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This might explain why India's winter rains were poor this year; but May delivered a drenching.

这可能解释了为什么印度今年冬天雨量少而五月雨量多的原因。

The study probe into at when extreme rainfall happenning incident research purpose department on city, estimate its flow of flood crest to defend and provide disaster relief the reference carried on the exercise of in follow-up ; While estimating the the depth of extreme rainfall , use separately: World Meteological Organization statistic method, storm transposition and dew point adjustment method and average recurrence interval rainfall depth factor method, inquire into and act as river valley wutu the upper reaches of Keelung and collect in the water area separately, wutu station with flood-diversion stands in the Huo-Shao-Liao station before Yuan-Shan-Tzu flood-diversion, the depth when the extreme rainfall happens separately, step forward and mix the set of design hyetograph by extreme rainfall ,finally,mix geomorphologic instantaneous unit hydrograph afterwards, in order to estimate the flow of flood crest produced cause by extreme rainfall incident .

本文之研究目的系探讨当极端暴雨事件发生於都会区时,推估其洪峰流量以作为后续防救灾演练之参考。在推估极端暴雨之降雨深度时,分别采用:世界气象组织统计法、暴雨移置与露点调整法及平均重现期距雨量因子法,分别推求当基隆河流域五堵上游集水区,员山子分洪前之火烧寮站与分洪后之五堵站,分别发生极端暴雨时之雨量,进一步将极端暴雨量套配设计雨型,最后再搭配地貌型瞬时单位历线模式,以推估因发生极端暴雨事件而产生之洪峰流量。

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。

In this paper, the Kriging method is used for optimal estimation of the point and areal precipitation.

本文应用克里格法对点雨量和面雨量进行了最优估计。

Enjoy monitoring your rainfall with this Cast Iron Bird Rain Gauge.

享受监测与此铸铁鸟雨量计的雨量

Using a neural network algorithm to establish a typhoon rainfall model and to seek the nonlinear relations between the relevant parameters and rainfall intensity is a rational approach. The rainfall data used in this study include rain gauge data and radar data, and is able to reflect the spatial distribution of the precipitation pattern.

雷达具有空间侦测能力,利用地面雨量计的雨量资料与雷达回波的资料,可以将空间中的降雨分布趋势表示出来;本研究当中所决定的台风降雨因子是根据过去相关研究文献所整理出来,而这些台风降雨因子是否能完全模拟台风降雨的机制,尚待观察。

Radar rainfall estimation combined with a few rain gauges has as good result as dense rain gauge network does in runoff simulation that gives a good prospect of radar application in flood monitoring and forecasting.

2雷达联合少量雨量计估测降水用于流域径流模拟时,模拟精度和用稠密雨量计网模拟的精度接近,显示雷达在流域径流模拟和洪水监测预报中有相当高的应用价值。

In order to investigate the excitation mechanism and response characteristics of wind-rain induced vibration of stay cable,an instrumentation system of wind-rain induced vibration measurement,which consists of anemometer,rain gauge and accelerometer,was installed on the Dongting Lake Bridge,Yueyang,China.

为了研究斜拉桥拉索风雨振的机理及响应特征,在岳阳洞庭湖大桥建立了由风速仪、雨量计、加速度传感器组成的风雨振现场观测系统,观测到了多次拉索风雨振现象;得到了发生拉索风雨振时风速、风向及雨量的基本条件,分析了风雨振时拉索振动的幅值、主振频率、模态参与特性及空气动力负阻尼比等响应特征。

The rainstorm process is a complex and stochastic multi-dimensional process.A correlation exists between the maximal annual period-storm and the rainfall duration,with overlooking many factors,the parameterwill not be a constant.Since 1980s,heavy rain and flood of small basins can be calculated by auto-recording rainfall observation system,and 20-year's self-recording rainfall data can improve the calculation accuraey.

暴雨过程是一个复杂的多维随机过程,年最大时段暴雨xt,p与暴雨历时t的暴雨公式属于经验相关关系,忽略了不少影响因素,因此,公式中参数n值不会是稳定不变的。20世纪80年代以后,随着自记雨量观测应用,到目前已经有20多年的资料系列,小流域暴雨设计的计算就可以直接利用时段实测降水资料系列进行计算,设计洪水时,可根据实测雨量时段资料,计算该设计流域的n值,可提高计算精度。

The theme is WET and Donal takes a ride with the rains from the wettest place in Europe, the little known Norwegian town of Bergen where it rains 265 days of the year, and onto the wettest place in the world - India, where 25 billion tons of water falls each day during the monsoon period.

摄制队走到多个下雨量称王的地方,包括挪威西南部港市卑尔根和印度,前者一年365日中有265日都是雨天,后者在雨季期间,每天的下雨量高达250亿公吨。

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