Variations of crop coefficient and its influencing factors in an arid advective cropland of northwest China. Issue 2 (30th January 2014)

• Record Type: Journal Article
• Authors: Ding, Risheng; Tong, Ling; Li, Fusheng; Zhang, Yanqun; Hao, Xinmei; Kang, Shaozhong
• Is Part Of: Hydrological processes. Volume 29:Issue 2(2015:Jan.)
• Page Start: 239
• Page End: 249
• Publication Date: 2014-01-30
• Subjects: Hydrology -- Periodicals; Hydrology -- Research -- Periodicals; Hydrologic models -- Periodicals; Hydrological forecasting -- Periodicals; 631.432
• DOI: 10.1002/hyp.10146
• Languages: English
• ISSNs: 0885-6087

Abstract

<abstract abstract-type="main"> <title>Abstract</title> <p>Understanding the variation and magnitude of crop coefficient (<italic>K<sub>c</sub></italic>) is important for accurate determination of crop evapotranspiration and water use. In this study, we calculated <italic>K<sub>c</sub></italic> in an irrigated maize field with ground mulching by eddy covariance evapotranspiration measurements during the whole growing periods in 2009 and 2010 in an arid region of northwest China. A semi‐empirical practical approach for estimating <italic>K<sub>c</sub></italic> was proposed by introducing the dynamic fraction of canopy cover and incorporating the effect of leaf senescence as a function of days after sowing. The contribution of arid advection of sensible heat resulting from irrigation to <italic>K<sub>c</sub></italic> and the response of <italic>K<sub>c</sub></italic> to canopy conductance (<italic>G<sub>c</sub></italic>) were investigated. The averaged values of daily <italic>K<sub>c</sub></italic> were lower than typical values obtained previously without mulching due to decreasing effect of mulching on <italic>K<sub>c</sub></italic>, with 0.82 and 0.80 for the 2 years, respectively. The maximum average <italic>K<sub>c</sub></italic> occurred at the heading stage, with 1.21 and 1.04 for the 2 years, respectively. The difference of <italic>K<sub>c</sub></italic> was attributed to the difference of leaf area index. The semi‐empirical practical approach could well estimate the variations of <italic>K<sub>c</sub></italic>, thus could be a robust and useful tool for the practical users and water managers. The contributions to daily <italic>K<sub>c</sub></italic> from the arid advection were 4.4–28.0% of the measured <italic>K<sub>c</sub></italic>. The <italic>G<sub>c</sub></italic> had stronger control on daily <italic>K<sub>c</sub></italic> at the early and later stages than at the middle stage. When <italic>G<sub>c</sub></italic>, leaf area index and relative soil extractable water were lower than the respective threshold values of 20 mm s<sup>−1</sup>, 3.0 m<sup>2</sup> m<sup>−2</sup> and 0.5, the daily <italic>K<sub>c</sub></italic> increased significantly with the increase of the three factors, and almost remained constant when the three factors were beyond the threshold values. These results are helpful for quantifying contributions of individual factors to <italic>K<sub>c</sub></italic>, and subsequently improving water management practices according to <italic>K<sub>c</sub></italic>. Copyright © 2014 John Wiley & Sons, Ltd.</p> </abstract>