降雨

Surveying several processes of rainfall, using the automatic hydrocone type ombrometer, analyzing the rainfall character in Dalian, drawing the frequency curve, especially, analyzing the time character of the storm, finding the time character of the storm, moreover, and the rainfall pattern is concerned.

利用安置在大连理工大学校园内的虹吸式自计雨量计，监测了数十场降雨过程，分析了大连市降雨的特点，计算并绘制出频率曲线，尤其对造成危害性较强的暴雨进行了时间特性的分析，结果得出了大连市暴雨的年、月、日以及短历时的时间特性，同时对雨型特点也进行了初步的分析。

Results show that the effective rainfall in Taiwan was more than 80% of the mean annual rainfall. The distribution types of the maximum 30-minute rainfall intensity (I30) in southwest and northeast area were leptokurtosis and platykurtosis respectivily, and there was a good relationship between I30 and mean rainfall intensity.

研究结果显示，台湾地区之有效雨量占年平均雨量之80%以上，其最大三十分钟降雨强度(I30)之分布型态，西南部属低阔峰分布，东北部则属於高狭峰的分布型态，且I30与平均降雨强度有较佳的相关性。

Normally, EI30 values are calculated from breakpoint rainfall information taken from continuous recording rain gauge charts, however, in many places in China the detailed chart-recorded rain gauge data relative to storm intensities are not readily available.

降雨侵蚀力是进行土壤流失量预报的基本因子，EI30是迄今得到广泛应用的定量指标，但它的计算需要降雨过程资料，使其推广应用受到很大限制。

The main reasons for the larger precipitation in Legates climatology are the rainband in the east of Taiwan during winter and the convective rainfall center over the southern Taiwan and Bashi Channel during summer.

Legates 的降雨气候较高的原因，主要是冬季在台湾东侧沿海有相当明显的雨带，以及夏季在巴士海峡与台湾南部的对流性降雨中心。

This is determined by the seasonal distribution of rainfall. Also serious erosion is brought by frequent farming activities.

这是由区域降雨季节分布特征所决定的，另外，这一时期的农事活动比较频繁，较高的降雨和农事活动相遇导致较大的侵蚀。

There were postive influence of temperture and rain on stress . The lower temperature, the lower feeling of stess. When it rained, the feeling of stress rase.

一、天气因子中以温度以及降雨与否对於三项压力均有显著影响，其中温度越低对於压力的感受越高，当降雨产生时对於压力的感受也越高，而雨量多寡仅对心理压力有正面显著影响。

An experimental embankment was constructed in Rouen,France,to study the embankment behavior under climatic effects.

路堤非饱和填土含水量的变化主要受大气降雨和蒸发影响，降雨造成了含水量的增加，而蒸发则起到了相反的作用。

This paper introduces the characteristics of this kind of landslide movement and investigates the influence of intense rainfall on the activities of crystalline schist landslide by examining rainfall and displacement of four typical landslides.

文章基于对此类滑坡活动观测资料和降雨资料的综合分析，阐述了结晶片岩滑坡的活动特点以及集中降雨对其的影响作用。

It shows that runoff is closely correlated with the features of individual precipitation, and it is also affected by vegetation within a short period of time. Raindrop erosion, sheet flow erosion and rill erosion on the slope are the main soil erosion patterns; sediment yield occurs mainly in flood season. Human activity and individual precipitation are two important factors that control the soil erosion at a small watershed. Comprehensive management on the slope in a small watershed is an efficient measure of water and soil conservation.

分析表明，小流域的产流方式容易随次降雨条件的变化而变化，植被因素在较小时间尺度内就会影响产流；产沙主要来源于坡面上的溅蚀、片蚀和细沟侵蚀，时间主要集中在汛期；人类活动以及次降雨条件是控制小流域侵蚀产沙的重要因素；在小流域内进行坡面的综合治理是水土保持的有效措施。

In the paper, we mostly studied the change of soil erosion process by a new REE tracer method, based on the theories of hydraulic mechanical subject and radionuclear tracer method, and simulated rainfall was applied to study the sheet erosion changing to rill erosion and the rill erosion process on slope land. The new REE tracer method should be useful to future studying of erosion processes on slope lands.1. Offering and testifying a new REE displacing method to study on the soil erosion of the loess slope.

本文以黄土坡面土壤侵蚀形态演变规律为研究重点，以新的核素示踪技术为手段，采用水动力学与核素示踪技术相结合、室内人工模拟降雨与稳定性REE元素示踪相结合的方法，利用先进的INAA技术，定量研究了不同雨强次降雨条件下细沟间侵蚀向细沟侵蚀的转变过程、细沟发生发育过程，为深入了解坡面侵蚀过程，建立黄土高原土壤侵蚀预报模型提供了研究基础。

The split between the two groups can hardly be papered over.

这两个团体间的分歧难以掩饰。

This approach not only encourages a greater number of responses, but minimizes the likelihood of stale groupthink.

这种做法不仅鼓励了更多的反应，而且减少跟风的可能性。