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
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