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Use of multiple correspondence analysis (MCA) to identify interactive meteorological conditions affecting relative throughfall

机译:使用多重对应分析(MCA)来确定影响相对穿透的交互式气象条件

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Forest canopies alter rainfall reaching the surface by redistributing it as throughfall. Throughfall supplies water and nutrients to a variety of ecohydrological components (soil microbial communities, stream water discharge/chemistry, and stormflow pathways) and is controlled by canopy structural interactions with meteorological conditions across temporal scales. This work introduces and applies multiple correspondence analyses (MCAs) to a range of meteorological thresholds (median intensity, median absolute deviation (MAD) of intensity, median wind-driven droplet inclination angle, and MAD of wind speed) for an example throughfall problem: identification of interacting storm conditions corresponding to temporal concentration in relative throughfall beyond the median observation (>= 73% of rain). MCA results from the example show that equalling or exceeding rain intensity thresholds (median and MAD) corresponded with temporal concentration of relative throughfall across all storms. Under these intensity conditions, two wind mechanisms produced significant correspondences: (1) high, steady wind-driven droplet inclination angles increased surface wetting; and (2) sporadic winds shook entrained droplets from surfaces. A discussion is provided showing that these example MCA findings agree well with previous work relying on more historically common methods (e.g., multiple regression and analytical models). Meteorological threshold correspondences to temporal concentration of relative throughfall at our site may be a function of heavy Tillandsia usneoides coverage. Applications of MCA within other forests may provide useful insights to how temporal throughfall dynamics are affected for drainage pathways dependent on different structures (leaves, twigs, branches, etc.). (C) 2015 Elsevier B.V. All rights reserved.
机译:森林冠层通过将降雨重新分配为穿透降雨来改变降雨。穿透降雨为各种生态水文学成分(土壤微生物群落,溪流水排放/化学物质和暴雨径流)提供水和养分,并通过冠层结构与时间尺度上气象条件的相互作用来控制。这项工作为一系列通气问题引入了多重对应分析(MCA)并将其应用于一系列气象阈值(中值强度,中值强度的绝对绝对偏差(MAD),中风驱动的液滴倾斜角度和风速的MAD):识别与中值观测值(> = 73%的降雨)以外的相对穿透中的时间集中相对应的相互作用风暴条件。该示例的MCA结果表明,等于或超过降雨强度阈值(中值和MAD)与所有风暴中相对穿透的时间集中性相对应。在这些强度条件下,两种风机制产生了明显的对应关系:(1)高,稳定的风驱动液滴倾斜角增加了表面润湿性; (2)零星的风从表面震动了夹带的水滴。提供的讨论表明,这些示例MCA发现与依靠历史上更常见的方法(例如,多元回归和分析模型)的先前工作非常吻合。气象阈值对应于我们站点相对穿透的时间集中度,可能是铁兰铁线莲覆盖率高的函数。 MCA在其他森林中的应用可能会提供有用的见解,以了解如何影响依赖于不同结构(叶子,树枝,树枝等)的排水路径的时空下降动态。 (C)2015 Elsevier B.V.保留所有权利。

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