Maximum hourly rainfall intensity 40 ~ 80 mm.
最大小时降雨强度40毫米80毫米。
Slope erosion has a very closely relationship with rainfall intensity.
降雨强度与坡面侵蚀之间的关系十分密切。
The effect of a moderate rainfall intensity on soil moisture was significant.
中等雨强降雨对土壤水分影响最大;
The amounts of nutrient loss were in direct proportion to rainfall intensity.
养分流失量与雨强成正比;
The threshold values of critical rainfall and critical rainfall intensity are discussed.
在此基础上,探讨了区域性滑坡发生的临界降雨量和降雨强度阀值。
The rainfall intensity is relevant with raindrop size and quantity as well as rainfall density.
降雨强度与雨滴大小、数量及雨滴密度有关。
Roof runoff water quality was affected by rainfall, rainfall intensity, roof material, season and air temperature.
屋面径流水质主要受降雨量、降雨强度、屋面材料、季节和气温的影响。
The water flow volume and phosphorus concentration in both runoffs increased with the rainfall intensity improved;
降雨强度大,表面径流和壤中流始流时间早,水流量和浓度相应高,累积输出也多。
The increase of rainfall intensity is mainly due to appear larger particles, the average diameter increases and cause;
雨强的增大主要是由于出现较大粒子,平均直径增大而引起的;
Slope sediment yield is under the impact of rainfall intensity, the change rules are similar to the runoff dynamic changes.
坡面产沙同样受降雨强度的影响,其变化规律同坡面产流的规律类似。
Rainfall intensity and initial water content are important infiltration factor which influence rainfall infiltration content.
降雨强度和初始含水量是影响入渗量的主要因素。
With the same slope conditions, the greater the rainfall intensity , the larger the runoff and sand content of the runoff are;
坡度相同时,降雨强度越大,径流量和径流的径流的含沙率越大;
Rill width and depth become bigger with rainfall intensity, erosion amount promptly enhances after rill appears, accounts for 91%.
细沟的宽度和深度随雨强的增大而增大,产生细沟后侵蚀量将迅速增大,最大占总侵蚀量的91%。
When slope gradient and soil surface hydrological condition had not change, runoff increased with increasing of rainfall intensity.
同一坡度和近地表水文条件下,平均侵蚀率是随雨强的增大而增加。
Storm brings strong rainfall intensity in short duration, moreover, the shorter duration the average rainfall intensity is stronger.
暴雨在短历时内产生较强的降雨,而且暴雨的间隔时间尺度越短平均雨强就越大。
The mostly factor effecting of the soil erosion were hypo-rainfall, hypo-rainfall intensity, rainfall kinetic energy and rainfall erosivity.
影响坡面土壤侵蚀的主要因子有次降雨量、雨强、降雨动能和降雨侵蚀力。
The maximum change of mean rainfall intensity is over 10% due to CDSU and difference among experiments is more obvious in the daytime than at night.
云滴谱的不确定性能够引起最大超过10%的平均降水强度的改变,而且其差异在白天比夜间更明显。
However, the regulation functions to karst water depend on the structure of the epikarst zone, occurrence of strata, land cover and rainfall intensity.
表层岩溶带对岩溶水的调蓄功能大小主要与表层岩溶带的结构、岩层产状、地表覆盖情况和降雨性质有关。
Because of the differences of the roughness, the interflow, the soil moisture and the rainfall intensity, the pipe flow process shows different hydraulic graph.
由于土管内部粗糙程度和分枝合流情况不同,土壤前期降雨量、本次降雨强度影响也造成管流的水文过程产生差别。
The analysis of summer rainfall intensity in China is carried on for the purpose of practical application of climatic data to the natural resources development.
本文关于中国夏季日降水强度的分析,是以对国民经济服务为目的的。
Slope in certain Geological setting and in a certain Mechanical Environment requires a certain rainfall, rainfall intensity or duration to promote slope damage.
在一定地质背景和力学环境下的斜坡需要一定的降雨量、降雨强度或降雨持续时间才能促使斜坡破坏。
The cumulative quantity of runoff's nutrient increases correspondingly along with the more enhancing rainfall intensity and longer duration of runoff generation.
随着雨强的增大、产流时间的增加,径流养分累积量也相应增大。
This article deals with a distance weighing method through which the rainfall intensity and the area precipitation amount detected by weather radar are adjusted.
本文用距离加权方法校准天气雷达估算降水强度和区域降水量。
The rainfall Intensity Duration Frequency formula is one of the bases in hydrology calculation, and has been of considerable interest to engineers and hydrologists.
降雨公式是水文计算的基本依据之一,也是工程师和水文学家十分关心的问题。
Remote measurements of rainfall intensity and areal precipitation by using weather radar are a problem that meteorological scientists have researched with an effort.
利用天气雷达遥测降雨强度和区域降雨量的大小一直是人们努力探索的课题。
In autumn, the average rainfall intensity increased in most parts of Yunnan and Guizhou, but decreased in the eastern Sichuan Basin and the western Sichuan highland.
秋季平均雨强在云南和贵州大部分地区有增大趋势,而盆地东部和川西高原有减小趋势。
The extent of vertical erosion increases with precipitation, rainfall intensity and soil infiltration rates, and different soil has different critical rainfall amount.
垂直侵蚀随降雨强度、降雨历时的增加而增加,不同土壤的侵蚀临界降雨量不同;
The extent of vertical erosion increases with precipitation, rainfall intensity and soil infiltration rates, and different soil has different critical rainfall amount.
垂直侵蚀随降雨强度、降雨历时的增加而增加,不同土壤的侵蚀临界降雨量不同;
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