中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Actual and Reference Evapotranspiration in a Cornfield in the Zhangye Oasis, Northwestern China

文献类型:期刊论文

作者Gu, Lianglei1; Hu, Zeyong1; Yao, Jimin2; Sun, Genhou1
刊名WATER
出版日期2017-07-01
卷号9期号:7页码:16
关键词actual evapotranspiration reference evapotranspiration crop coefficient K-c eddy covariance method FAO Penman-Monteith method Zhangye oasis Heihe river basin
ISSN号2073-4441
DOI10.3390/w9070499
通讯作者Gu, Lianglei(gull@lzb.ac.cn)
英文摘要Evapotranspiration (ET) is an important component of the surface energy balance and water cycle, especially in arid and semiarid regions. The characteristics of the actual evapotranspiration (ETa), which was calculated using the eddy covariance method, and the reference evapotranspiration (ET0), which was estimated using the Food and Agriculture Organisation (FAO) Penman-Monteith method, were analysed. This work focussed on the seasonal variations in evapotranspiration and crop coefficient (K-c) above the heterogeneous canopy of an arid oasis ecosystem in a cornfield of the Zhangye oasis in northwestern China. The results showed that in 2008, the total net radiation (R-n) was 2457.73 MJ.m(-2) and that the rainfall was 117 mm. The average wind velocity, air temperature, and specific humidity, which were observed 2 m above the ground surface, were 1.23 m.s(-1), 7.07 degrees C, and 3.66 g.kg(-1), respectively. The total ETa and ET0 were 654.69 mm and 1039.92 mm, respectively; thus, the ET0 was higher than the ETa. The difference between the ET0 and ETa was high in summer and autumn, and low in winter and spring. The ETa was greatly influenced by irrigation events, whereas the ET0 was not influenced by irrigation. The ETa and ET0 were both greatly influenced by meteorological elements. The K-c values were less than 0.5 outside of the maize-growing stage and greater than 0.5 during the entire maize-growing stage (from 20 April to 22 September 2008). The K-c values were 0.63, 0.75, 0.78, 0.76, 0.61 and 0.71 at the seedling, shooting, heading, filling, and maturity stages and the entire growth stage, respectively.
收录类别SCI
WOS关键词PENMAN-MONTEITH EQUATION ; HEIHE RIVER-BASIN ; ENERGY-BALANCE ; CROP COEFFICIENT ; TIBETAN PLATEAU ; SPRING WHEAT ; EVAPO-TRANSPIRATION ; WATER-USE ; CLIMATE ; MAIZE
WOS研究方向Water Resources
WOS类目Water Resources
语种英语
WOS记录号WOS:000406681700050
出版者MDPI AG
URI标识http://www.irgrid.ac.cn/handle/1471x/2557676
专题寒区旱区环境与工程研究所
通讯作者Gu, Lianglei
作者单位1.Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, Nagqu Stn Plateau Climate & Environm NPCE, Key Lab Land Surface Proc & Climate Change Cold &, Lanzhou 730000, Gansu, Peoples R China
2.Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, SKLCS, Cryosphere Res Stn Qinghai Xizang Plateau CRS, Lanzhou 730000, Gansu, Peoples R China
推荐引用方式
GB/T 7714
Gu, Lianglei,Hu, Zeyong,Yao, Jimin,et al. Actual and Reference Evapotranspiration in a Cornfield in the Zhangye Oasis, Northwestern China[J]. WATER,2017,9(7):16.
APA Gu, Lianglei,Hu, Zeyong,Yao, Jimin,&Sun, Genhou.(2017).Actual and Reference Evapotranspiration in a Cornfield in the Zhangye Oasis, Northwestern China.WATER,9(7),16.
MLA Gu, Lianglei,et al."Actual and Reference Evapotranspiration in a Cornfield in the Zhangye Oasis, Northwestern China".WATER 9.7(2017):16.

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来源:寒区旱区环境与工程研究所

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