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Feasibility analysis of using inverse modeling for estimating field-scale evapotranspiration in maize and soybean fields from soil water content monitoring networks

机译:利用逆模型从土壤含水量监测网络估算玉米和大豆田田间蒸散量的可行性分析

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In this study, the feasibility of using inverse vadose zone modeling for estimating field-scale actual evapotranspiration (ETsuba/sub) was explored at a long-term agricultural monitoring site in eastern Nebraska. Data from both point-scale soil water content (SWC) sensors and the area-average technique of cosmic-ray neutron probes were evaluated against independent ETsuba/sub estimates from a co-located eddy covariance tower. While this methodology has been successfully used for estimates of groundwater recharge, it was essential to assess the performance of other components of the water balance such as ETsuba/sub. In light of recent evaluations of land surface models (LSMs), independent estimates of hydrologic state variables and fluxes are critically needed benchmarks. The results here indicate reasonable estimates of daily and annual ETsuba/sub from the point sensors, but with highly varied soil hydraulic function parameterizations due to local soil texture variability. The results of multiple soil hydraulic parameterizations leading to equally good ETsuba/sub estimates is consistent with the hydrological principle of equifinality. While this study focused on one particular site, the framework can be easily applied to other SWC monitoring networks across the globe. The value-added products of groundwater recharge and ETsuba/sub flux from the SWC monitoring networks will provide additional and more robust benchmarks for the validation of LSM that continues to improve their forecast skill. In addition, the value-added products of groundwater recharge and ETsuba/sub often have more direct impacts on societal decision-making than SWC alone. Water flux impacts human decision-making from policies on the long-term management of groundwater resources (recharge), to yield forecasts (ETsuba/sub), and to optimal irrigation scheduling (ETsuba/sub). Illustrating the societal benefits of SWC monitoring is critical to insure the continued operation and expansion of these public datasets.
机译:在这项研究中,在内布拉斯加州东部的一个长期农业监测点,探讨了使用反渗流带模型估算田间规模实际蒸散量(ET a )的可行性。根据同位涡动协方差塔的独立ET a 估计,评估了点尺度土壤水分(SWC)传感器和宇宙射线中子探针的面积平均技术的数据。尽管此方法已成功用于估算地下水补给量,但评估水平衡的其他组成部分(如ET a )的性能至关重要。根据最近对陆地表面模型(LSM)的评估,迫切需要水文状态变量和流量的独立估计。这里的结果表明了从点传感器获得的每日和每年ET a 的合理估计,但是由于局部土壤质地的变化,土壤水力功能参数设置变化很大。多次土壤水力参数化的结果导致同样好的ET a 估计与等量性水文原理相一致。尽管此研究仅针对一个特定站点,但该框架可以轻松地应用于全球其他SWC监视网络。 SWC监测网络中的地下水补给和ET a 通量的增值产品将为LSM的验证提供更多且更可靠的基准,从而继续提高其预报技能。此外,地下水补给和ET a 的增值产品通常对社会决策的影响比单独对SWC的影响更大。水流量会影响人的决策,包括政策对地下水资源的长期管理(补给),产量预测(ET a )和最佳灌溉计划(ET a )。说明SWC监控的社会效益对于确保这些公共数据集的持续运行和扩展至关重要。

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