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首页> 外文期刊>Journal of Hydrology >Application of three canopy interception models to a young stand of Japanese cypress and interpretation in terms of interception mechanism
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Application of three canopy interception models to a young stand of Japanese cypress and interpretation in terms of interception mechanism

机译:三种林冠截留模型在日本柏幼林中的应用及截留机理的解释

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Three canopy interception models were applied to a stand of young Japanese cypress to obtain a better understanding of the dependence of canopy interception on rainfall intensity (DOCIORI) and the mechanism of splash droplet evaporation (SDE). The applied models were the heat budget model, the newly proposed DOCIORI model, and the revised Gash model. The heat budget model underestimated observed interception by 62.9% in 1999 and 63.4% in 2000; these amounts could be regarded as approximately equal to the amount of SIDE. Canopy interception comprises SDE and evaporation from the canopy surface, but the heat budget model calculates evaporation only from the canopy surface. Estimates derived from both the DOCIORI model and the revised Gash model are consistent with observed interception; these models are mathematically equivalent. Reanalysis of previously published data yielded DOCIORI values for interception sites in Spain, Puerto Rico, and the USA. In addition, the relation between mean rainfall intensity and mean evaporation rate calculated using the original and revised Gash models was examined using combined data from the present study and previously published studies; a positive correlation was found between the two values especially in the areas where the rainfall intensity is high. These results support the proposal that DOCIORI and SDE are universal phenomena especially in the high rainfall intensity areas. As literature data indicate that mean evaporation rate is independent of tree height and leaf area index, it can be concluded that canopy interception is mainly governed by rainfall regime rather than forest architecture in the high rainfall intensity areas. (C) 2007 Elsevier B.V. All rights reserved.
机译:三种冠层截留模型被应用到了一个年轻的日本柏树上,以更好地了解冠层截留对降雨强度的依赖性(DOCIORI)和飞溅液滴蒸发的机理(SDE)。应用的模型是热预算模型,新提出的DOCIORI模型和修订的Gash模型。热预算模型低估了1999年和2000年62.9%和63.4%的拦截率。这些数量可以视为大约等于SIDE的数量。冠层截留包括SDE和来自冠层表面的蒸发,但是热量收支模型仅计算来自冠层表面的蒸发。从DOCIORI模型和修正的Gash模型得出的估计值与观察到的拦截一致;这些模型在数学上是等效的。重新分析以前发布的数据得出西班牙,波多黎各和美国的拦截点的DOCIORI值。此外,使用本研究和先前发表的研究的综合数据,检查了使用原始和修正的Gash模型计算的平均降雨强度与平均蒸发率之间的关系。在这两个值之间发现正相关,特别是在降雨强度较高​​的地区。这些结果支持了DOCIORI和SDE是普遍现象的建议,尤其是在高降雨强度地区。文献资料表明,平均蒸发速率与树高和叶面积指数无关,因此可以得出结论,在高降雨强度地区,林冠截留主要由降雨体制决定,而不是森林结构。 (C)2007 Elsevier B.V.保留所有权利。

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