中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Changes in the Thermal and Hydraulic Regime within the Active Layer in the Qinghai-Tibet Plateau

文献类型:期刊论文

作者XIE Changwei ; ZHAO Lin ; WU Tonghua ; DONG Xicheng
刊名Journal of Mountain Science
出版日期2012-08
卷号9期号:4页码:483-491
关键词Soil temperature Water content Active layer Permafrost Qinghai-Tibet Plateau (QTP)
通讯作者XIE Changwei
英文摘要The change trends of air temperature, precipitation and evaporation from 1999 to 2008 shows that the climate in the Qinghai-Tibet Plateau permafrost region had become warmer. The analysis of the systematic active-layer data monitoring network along the Qinghai-Tibet Highway indicated that the active-layer thickness had been increasing and the soil temperature was rising. The soil temperature was rising in winter but not at the end of spring or during the entire summer. With thickening and warming of the active layer, the liquid water content of the active layer had an obvious downward migration and liquid water content in the top horizons decreased, but in the deeper horizons it increased. 
收录类别SCI
语种英语
公开日期2013-04-17
源URL[http://192.168.143.20:8080/handle/131551/5122]  
专题成都山地灾害与环境研究所_Journal of Mountain Science _Journal of Mountain Science-2012_Vol9 No.4
推荐引用方式
GB/T 7714
XIE Changwei,ZHAO Lin,WU Tonghua,et al. Changes in the Thermal and Hydraulic Regime within the Active Layer in the Qinghai-Tibet Plateau[J]. Journal of Mountain Science,2012,9(4):483-491.
APA XIE Changwei,ZHAO Lin,WU Tonghua,&DONG Xicheng.(2012).Changes in the Thermal and Hydraulic Regime within the Active Layer in the Qinghai-Tibet Plateau.Journal of Mountain Science,9(4),483-491.
MLA XIE Changwei,et al."Changes in the Thermal and Hydraulic Regime within the Active Layer in the Qinghai-Tibet Plateau".Journal of Mountain Science 9.4(2012):483-491.

入库方式: OAI收割

来源:成都山地灾害与环境研究所

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