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Assessing raindrop impact energy at the forest floor in a mature Japanese cypress plantation using continuous raindrop-sizing instruments

机译:使用连续雨水尺寸仪器评估森林地板雨滴的雨滴冲击能量

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The raindrop size distribution of throughfall and open rainfall was monitored continuously during a rainfall event using laser raindrop-sizing instruments (LD gauges), in order to calculate the raindrop impact energy in a plantation of mature Japanese cypress (Chamaecyparis obtusa), where surface erosion at the forest floor had been a problem. Data from two rainfall events were analyzed. The LD gauges recorded qualitative raindrop size distribution, and the capture rate during each rainfall event was used to manipulate raindrop data quantitatively. Throughfall and open rainfall comparisons revealed several important differences. First, throughfall raindrops were fewer in number and larger in size than open rainfall drops. In one rainfall event, for example, throughfall raindrops were less than one-fifth as frequent as open rainfall raindrops; in addition, the maximum throughfall raindrop diameter was 6.35mm compared to 3.31mm for open rainfall raindrops. Second, throughfall raindrops that were larger than the largest open rainfall raindrops comprised 63.8% of the throughfall precipitation by volume. Third, total raindrop impact energy from throughfall was over twice that of open rainfall. Moreover, comparison of throughfall events implied that throughfall raindrops did not always have a uniform distribution between different events or among different periods of time in one rainfall event, in contrast to findings in previous studies which showed that throughfall raindrops had a uniform size distribution independent of rainfall intensity. It is possible that an abrupt transition of throughfall intensity from low to high changes the distribution of throughfall raindrops.
机译:在使用激光雨滴尺寸仪器(LD仪表)的降雨事件期间,在降雨事件期间连续监测雨水尺寸分布,以便计算成熟日本赛普拉斯(Chamaecyparis oblusa)的种植园中的雨滴冲击能量在森林楼层是一个问题。分析了两个降雨事件的数据。 LD仪表记录了定性雨滴尺寸分布,并且每次降雨事件期间的捕获率被用于定量操纵雨滴数据。通过降雨量和开放的降雨比较揭示了几个重要的差异。首先,缺水雨滴数量较少,大小比开放降雨量更大。例如,在一个降雨事件中,通过降雨雨滴频繁的缺水雨滴小于五分之一;此外,与3.31毫米的开放降雨雨滴相比,最大的通过降雨量为6.35mm。其次,大于最大的开放降雨雨滴的缺水雨滴包括63.8%的吞吐量沉淀。第三,通过降雨量的雨水从雨滴的总雨滴造成的两倍于露天降雨量。此外,缺乏事件的比较暗示,通过流量雨滴并不总是在一个降雨事件中不同的事件或不同时间段之间的均匀分布,与先前研究中的结果相比,这表明通过了云雨滴具有均匀的尺寸分布降雨强度。缺水强度从低到高改变溢流雨滴的分布也可能发生突然转变。

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