Wetland succession in a permafrost collapse: interactions between fire and thermokarst

نویسندگان

  • I. H. Myers-Smith
  • A. D. McGuire
چکیده

1 Institute of Arctic Biology, 311 Irving I Bldg., University of Alaska Fairbanks, Fairbanks, Alaska, 99775, USA 2 US Geological Survey, 345 Middlefield Rd. MS 962, Menlo Park, California, 94025, USA 3 Institute for Botany and Landscape Ecology, Grimmer Strasse 88, Greifswald University, 17487, Greifswald, Germany 4 U.S. Geological Survey, Alaska Cooperative Fish and Wildlife Research Unit, Univ. of Alaska Fairbanks, 214 Irving I Bldg., Univ. of Alaska Fairbanks, Fairbanks, Alaska, 99775, USA * now at: Department of Biological Sciences, CW 405, Biological Sciences Centre, University of Alberta, Edmonton, Alberta, T6G 2E9, Canada

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منابع مشابه

Wetland succession in a permafrost collapse

Wetland succession in a permafrost collapse: interactions between fire and thermokarst I. H. Myers-Smith, J. W. Harden, M. Wilmking, C. C. Fuller, A. D. McGuire, and F. S. Chapin III Institute of Arctic Biology, 311 Irving I Bldg., University of Alaska Fairbanks, Fairbanks, Alaska, 99775, USA US Geological Survey, 345 Middlefield Rd. MS 962, Menlo Park, California, 94025, USA Institute for Bota...

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Thermokarst rates intensify due to climate change and forest fragmentation in an Alaskan boreal forest lowland.

Lowland boreal forest ecosystems in Alaska are dominated by wetlands comprised of a complex mosaic of fens, collapse-scar bogs, low shrub/scrub, and forests growing on elevated ice-rich permafrost soils. Thermokarst has affected the lowlands of the Tanana Flats in central Alaska for centuries, as thawing permafrost collapses forests that transition to wetlands. Located within the discontinuous ...

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تاریخ انتشار 2007