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Methane hydrates and global climate

Journal Article · · Global Biogeochemical Cycles; (USA)
OSTI ID:6657129
 [1]
  1. Geological Survey, Menlo Park, CA (USA)
Methane hydrates are globally widespread in permafrost regions and beneath the sea in sediment of outer continental margins. The amount of methane sequestered in gas hydrates is probably enormous, but estimates of the amounts are speculative and range over three orders of magnitude (about 1,000 to 1,000,000 gigatons). A question of current interest concerns the possible consequences of an addition of methane to the atmosphere from destabilized methane hydrates due to global warming. Models of greenhouse warming predict that climatic change will be greatest in the Arctic. Thus, if methane from destabilized gas hydrates contributes to greenhouse warming, this stabilization will most likely take place first in the Arctic, particularly in the shallow nearshore regions of the Arctic Ocean where offshore permafrost is found. The process of permafrost warming and release of methane from gas hydrates may already be in progress, but the amount being released now and to be released in the 21st century is probably small. The positive feedback of this atmospheric methane on global climates will likely be minimal. 48 refs., 4 figs., 2 tabs.
OSTI ID:
6657129
Journal Information:
Global Biogeochemical Cycles; (USA), Journal Name: Global Biogeochemical Cycles; (USA) Vol. 2:3; ISSN 0886-6236; ISSN GBCYE
Country of Publication:
United States
Language:
English

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