Ebullition and storm-induced methane release from the East Siberian Arctic Shelf

Natalia Evgenievna Shakhova, Igor Petrovich Semiletov, Ira Leifer, Valentin Sergienko, Anatoly Salyuk, Denis Kosmach, Denis Chernykh, Chris Stubbs, Dmitry Nicolsky, Vladimir Tumskoy, Örjan Gustafsson

    Результат исследований: Материалы для журналаСтатья

    139 Цитирования (Scopus)

    Выдержка

    Vast quantities of carbon are stored in shallow Arctic reservoirs, such as submarine and terrestrial permafrost. Submarine permafrost on the East Siberian Arctic Shelf started warming in the early Holocene, several thousand years ago. However, the present state of the permafrost in this region is uncertain. Here, we present data on the temperature of submarine permafrost on the East Siberian Arctic Shelf using measurements collected from a sediment core, together with sonar-derived observations of bubble flux and measurements of seawater methane levels taken from the same region. The temperature of the sediment core ranged from-1.8 to 0C. Although the surface layer exhibited the lowest temperatures, it was entirely unfrozen, owing to significant concentrations of salt. On the basis of the sonar data, we estimate that bubbles escaping the partially thawed permafrost inject 100-630 mg methane m-2 d-1 into the overlying water column. We further show that water-column methane levels had dropped significantly following the passage of two storms. We suggest that significant quantities of methane are escaping the East Siberian Shelf as a result of the degradation of submarine permafrost over thousands of years. We suggest that bubbles and storms facilitate the flux of this methane to the overlying ocean and atmosphere, respectively.

    Язык оригиналаАнглийский
    Страницы (с-по)64-70
    Число страниц7
    ЖурналNature Geoscience
    Том7
    Номер выпуска1
    DOI
    СостояниеОпубликовано - 2014

    Отпечаток

    permafrost
    methane
    bubble
    sonar
    sediment core
    water column
    surface layer
    warming
    temperature
    Holocene
    salt
    seawater
    degradation
    atmosphere
    carbon
    ocean

    ASJC Scopus subject areas

    • Earth and Planetary Sciences(all)

    Цитировать

    Ebullition and storm-induced methane release from the East Siberian Arctic Shelf. / Shakhova, Natalia Evgenievna; Semiletov, Igor Petrovich; Leifer, Ira; Sergienko, Valentin; Salyuk, Anatoly; Kosmach, Denis; Chernykh, Denis; Stubbs, Chris; Nicolsky, Dmitry; Tumskoy, Vladimir; Gustafsson, Örjan.

    В: Nature Geoscience, Том 7, № 1, 2014, стр. 64-70.

    Результат исследований: Материалы для журналаСтатья

    Shakhova, NE, Semiletov, IP, Leifer, I, Sergienko, V, Salyuk, A, Kosmach, D, Chernykh, D, Stubbs, C, Nicolsky, D, Tumskoy, V & Gustafsson, Ö 2014, 'Ebullition and storm-induced methane release from the East Siberian Arctic Shelf', Nature Geoscience, том. 7, № 1, стр. 64-70. https://doi.org/10.1038/ngeo2007
    Shakhova, Natalia Evgenievna ; Semiletov, Igor Petrovich ; Leifer, Ira ; Sergienko, Valentin ; Salyuk, Anatoly ; Kosmach, Denis ; Chernykh, Denis ; Stubbs, Chris ; Nicolsky, Dmitry ; Tumskoy, Vladimir ; Gustafsson, Örjan. / Ebullition and storm-induced methane release from the East Siberian Arctic Shelf. В: Nature Geoscience. 2014 ; Том 7, № 1. стр. 64-70.
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    abstract = "Vast quantities of carbon are stored in shallow Arctic reservoirs, such as submarine and terrestrial permafrost. Submarine permafrost on the East Siberian Arctic Shelf started warming in the early Holocene, several thousand years ago. However, the present state of the permafrost in this region is uncertain. Here, we present data on the temperature of submarine permafrost on the East Siberian Arctic Shelf using measurements collected from a sediment core, together with sonar-derived observations of bubble flux and measurements of seawater methane levels taken from the same region. The temperature of the sediment core ranged from-1.8 to 0C. Although the surface layer exhibited the lowest temperatures, it was entirely unfrozen, owing to significant concentrations of salt. On the basis of the sonar data, we estimate that bubbles escaping the partially thawed permafrost inject 100-630 mg methane m-2 d-1 into the overlying water column. We further show that water-column methane levels had dropped significantly following the passage of two storms. We suggest that significant quantities of methane are escaping the East Siberian Shelf as a result of the degradation of submarine permafrost over thousands of years. We suggest that bubbles and storms facilitate the flux of this methane to the overlying ocean and atmosphere, respectively.",
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    AU - Sergienko, Valentin

    AU - Salyuk, Anatoly

    AU - Kosmach, Denis

    AU - Chernykh, Denis

    AU - Stubbs, Chris

    AU - Nicolsky, Dmitry

    AU - Tumskoy, Vladimir

    AU - Gustafsson, Örjan

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