You are not currently logged in.
Access JSTOR through your library or other institution:
If You Use a Screen ReaderThis content is available through Read Online (Free) program, which relies on page scans. Since scans are not currently available to screen readers, please contact JSTOR User Support for access. We'll provide a PDF copy for your screen reader.
Ocean Methane Hydrates as a Slow Tipping Point in the Global Carbon Cycle
David Archer, Bruce Buffett, Victor Brovkin and Hans Joachim Schellnhuber
Proceedings of the National Academy of Sciences of the United States of America
Vol. 106, No. 49 (Dec. 8, 2009), pp. 20596-20601
Published by: National Academy of Sciences
Stable URL: http://www.jstor.org/stable/40536042
Page Count: 6
You can always find the topics here!Topics: Methane, Hydrates, Climate models, Oceans, Sediments, Paleoclimatology, Simulations, Climate cycles, Ocean floor, Carbon dioxide
Were these topics helpful?See somethings inaccurate? Let us know!
Select the topics that are inaccurate.
Since scans are not currently available to screen readers, please contact JSTOR User Support for access. We'll provide a PDF copy for your screen reader.
Preview not available
We present a model of the global methane inventory as hydrate and bubbles below the sea floor. The model predicts the inventory of CH₄ in the ocean today to be ≈1600-2,000 Pg of C. Most of the hydrate in the model is in the Pacific, in large part because lower oxygen levels enhance the preservation of organic carbon. Because the oxygen concentration today may be different from the long-term average, the sensitivity of the model to O₂ is a source of uncertainty in predicting hydrate inventories. Cold water column temperatures in the high latitudes lead to buildup of hydrates in the Arctic and Antarctic at shallower depths than is possible in low latitudes. A critical bubble volume fraction threshold has been proposed as a critical threshold at which gas migrates all through the sediment column. Our model lacks many factors that lead to heterogeneity in the real hydrate reservoir in the ocean, such as preferential hydrate formation in sandy sediments and subsurface gas migration, and is therefore conservative in its prediction of releasable methane, finding only 35 Pg of C released after 3 °C of uniform warming by using a 10% critical bubble volume. If 2.5% bubble volume is taken as critical, then 940 Pg of C might escape in response to 3 °C warming. This hydrate model embedded into a global climate model predicts ≈0.4-0.5 °C additional warming from the hydrate response to fossil fuel CO₂ release, initially because of methane, but persisting through the 10-kyr duration of the simulations because of the CO₂ oxidation product of methane.
Proceedings of the National Academy of Sciences of the United States of America © 2009 National Academy of Sciences