Distributed natural gas venting offshore along the Cascadia margin.
basic_science · Level V
Where this comes from
- Record sourced from PubMed, PMID 30111802.
- Also identified by DOI 10.1038/s41467-018-05736-x and PMC identifier 6093902.
- Licence recorded as CC BY.
- The licence permits redistribution, so the abstract is shown in full and the full text is available from the publisher.
Abstract
Widespread gas venting along the Cascadia margin is investigated from acoustic water column data and reveals a nonuniform regional distribution of over 1100 mapped acoustic flares. The highest number of flares occurs on the shelf, and the highest flare density is seen around the nutrition-rich outflow of the Juan de Fuca Strait. We determine ∼430 flow-rates at ∼340 individual flare locations along the margin with instantaneous in situ values ranging from ∼6 mL min<sup>-1</sup> to ∼18 L min<sup>-1</sup>. Applying a tidal-modulation model, a depth-dependent methane density, and extrapolating these results across the margin using two normalization techniques yields a combined average in situ flow-rate of ∼88 × 10<sup>6</sup> kg y<sup>-1</sup>. The average methane flux-rate for the Cascadia margin is thus estimated to ∼0.9 g y<sup>-1</sup>m<sup>-2</sup>. Combined uncertainties result in a range of these values between 4.5 and 1800% of the estimated mean values.