Response of
Methane Hydrate Systems to Environmental Change.
These new projects, managed by the Energy Department's National Energy Technology Laboratory, will focus research on field programs for deepwater hydrate characterization, the response of
methane hydrate systems to changing climates, and advances in the understanding of gas - hydrate - bearing deposits.
Not exact matches
«But it's not like the
hydrates are just building up over time, because we're also losing
methane out of these
systems.»
Even if engineers could construct a
system to bring a load of
hydrate to the surface before it disappeared, extracting the
methane from the matrix of mud and rock would still present a problem.
We don't know that anthropogenic global warming will be limited before the
system goes into runaway positive feedback driven by melting
methane hydrates we can't control.
Pachauri outlined the potential for major changes to the climate
system, which could overwhelm human response strategies - breakdown of the thermohaline circulation, disintegration of the West Antarctic Ice Sheet, a shift in mean climate towards an El Nino - like state, reduced carbon sink capacity,
methane release from
hydrates, and a rearrangement of biome distributions.
Knowledge of the timescales of gas
hydrate dissociation and subsequent
methane release are critical in understanding the impact of marine gas
hydrates on the ocean — atmosphere
system, says Shyam Chand, researcher at NGU / CAGE.
Indeed, the long lifetime of fossil fuel carbon in the climate
system and persistence of the ocean warming ensure that «slow» feedbacks, such as ice sheet disintegration, changes of the global vegetation distribution, melting of permafrost, and possible release of
methane from
methane hydrates on continental shelves, would also have time to come into play.
Dramatic warming and upheaval of the carbon
system at the end of the Paleocene Epoch have been linked to massive dissociation of sedimentary
methane hydrate.
They report that these
methane hydrates were found in «coarse - grained sand - rich depositional
systems in the Krishna - Godavari basin» and are more easily mined than the
methane hydrates off the United States continental shelf.
They claim that salt allows the
methane hydrate deposits to be at the «triple point» of the
system making the
system much more temperature sensitive than low salt deposits.
Archer et al. (13) provide evidence that
methane hydrates in deep - sea sediments should be regarded as TE in the climate
system.