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Monitoring temporal variability of bubble release at seeps: The hydroacoustic swath system GasQuant

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Monitoring temporal variability of bubble release at seeps: The hydroacoustic swath system GasQuant (English)

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Jens Greinert

1

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English

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publication date

30 July 2008

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published in

Journal of Geophysical Research

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volume

113

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issue

C7

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cites work

Dissociation of oceanic methane hydrate as a cause of the carbon isotope excursion at the end of the Paleocene

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Mud volcanoes—the most important pathway for degassing deeply buried sediments

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Hydroacoustic experiments to establish a method for the determination of methane bubble fluxes at cold seeps

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1300-m-high rising bubbles from mud volcanoes at 2080m in the Black Sea: Hydroacoustic characteristics and temporal variability

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The world's most spectacular marine hydrocarbon seeps (Coal Oil Point, Santa Barbara Channel, California): Quantification of emissions

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Fate of rising methane bubbles in stratified waters: How much methane reaches the atmosphere?

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Geological and morphological setting of 2778 methane seeps in the Dnepr paleo-delta, northwestern Black Sea

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Anomalous sea-floor backscatter patterns in methane venting areas, Dnepr paleo-delta, NW Black Sea

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Carbon cycling and chronology of climate warming during the Palaeocene/Eocene transition

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Decrease in natural marine hydrocarbon seepage near Coal Oil Point, California, associated with offshore oil production

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Methane discharge from a deep-sea submarine mud volcano into the upper water column by gas hydrate-coated methane bubbles

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Gas hydrate destabilization: enhanced dewatering, benthic material turnover and large methane plumes at the Cascadia convergent margin

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Measurements of transience and downward fluid flow near episodic methane gas vents, Hydrate Ridge, Cascadia

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Sublacustrine mud volcanoes and methane seeps caused by dissociation of gas hydrates in Lake Baikal

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Monitoring temporal variability of bubble release at seeps: The hydroacoustic swath system GasQuant

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