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CALIBRATION, REFINEMENT, AND APPLICATION OF THE WEPP MODEL FOR SIMULATING CLIMATIC IMPACT ON WHEAT PRODUCTION

机译:用于模拟气候对小麦生产的影响的WEPP模型的校准,完善和应用

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摘要

Agricultural system models are useful tools for tailoring agricultural production systems to possible climate variations. The objectives of this work were: (1) to evaluate and calibrate the water balance and crop components of the Water Erosion Prediction Project (WEPP) model and to make improvements if necessary, and (2) to simulate hydrologic and crop responses to generated climate scenarios for winter wheat (Triticum aestivum L.). Precipitation, surface runoff, soil moisture, and wheat biomass collected between 1980 and 1996 on a 1.6 ha watershed near El Reno, Oklahoma, were used. Two contrasting (wet and dry) climate scenarios were generated using a climate generator (CLIGEN) for assessing the overall sensitivity of WEPP to climate variations. Optimized saturated hydraulic conductivity (Ks) agreed well with field-measured K{sub}s, indicating that the infiltration routine of the model functioned properly. WEPP's original water use function substantially overpredicted plant water uptake and therefore was modified. The revised water use function resulted in better predictions of soil water balance, plant water stress, and biomass production. Predicted aboveground biomass agreed relatively well with measured data (model efficiency = 0.5). However, wheat grain yields were less well predicted because of inadequate adjustments to harvest index in the model. The general relationship between total aboveground biomass and growing-season evapotranspiration for winter wheat was reasonably simulated by the model. Model simulations under the generated wet and dry scenarios showed that each percent increase in growing-season precipitation would result in, on average, 3.38%, 0.34%, 0.73%, 1.09%, and 0.81% increases in surface runoff, plant transpiration, soil evaporation, deep percolation, and wheat grain yield, respectively, under the study conditions. This work has shown that WEPP is capable of simulating hydrologic and crop responses to climate variations.
机译:农业系统模型是使农业生产系统适应可能的气候变化的有用工具。这项工作的目标是:(1)评估和校准水蚀预测项目(WEPP)模型中的水平衡和作物成分,并在必要时进行改进,以及(2)模拟水文和作物对产生的气候的响应冬小麦(Triticum aestivum L.)的情景。使用了1980年至1996年之间在俄克拉荷马州埃尔雷诺附近1.6公顷流域收集的降水,地表径流,土壤湿度和小麦生物量。使用气候生成器(CLIGEN)生成了两种截然不同的(潮湿和干燥)气候情景,用于评估WEPP对气候变化的总体敏感性。优化的饱和导水率(Ks)与现场测得的K {sub} s非常吻合,表明该模型的渗透程序正常运行。 WEPP最初的用水功能大大高估了植物的吸水量,因此进行了修改。修改后的用水功能可以更好地预测土壤水分平衡,植物水分胁迫和生物量产量。预测的地上生物量与测得的数据相对吻合(模型效率= 0.5)。但是,由于模型中对收获指数的调整不足,因此无法预测小麦的单产。该模型合理地模拟了冬小麦地上总生物量与生长季蒸散量之间的一般关系。在产生的干湿情况下的模型模拟表明,生长季节降水量每增加百分之百,平均将导致地表径流,植物蒸腾作用,土壤增加3.38%,0.34%,0.73%,1.09%和0.81%。在研究条件下的蒸发,深度渗滤和小麦籽粒产量分别。这项工作表明,WEPP能够模拟水文和农作物对气候变化的响应。

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