent top-down studies based on observations showed CH4 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 CH4 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 CH4 using a Bayesian least squares method in a four-dimensional inversion. Simulated CH4 concentrations with the posterior emission inventory achieve much better correlations with the measurements (R2 = 0.7) than using the prior inventory (U.S. Environmental Protection Agency's National Emission Inventory 2005, R2 = 0.5). The emission estimates for CH4 in the posterior, 46.3 ± 9.2 Mg CH4/h, are consistent with published observation-based estimates. Changes in the spatial distribution of CH4 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. Furthermore, we estimate that dairies contributed 5.9 ± 1.7 Mg CH4/h and the two sectors of oil and gas industries (production and downstream) and landfills together contributed 39.6 ± 8.1 Mg CH4/h in the SoCAB.
- Research Organization:
- Sandia National Lab. (SNL-NM), Albuquerque, NM (United States)
- Sponsoring Organization:
- USDOE National Nuclear Security Administration (NNSA)
- Grant/Contract Number:
- AC04-94AL85000
- OSTI ID:
- 1235292
- Report Number(s):
- SAND-2015-4909J; 594363
- Journal Information:
- Journal of Geophysical Research: Atmospheres (Online), Vol. 120, Issue 13; ISSN 2169-8996
- Publisher:
- American Geophysical UnionCopyright Statement
- Country of Publication:
- United States
- Language:
- English
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