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
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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 |
DOI | 10.1007/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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