2012-07-26 14:15:24.0 [mpmorahan] insert Definition (id: null text: Arctic methane release is the release of methane from seas and soils in permafrost regions of the Arctic, as part of a more general release of carbon from these soils and seas. Whilst a long-term natural process, it may be exacerbated by global warming. This results in a positive feedback effect, as methane is itself a powerful greenhouse gas. The feedback of the undisturbed process is comparably weak, however, because the local release leads to a warming spread over the whole globe. The Arctic region is one of the many natural sources of the greenhouse gas methane.[1] Global warming may accelerate its release, due to both release of methane from existing stores, and from methanogenesis in rotting biomass.[2] Large quantities of methane are stored in the Arctic in natural gas deposits, permafrost, and as submarine clathrates. Permafrost and clathrates degrade on warming, thus large releases of methane from these sources may arise as a result of global warming.[3][4] Other sources of methane include submarine taliks, river transport, ice complex retreat, submarine permafrost and decaying gas hydrate deposits.[5] language code: en);
2012-06-26 15:24:12.0 [gee-cee] Insert Concept add broader relation (PERMAFROST/METHANE RELEASE [478092f3-7cdd-4136-84ec-cebf0d539480,40085] - PALEOCLIMATE INDICATORS [c9a5b3eb-7556-41a8-a2b8-c015db80e5b2,39947]);
Arctic methane release is the release of methane from seas and soils in permafrost regions of the Arctic, as part of a more general release of carbon from these soils and seas. Whilst a long-term natural process, it may be exacerbated by global warming. This results in a positive feedback effect, as methane is itself a powerful greenhouse gas. The feedback of the undisturbed process is comparably weak, however, because the local release leads to a warming spread over the whole globe. The Arctic region is one of the many natural sources of the greenhouse gas methane.[1] Global warming may accelerate its release, due to both release of methane from existing stores, and from methanogenesis in rotting biomass.[2] Large quantities of methane are stored in the Arctic in natural gas deposits, permafrost, and as submarine clathrates. Permafrost and clathrates degrade on warming, thus large releases of methane from these sources may arise as a result of global warming.[3][4] Other sources of methane include submarine taliks, river transport, ice complex retreat, submarine permafrost and decaying gas hydrate deposits.[5]
PERMAFROST/METHANE RELEASE
PALEOCLIMATE INDICATORS