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首页> 外文期刊>Journal of Hydrology >Evaluation of seasonal evapotranspiration of winter wheat in humid region of East China using large-weighted lysimeter and three models
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Evaluation of seasonal evapotranspiration of winter wheat in humid region of East China using large-weighted lysimeter and three models

机译:基于大加权溶度计和3个模型的华东湿润区冬小麦季节蒸散量评价

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摘要

Water consumption demand of winter wheat remains uncertain in humid region of East China. A better prediction of water consumption can improve agricultural water management. Based on the evapotranspiration (ET) data determined by large-weighted lysimeter and the meteorological data during 2011-2018, the actual ET of winter wheat was compared with the ET simulated by Priestley-Taylor (PT), Penman-Monteith (PM) and FAO- 56 single crop coefficient (K_c) models, and the relationships between ET of winter wheat and its driving environmental factors were assessed to localize the model's parameters. The results showed that the seasonal variations of ET in winter wheat could be divided into three stages with the canopy development, i.e., Stage I: from sowing to wintering when hourly ET maintained a low level (0.03-0.35 mm/h); Stage II: from revival to dough when hourly ET increased rapidly to 0.60-1.50 mm/h during daytime; Stage III: the ripening stage with hourly ET decreasing to 0.01-1.00 mm/h. The ET of winter wheat was mainly determined by wind speed at Stage I and by net solar radiation (R_n) at Stage II and III by Besides primary determining factor net radiation at the whole season, vapor pressure deficit and air temperature was the second factor that dominated ET at Stages III and Stage III, respectively. The PM model performed excellently for hourly ET modelling at Stage II with R~2 of 0.944 during 2017-2018. All models did not perform well at Stage I and III on hourly time scale. PM model was the best among the three models for calculating daily ET at Stage II, while both PM and PT models could be used to simulate daily ET at Stage III. After local parameterization, the calibrated PT_x and K_(cx) models were validated with daily ET simulation with the coefficients of 1.52 and 1.25 at Stage I, 1.81 and 1.80 at Stage II, and 1.12 and 0.78 at Stage III, respectively. The PT_x model was suitable to calculate daily ET at Stage I and III with R~2 of 0.19 and 0.55, MAE of
机译:华东湿润地区冬小麦用水需求仍不明朗。更好地预测用水量可以改善农业用水管理。基于2011—2018年大加权溶血仪测定的蒸散量(ET)数据和气象资料,将冬小麦实际ET与Priestley-Taylor(PT)、Penman-Monteith(PM)和FAO-56单季作物系数(K_c)模型模拟的ET进行比较,评估冬小麦ET与其驱动环境因子的关系,对模型参数进行定位。结果表明:冬小麦ET的季节变化随冠层发育可分为3个阶段,即I.期:从播种到越冬,小时ET保持在较低水平(0.03-0.35 mm/h);第二阶段:从复活到面团,白天每小时ET迅速增加到0.60-1.50 mm/h;第三阶段:成熟期,每小时ET降至0.01-1.00 mm/h。冬小麦ET在I.期主要受风速影响,在II.期和III.期主要受太阳净辐射(R_n)的影响,除主要决定因素外,水汽压差和气温是主导III.期和III.期ET的第二因素。 分别。PM模型在2017—2018年第二阶段逐时ET建模中表现优异,R~2为0.944。所有模型在第一阶段和第三阶段的小时时间尺度上表现不佳。PM模型是计算II阶段每日ET的三个模型中最好的,而PM和PT模型都可用于模拟III阶段的每日ET。局部参数化后,通过每日ET模拟验证了校准后的PT_x和K_(cx)模型,第一阶段的系数分别为1.52和1.25,第二阶段的系数分别为1.81和1.80,第三阶段的系数分别为1.12和0.78。PT_x模型适用于计算I.期和III.期的日ET,R~2分别为0.19和0.55,MAE为

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  • 来源
    《Journal of Hydrology》 |2020年第2期|125388-1-125388-12|共12页
  • 作者单位

    Jiangsu Provincial Key Laboratory of Agricultural Meteorology, College of Applied Meteorology, International Center for Ecology, Meteorology and Environment, Nanjing University of Information Science and Technology, Nanjing 210044, China;

    State Key Laboratory of Hydraulics and Mountain River Engineering & College of Water Resource and Hydropower, Sichuan University, Chengdu, China;

    Key Laboratory of Agricultural Soil and Water Engineering in Arid and Semiarid Areas, Northwest A&F University, Yangling, ChinaDepartment of Civil Engineering, The University of Hong Kong, Pokfulam Road, Hong Kong, ChinaInstitute of Environment and Sustainable Development in Agriculture, Chinese Academy of Agricultural Sciences, Beijing, China;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 英语
  • 中图分类 水文科学(水界物理学);
  • 关键词

    Winter wheat; Evapotranspiration; Penman-Monteith; Priestley-Taylor; FAO-56 single crop coefficient model; Large-weighted lysimeter;

    机译:冬小麦;蒸散;彭曼-蒙特斯;普里斯特利-泰勒;FAO-56单季作物系数模型;大加权裂解仪;
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