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Fred Murphy

Fred is a Scientist Emeritus with the Geology, Minerals, Energy, and Geophysics Science Center

Science and Products

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scientists collecting permafrost cores

Arctic Biogeochemical Response to Permafrost Thaw (ABRUPT)

Warming and thawing of permafrost soils in the Arctic is expected to become widespread over the coming decades. Permafrost thaw changes ecosystem structure and function, affects resource availability for wildlife and society, and decreases ground stability which affects human infrastructure. Since permafrost soils contain about half of the global soil carbon (C) pool, the magnitude of C losses...
By
Climate Research and Development Program, Geology, Minerals, Energy, and Geophysics Science Center
link

Arctic Biogeochemical Response to Permafrost Thaw (ABRUPT)

Warming and thawing of permafrost soils in the Arctic is expected to become widespread over the coming decades. Permafrost thaw changes ecosystem structure and function, affects resource availability for wildlife and society, and decreases ground stability which affects human infrastructure. Since permafrost soils contain about half of the global soil carbon (C) pool, the magnitude of C losses...
Learn More
Image: Collecting Gas Sample at a Fumarole
link
Image: Taking Measurements at a Thermal Area
link

Science and Products

  • Science
    link
    scientists collecting permafrost cores

    Arctic Biogeochemical Response to Permafrost Thaw (ABRUPT)

    Warming and thawing of permafrost soils in the Arctic is expected to become widespread over the coming decades. Permafrost thaw changes ecosystem structure and function, affects resource availability for wildlife and society, and decreases ground stability which affects human infrastructure. Since permafrost soils contain about half of the global soil carbon (C) pool, the magnitude of C losses...
    By
    Climate Research and Development Program, Geology, Minerals, Energy, and Geophysics Science Center
    link

    Arctic Biogeochemical Response to Permafrost Thaw (ABRUPT)

    Warming and thawing of permafrost soils in the Arctic is expected to become widespread over the coming decades. Permafrost thaw changes ecosystem structure and function, affects resource availability for wildlife and society, and decreases ground stability which affects human infrastructure. Since permafrost soils contain about half of the global soil carbon (C) pool, the magnitude of C losses...
    Learn More
  • Multimedia
    Image: Collecting Gas Sample at a Fumarole
    link
    Image: Taking Measurements at a Thermal Area
    link