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Transient seafloor venting on continental slopes from warming‐induced methane hydrate dissociation

Journal Article · · Geophysical Research Letters
DOI:https://doi.org/10.1002/2015GL067012· OSTI ID:1402313
 [1];  [2]
  1. Department of Geological Sciences University of Texas at Austin Austin Texas USA, Institute for Geophysics University of Texas at Austin Austin Texas USA
  2. Department of Geological Sciences University of Texas at Austin Austin Texas USA, Institute for Geophysics University of Texas at Austin Austin Texas USA, Bureau of Economic Geology University of Texas at Austin Austin Texas USA

Abstract

Methane held in frozen hydrate cages within marine sediment comprises one of the largest carbon reservoirs on the planet. Recent submarine observations of widespread methane seepage may record hydrate dissociation due to oceanic warming, which consequently may further amplify climate change. Here we simulate the effect of seafloor warming on marine hydrate deposits using a multiphase flow model. We show that hydrate dissociation, gas migration, and subsequent hydrate formation cangenerate temporary methane venting into the ocean through the hydrate stability zone. Methane seeps venting through the hydrate stability zone on the eastern Atlantic margin may record this process due to warming begun thousands of years ago. Our results contrast with the traditional view that venting occurs only updip of the hydrate stability zone.

Sponsoring Organization:
USDOE
OSTI ID:
1402313
Journal Information:
Geophysical Research Letters, Journal Name: Geophysical Research Letters Journal Issue: 24 Vol. 42; ISSN 0094-8276
Publisher:
American Geophysical Union (AGU)Copyright Statement
Country of Publication:
United States
Language:
English

References (19)

Thermogenic methane injection via bubble transport into the upper Arctic Ocean from the hydrate-charged Vestnesa Ridge, Svalbard journal May 2014
Seabed fluid expulsion along the upper slope and outer shelf of the U.S. Atlantic continental margin: U.S. ATLANTIC MARGIN FLUID EXPULSION journal January 2014
The evolution of methane vents that pierce the hydrate stability zone in the world's oceans: EVOLUTION OF METHANE VENTS journal August 2014
Dissociation of Cascadia margin gas hydrates in response to contemporary ocean warming journal December 2014
Widespread gas hydrate instability on the upper U.S. Beaufort margin: U.S. Beaufort Margin Hydrate Instability journal December 2014
Estimates of future warming-induced methane emissions from hydrate offshore west Svalbard for a range of climate models: 21st Century CH journal May 2015
The response of methane hydrate beneath the seabed offshore Svalbard to ocean warming during the next three centuries journal October 2013
The prediction of methane solubility in natural waters to high ionic strength from 0 to 250°C and from 0 to 1600 bar journal April 1992
Formation of natural gas hydrates in marine sediments: 2. Thermodynamic calculations of stability conditions in porous sediments journal October 1999
Enhanced lifetime of methane bubble streams within the deep ocean: ENHANCED LIFETIME OF METHANE BUBBLES journal August 2002
Dynamic multiphase flow model of hydrate formation in marine sediments journal January 2007
Escape of methane gas from the seabed along the West Spitsbergen continental margin: ARCTIC METHANE GAS PLUMES journal August 2009
Large-scale simulation of methane hydrate dissociation along the West Spitsbergen Margin journal January 2009
Rising Arctic Ocean temperatures cause gas hydrate destabilization and ocean acidification: ARCTIC OCEAN GAS HYDRATES journal April 2011
Methane release from warming-induced hydrate dissociation in the West Svalbard continental margin: Timing, rates, and geological controls: METHANE FROM WARMING-INDUCED HYDRATE DISSOCIATION IN SVALBARD journal January 2013
Recent changes to the Gulf Stream causing widespread gas hydrate destabilization journal October 2012
Widespread methane leakage from the sea floor on the northern US Atlantic margin journal August 2014
Temporal Constraints on Hydrate-Controlled Methane Seepage off Svalbard journal January 2014
Abiotic methane from ultraslow-spreading ridges can charge Arctic gas hydrates journal May 2015

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