Current rates and mechanisms of subsea permafrost degradation in the East Siberian Arctic Shelf
The rate of subsea permafrost degradation is a key factor controlling marine methane emissions in the Arctic. Here, using re-drilled boreholes, the authors show that the ice-bonded permafrost table in the near-shore East Siberian Arctic Shelf has deepened by ∼14 cm per year over the past 31–32 years...
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Nature Portfolio
2017
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oai:doaj.org-article:b5ceac8827a5459c95a919791fe85ff52021-12-02T14:42:35ZCurrent rates and mechanisms of subsea permafrost degradation in the East Siberian Arctic Shelf10.1038/ncomms158722041-1723https://doaj.org/article/b5ceac8827a5459c95a919791fe85ff52017-06-01T00:00:00Zhttps://doi.org/10.1038/ncomms15872https://doaj.org/toc/2041-1723The rate of subsea permafrost degradation is a key factor controlling marine methane emissions in the Arctic. Here, using re-drilled boreholes, the authors show that the ice-bonded permafrost table in the near-shore East Siberian Arctic Shelf has deepened by ∼14 cm per year over the past 31–32 years.Natalia ShakhovaIgor SemiletovOrjan GustafssonValentin SergienkoLeopold LobkovskyOleg DudarevVladimir TumskoyMichael GrigorievAlexey MazurovAnatoly SalyukRoman AnanievAndrey KoshurnikovDenis KosmachAlexander CharkinNicolay DmitrevskyVictor KarnaukhAlexey GunarAlexander MeluzovDenis ChernykhNature PortfolioarticleScienceQENNature Communications, Vol 8, Iss 1, Pp 1-13 (2017) |
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Science Q Natalia Shakhova Igor Semiletov Orjan Gustafsson Valentin Sergienko Leopold Lobkovsky Oleg Dudarev Vladimir Tumskoy Michael Grigoriev Alexey Mazurov Anatoly Salyuk Roman Ananiev Andrey Koshurnikov Denis Kosmach Alexander Charkin Nicolay Dmitrevsky Victor Karnaukh Alexey Gunar Alexander Meluzov Denis Chernykh Current rates and mechanisms of subsea permafrost degradation in the East Siberian Arctic Shelf |
description |
The rate of subsea permafrost degradation is a key factor controlling marine methane emissions in the Arctic. Here, using re-drilled boreholes, the authors show that the ice-bonded permafrost table in the near-shore East Siberian Arctic Shelf has deepened by ∼14 cm per year over the past 31–32 years. |
format |
article |
author |
Natalia Shakhova Igor Semiletov Orjan Gustafsson Valentin Sergienko Leopold Lobkovsky Oleg Dudarev Vladimir Tumskoy Michael Grigoriev Alexey Mazurov Anatoly Salyuk Roman Ananiev Andrey Koshurnikov Denis Kosmach Alexander Charkin Nicolay Dmitrevsky Victor Karnaukh Alexey Gunar Alexander Meluzov Denis Chernykh |
author_facet |
Natalia Shakhova Igor Semiletov Orjan Gustafsson Valentin Sergienko Leopold Lobkovsky Oleg Dudarev Vladimir Tumskoy Michael Grigoriev Alexey Mazurov Anatoly Salyuk Roman Ananiev Andrey Koshurnikov Denis Kosmach Alexander Charkin Nicolay Dmitrevsky Victor Karnaukh Alexey Gunar Alexander Meluzov Denis Chernykh |
author_sort |
Natalia Shakhova |
title |
Current rates and mechanisms of subsea permafrost degradation in the East Siberian Arctic Shelf |
title_short |
Current rates and mechanisms of subsea permafrost degradation in the East Siberian Arctic Shelf |
title_full |
Current rates and mechanisms of subsea permafrost degradation in the East Siberian Arctic Shelf |
title_fullStr |
Current rates and mechanisms of subsea permafrost degradation in the East Siberian Arctic Shelf |
title_full_unstemmed |
Current rates and mechanisms of subsea permafrost degradation in the East Siberian Arctic Shelf |
title_sort |
current rates and mechanisms of subsea permafrost degradation in the east siberian arctic shelf |
publisher |
Nature Portfolio |
publishDate |
2017 |
url |
https://doaj.org/article/b5ceac8827a5459c95a919791fe85ff5 |
work_keys_str_mv |
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