I noticed this article via a mention on The Australian's website this morning. Yes, that's right, The Australian. What's going on? The regular science editor on holiday?
Anyhow, while it is basically an estimate of how much carbon (and CO2) could be coming from defrosting Siberian permafrost, the figures are quite large sounding:
Thawing of Arctic permafrost could release significant amounts of carbon into the atmosphere in this century3. Ancient Ice Complex deposits outcropping along the ~7,000-kilometre-long coastline of the East Siberian Arctic Shelf (ESAS)4, 5, and associated shallow subsea permafrost6, 7, are two large pools of permafrost carbon8, yet their vulnerabilities towards thawing and decomposition are largely unknown9, 10, 11. Recent Arctic warming is stronger than has been predicted by several degrees, and is particularly pronounced over the coastal ESAS region12, 13. There is thus a pressing need to improve our understanding of the links between permafrost carbon and climate in this relatively inaccessible region. Here we show that extensive release of carbon from these Ice Complex deposits dominates (57 ± 2 per cent) the sedimentary carbon budget of the ESAS, the world’s largest continental shelf, overwhelming the marine and topsoil terrestrial components. Inverse modelling of the dual-carbon isotope composition of organic carbon accumulating in ESAS surface sediments, using Monte Carlo simulations to account for uncertainties, suggests that 44 ± 10 teragrams of old carbon is activated annually from Ice Complex permafrost, an order of magnitude more than has been suggested by previous studies14. We estimate that about two-thirds (66 ± 16 per cent) of this old carbon escapes to the atmosphere as carbon dioxide, with the remainder being re-buried in shelf sediments.
For those who say "why does a thawing Arctic ice cap matter?", there's part of your answer.
No comments:
Post a Comment