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The magnitude of a major methane leak

The Aliso Canyon underground gas storage facility outside Los Angeles, CA, houses enormous natural gas reserves. One well at the site experienced a blowout in late October 2015 and began leaking gas until it was sealed in February 2016. Over the course of 13 flights in the region, Conley et al. sampled the air column and determined daily release rates of methane (a powerful greenhouse gas) and ethane throughout the leak. The methane release rates were nearly double that of the entire Los Angeles region combined. Thus, single vulnerabilities can have major implications for state and federal climate policy.
Science, this issue p. 1317

Abstract

Single-point failures of natural gas infrastructure can hamper methane emission control strategies designed to mitigate climate change. The 23 October 2015 blowout of a well connected to the Aliso Canyon underground storage facility in California resulted in a massive release of natural gas. Analysis of methane and ethane data from dozens of plume transects, collected during 13 research-aircraft flights between 7 November 2015 and 13 February 2016, shows atmospheric leak rates of up to 60 metric tons of methane and 4.5 metric tons of ethane per hour. At its peak, this blowout effectively doubled the methane emission rate of the entire Los Angeles basin and, in total, released 97,100 metric tons of methane to the atmosphere.
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Supplementary Material

Summary

Materials and Methods
Figs. S1 and S2
Tables S1 and S2
References (3744)

Resources

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Science
Volume 351 | Issue 6279
18 March 2016

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Received: 11 January 2016
Accepted: 17 February 2016
Published in print: 18 March 2016

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Acknowledgments

The first two Scientific Aviation flights were funded by the California Energy Commission through University of California–Davis project #201401201. Subsequent flights were funded by the Southern California Gas Company, the operator of the Aliso Canyon storage facility. I.F. was supported in part by the California Agricultural Experiment Station (Hatch project CA-D-LAW-2229-H). J.P. and T.R. were supported in part by the NOAA Climate Program Office and the NOAA Atmospheric Chemistry, Carbon Cycle, and Climate program. We acknowledge the contributions of M. Trainer for scientific input and K. Aikin and S. Wolter for time-critical technical support. The views expressed here are those of the authors and do not constitute endorsement by their funding agencies. Data used in this report are posted at esrl.noaa.gov/csd/scientificaviation.

Authors

Affiliations

S. Conley*,
Scientific Aviation, 3335 Airport Road, Boulder, CO 80301, USA.
Department of Land, Air, and Water Resources, University of California–Davis, Davis, CA 95616, USA.
G. Franco
Research and Development Division, California Energy Commission, Sacramento, CA 95814, USA.
I. Faloona
Department of Land, Air, and Water Resources, University of California–Davis, Davis, CA 95616, USA.
D. R. Blake
Department of Chemistry, University of California–Irvine, Irvine, CA 92617, USA.
J. Peischl
Cooperative Institute for Research in Environmental Sciences, University of Colorado–Boulder, Boulder, CO, 80309, USA.
Earth System Research Laboratory, National Oceanic and Atmospheric Administration (NOAA), Boulder, CO, 80305, USA.
T. B. Ryerson
Earth System Research Laboratory, National Oceanic and Atmospheric Administration (NOAA), Boulder, CO, 80305, USA.

Notes

*Corresponding author. E-mail: [email protected]
These authors contributed equally to this work.

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