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首页> 外文期刊>Journal of Geophysical Research. Biogeosciences >Modeling actual evapotranspiration with routine meteorological variables in the data-scarce region of the Tibetan Plateau: Comparisons and implications
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Modeling actual evapotranspiration with routine meteorological variables in the data-scarce region of the Tibetan Plateau: Comparisons and implications

机译:青藏高原数据稀少地区的常规蒸发量与常规气象变量的模拟:比较与启示

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Quantitative estimation of actual evapotranspiration (ET_a) by in situ measurements and mathematical modeling is a fundamental task for physical understanding of ET_a as well as the feedback mechanisms between land and the ambient atmosphere. However, the ET_a information in the Tibetan Plateau (TP) has been greatly impeded by the extremely sparse ground observation network in the region. Approaches for estimating ET_a solely from routine meteorological variables are therefore important for investigating spatiotemporal variations of ET_a in the data-scarce region of the TP. Motivated by this need, the complementary relationship (CR) and Penman-Monteith approaches were evaluated against in situ measurements of ET_a on a daily basis in an alpine steppe region of the TP. The former includes the Nonlinear Complementary Relationship (Nonlinear-CR) as well as the Complementary Relationship Areal Evapotranspiration (CRAE) models, while the latter involves the Katerji-Perrier and the Todorovic models. Results indicate that the Nonlinear-CR, CRAE, and Katerji-Perrier models are all capable of efficiently simulating daily ET_a, provided their parameter values were appropriately calibrated. The Katerji-Perrier model performed best since its site-specific parameters take the soil water status into account. The Nonlinear-CR model also performed well with the advantage of not requiring the user to choose between a symmetric and asymmetric CR. The CRAE model, even with a relatively low Nash-Sutcliffe efficiency (NSE) value, is also an acceptable approach in this data-scarce region as it does not need information ofwind speed and ground surface conditions. In contrast, application of the Todorovicmodel was found to be inappropriate in the dry regions of the TP due to its significant overestimation of ET_a as it neglects the effect of water stress on the bulk surface resistance. Sensitivity analysis of the parameter values demonstrated the relative importance of each parameter in the correspondingmodel. Overall, the Nonlinear-CR model is recommended in the absence of measured ET_a for local calibration of the model parameter values.
机译:通过现场测量和数学建模对实际蒸散量(ET_a)进行定量估计是对ET_a以及陆地与周围大气之间反馈机制进行物理理解的一项基本任务。但是,该地区极为稀疏的地面观测网络极大地阻碍了青藏高原(TP)的ET_a信息。因此,仅根据常规气象变量估算ET_a的方法对于调查TP数据稀少区域中ET_a的时空变化非常重要。出于这种需求,每天在TP的高山草原地区,针对ET_a的原位测量结果评估了互补关系(CR)和Penman-Monteith方法。前者包括非线性互补关系(Nonlinear-CR)以及地域蒸散量(CRAE)模型,而后者涉及Katerji-Perrier模型和Todorovic模型。结果表明,只要适当地校准了它们的参数值,Nonlinear-CR,CRAE和Katerji-Perrier模型都能够有效地模拟每日ET_a。 Katerji-Perrier模型表现最佳,因为其特定于地点的参数考虑了土壤水分状况。非线性CR模型也表现良好,其优点是不需要用户在对称CR和非对称CR之间进行选择。即使具有相对较低的纳什-苏特克利夫效率(NSE)值,CRAE模型在此数据稀缺的区域也是一种可接受的方法,因为它不需要风速和地面状况的信息。相比之下,发现Todorovicmodel在TP的干燥区域是不合适的,因为它明显地高估了ET_a,因为它忽略了水分胁迫对整体表面电阻的影响。参数值的敏感性分析表明了相应模型中每个参数的相对重要性。总体而言,建议在没有测得的ET_a的情况下使用非线性CR模型进行模型参数值的本地校准。

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