中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Evapotranspiration dynamics over a temperate meadow ecosystem in eastern Inner Mongolia, China

文献类型:期刊论文

作者Guan, Dexin1; Li, Huidong1,2; Wang, Anzhi1; Yuan, Fenghui1; Jin, Changjie1; Wu, Jiabing1; Zhao, Tongbin3
刊名ENVIRONMENTAL EARTH SCIENCES
出版日期2016-06-01
卷号75期号:11
关键词Evapotranspiration Temperate Meadow Igbp-nect
ISSN号1866-6280
DOI10.1007/s12665-016-5786-z
英文摘要Ecosystem evapotranspiration links surface energy and water balance, which is very important to the forming and evolution of regional climate. To understand the evapotranspiration dynamic over the temperate meadow in Inner Mongolia grassland, a long-term continuous measurement of water vapour flux was conducted using eddy covariance technique from 2008 to 2013. The results showed that the seasonal variation of daily evapotranspiration displayed a unimodal pattern with maximum value of 6.45 mm day(-1). The mean value of annual evapotranspiration (ET) was 650 mm with 72 % occurring during the growing season from May to September. The annual evapotranspiration was larger than the annual precipitation (P), while less than the annual evaporation (E). The ET/P reached up to 1.91, while the ET/E was only 0.60. The evapotranspiration was not limited by precipitation due to additional water supply from surrounding dunes. The daily evapotranspiration was mainly driven by atmospheric moisture demand in the growing season with high Priestley-Taylor parameter, averaged 1.04. The daily evapotranspiration presented positive correlation with net radiation, and the correlation was affected by water vapour pressure deficit. The net radiation and water vapour pressure deficit controlled the evapotranspiration process together. The study site had the largest annual evapotranspiration and ET/P compared with the other ecosystems along the transection of Northeast China Transect, International Geosphere Biosphere Programme. The harvest activity could increase the albedo and then decrease the available energy of the surface, eventually reducing the monthly evapotranspiration as much as 33.98 % in September.
WOS研究方向Environmental Sciences & Ecology ; Geology ; Water Resources
语种英语
WOS记录号WOS:000378864300046
出版者SPRINGER
源URL[http://210.72.129.5/handle/321005/122781]  
专题中国科学院沈阳应用生态研究所
通讯作者Wu, Jiabing
作者单位1.Chinese Acad Sci, Inst Appl Ecol, Key Lab Forest Ecol & Management, Shenyang 110016, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
3.Liaoning Prov Meteorol Informat Ctr, Shenyang 110166, Peoples R China
推荐引用方式
GB/T 7714
Guan, Dexin,Li, Huidong,Wang, Anzhi,et al. Evapotranspiration dynamics over a temperate meadow ecosystem in eastern Inner Mongolia, China[J]. ENVIRONMENTAL EARTH SCIENCES,2016,75(11).
APA Guan, Dexin.,Li, Huidong.,Wang, Anzhi.,Yuan, Fenghui.,Jin, Changjie.,...&Zhao, Tongbin.(2016).Evapotranspiration dynamics over a temperate meadow ecosystem in eastern Inner Mongolia, China.ENVIRONMENTAL EARTH SCIENCES,75(11).
MLA Guan, Dexin,et al."Evapotranspiration dynamics over a temperate meadow ecosystem in eastern Inner Mongolia, China".ENVIRONMENTAL EARTH SCIENCES 75.11(2016).

入库方式: OAI收割

来源:沈阳应用生态研究所

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