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- W1659276873 abstract "[1] The release of methane sequestered within deep-sea methane hydrates is postulated as a mechanism for abrupt climate change; however, whether emitted seabed methane reaches the atmosphere is debatable. We observed methane emissions for a blowout from a shallow (22 m) hydrocarbon seep. The emission from the blowout was determined from atmospheric plume measurements. Simulations suggest a 1.1% gas loss to dissolution compared to ∼10% loss for a typical low-flux bubble plume. Transfer to the atmosphere primarily was enhanced by the rapid upwelling flows induced by the massive discharge. This mechanism could allow methane suddenly released from deeper (>250 m) waters to contribute significantly to atmospheric methane budgets." @default.
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- W1659276873 date "2006-07-20" @default.
- W1659276873 modified "2023-10-16" @default.
- W1659276873 title "Natural marine seepage blowout: Contribution to atmospheric methane" @default.
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- W1659276873 doi "https://doi.org/10.1029/2005gb002668" @default.
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