• DocumentCode
    2709232
  • Title

    Carbon cycle review of the permafrost in Qinghai-Tibet Plateau

  • Author

    Xie, Zhenhong ; Jiang, Qigang ; Wu, Hao

  • Author_Institution
    Coll. of Geoexploration Sci. & Technol., Jilin Univ., Changchun, China
  • fYear
    2011
  • fDate
    24-26 June 2011
  • Firstpage
    1
  • Lastpage
    4
  • Abstract
    The permafrost in Qinghai-Tibet Plateau is the biggest thickness and the broadest area in middle and low latitude in the present world, the permafrost ecosystem is one of main ecosystem, the carbon cycle of permafrost ecosystems plays an important role in the global carbon cycle. Firstly, reviewed research progress of the permafrost and temperature changes and reasons for the differences, and subsequently summarized permafrost carbon emissions and sinks, but so far it is still unclear how the rising temperature and changes in permafrost influences soil organic carbon dynamically there, thus, we must study the Tibetan Plateau on the entire region avoiding inconsistencies in the local area of permafrost distribution, and long-term observations and experiments should be conducted in order to explain the relationship of climate changes and permafrost and soil organic carbon cyclical.
  • Keywords
    atmospheric boundary layer; atmospheric composition; glaciology; ice; soil; China; Qinghai-Tibet plateau; global carbon cycle; permafrost carbon cycle; permafrost carbon emissions; permafrost carbon sinks; permafrost ecosystem; soil organic carbon; temperature changes; Carbon; Carbon dioxide; Global warming; Land surface temperature; Snow; Soil; Qinghai-Tibet Plateau; carbon cycle; climatic change; permafrost;
  • fLanguage
    English
  • Publisher
    ieee
  • Conference_Titel
    Geoinformatics, 2011 19th International Conference on
  • Conference_Location
    Shanghai
  • ISSN
    2161-024X
  • Print_ISBN
    978-1-61284-849-5
  • Type

    conf

  • DOI
    10.1109/GeoInformatics.2011.5980869
  • Filename
    5980869