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首页> 外文期刊>Hydrology and Earth System Sciences >Combined measurement and modeling of the hydrological impact of hydraulic redistribution using CLM4.5 at eight AmeriFlux sites
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Combined measurement and modeling of the hydrological impact of hydraulic redistribution using CLM4.5 at eight AmeriFlux sites

机译:使用CLM4.5在八个AmeriFlux站点对水力重新分配的水文影响进行联合测量和建模

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Effects of hydraulic redistribution (HR) on hydrological, biogeochemical, and ecological processes have been demonstrated in the field, but the current generation of standard earth system models does not include a representation of HR. Though recent studies have examined the effect of incorporating HR into land surface models, few (if any) have done cross-site comparisons for contrasting climate regimes and multiple vegetation types via the integration of measurement and modeling. Here, we incorporated the HR scheme of Ryel et al.?(2002) into the NCAR Community Land Model Version 4.5 (CLM4.5), and examined the ability of the resulting hybrid model to capture the magnitude of HR flux and/or soil moisture dynamics from which HR can be directly inferred, to assess the impact of HR on land surface water and energy budgets, and to explore how the impact may depend on climate regimes and vegetation conditions. Eight AmeriFlux sites with contrasting climate regimes and multiple vegetation types were studied, including the Wind River Crane site in Washington State, the Santa Rita Mesquite savanna site in southern Arizona, and six sites along the Southern California Climate Gradient. HR flux, evapotranspiration (ET), and soil moisture were properly simulated in the present study, even in the face of various uncertainties. Our cross-ecosystem comparison showed that the timing, magnitude, and direction (upward or downward) of HR vary across ecosystems, and incorporation of HR into CLM4.5 improved the model-measurement matches of evapotranspiration, Bowen ratio, and soil moisture particularly during dry seasons. Our results also reveal that HR has important hydrological impact in ecosystems that have a pronounced dry season but are not overall so dry that sparse vegetation and very low soil moisture limit HR.
机译:水力再分配(HR)对水文,生物地球化学和生态过程的影响已在该领域得到证明,但是当前的标准地球系统模型尚不包括HR的表示。尽管最近的研究已经检查了将HR纳入陆地表面模型的效果,但很少(如果有的话)通过测量和建模的集成进行跨站点比较,以对比气候状况和多种植被类型。在这里,我们将Ryel等人(2002)的HR方案纳入NCAR社区土地模型版本4.5(CLM4.5),并研究了所得混合模型捕获HR通量和/或土壤量的能力。可以从中直接推断出HR的水分动态,以评估HR对土地地表水和能源预算的影响,并探讨影响如何取决于气候状况和植被状况。研究了八个气候条件不同且植被类型多种多样的AmeriFlux站点,包括华盛顿州的Wind River Crane站点,亚利桑那州南部的Santa Rita Mesquite稀树草原站点和南加州气候梯度的六个站点。即使在面对各种不确定性的情况下,本研究也对HR通量,蒸散量(ET)和土壤湿度进行了正确模拟。我们的跨生态系统比较显示,HR的时间,大小和方向(在向上或向下)在整个生态系统中都不同,并且将HR纳入CLM4.5可以改善蒸散量,Bowen比和土壤水分的模型测量匹配,特别是在干燥的季节。我们的研究结果还表明,HR对干旱季节明显但总体上不那么干燥以至于植被稀疏和土壤湿度极低的生态系统具有重要的水文影响。

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