汛期平水期,normal water period of flood season
1)normal water period of flood season汛期平水期
1.The paper analyzes the characteristics of sediment and discharge and its influence to channel scour and fill regulation innormal water period of flood season of the lower Yellow River.对黄河下游汛期平水期的水沙特点及其对河槽冲淤调整的影响进行了分析,结果表明:汛期平水期进入黄河下游河道的平均含沙量小于15 kg/m3、水沙搭配系数小于0。
英文短句/例句
1.Analysis on Channel Scour and Fill Regulation in Normal Water Period of Flood Season of the Lower Yellow River黄河下游汛期平水期河槽冲淤调整分析
2.Flood Season Division and Reansonable-Determination of Limited Water Level of Cascade Resevoirs;梯级水库汛期分期及汛限水位合理确定研究
3.Fuzzy Division of Flood Season and the Determination of Its Flood Control Water Level of Reservoir水库汛期模糊划分及其分期汛限水位的确定
4.Fuzzy Partition of Flood Season and Determination of Limited Water Level on Zhangze Reservoir;漳泽水库汛期模糊划分及汛限水位的确定
5.Decision-making on reservoir flood control level and its control manner in post-flooding seasons for Biliuhe Reservoir碧流河水库后汛期汛限水位及控制运用方式
6.The Application of Staged Limited Level of Reservoir during Flood Season and Seasonal Flood Periods Classification in the Dongfeng Reservoir;水库汛期分期及汛限水位调整在东风水库中的应用
7.ANALYSIS OF THE MECHANISM OF PACIFIC SSTA INFLUENCING EXTREME RAINFALL PRECIPITATION EVENTS IN ANNUALLY FIRST RAINING SEASON IN GUANGDONG太平洋SSTA对广东前汛期极端降水事件影响的机制分析
8.Risk and Benefit Analysis to Stage Flood Season Limited Water Level of Reservoir;水库分期汛限水位的风险与效益分析
9.It might be a useful index for rainfall forecast in China.这是每年汛期降水预报的一个指标.
10.Typhoon Activity Effect on Precipitation over North China During Flood Season;台风活动对华北汛期降水影响的研究
11.Precipitation Test by WRF Model in Jiaozuo Flood Season in WRF模式对焦作汛期降水的检验
12.Water Vapor Analysis of Heavy Rain Events in Guangxi in July 7月广西汛期暴雨过程水汽特征
13.Changes of Flood-Season Severe Precipitation over South China in 2071-210021世纪末华南汛期强降水变化分析
14.Period and Trend Analysis of Runoff and Sediment Transport at Tongguan Station along the Middle Yellow River in Flood Season黄河潼关汛期水沙变化周期及其趋势分析
15.Research of Hydrodynamic and Water Quality Simulation in Three Gorges Reservoir at Non-flood Season;三峡水库非汛期水动力及水质模拟研究
16.The river water chilled me to the bone; the snowmelt of the flood season was throwing up great waves.河水冷得刺骨，汛期的雪水在河里掀着大浪。
17.Research on Water Quality Objective Combined Optimal Dispatching of Three Gorges Reservoir in Non-flood Season耦合水质目标的三峡水库非汛期优化调度研究
18.Study on Stage Flood Control Water Level of Danjiangkou Reservoir丹江口水库汛限水位分期控制初步探讨
相关短句/例句
floods season precipitation汛期降水
1.The results showed that there is a high correlation betweenfloods season precipitation in Zhejiang and SSTA.根据1951年1月～1999年12月浙江省23站汛期降水的资料,寻求海温因子对浙江省汛期降水的影响,结果表明:热带海洋海温异常与浙江省汛期降水异常有较好的对应关系。
2.In the study of the mechanism of the precipitation anomalies, the discovery is then chiefly to study the effect of SSTA on rainfall in floods season in TPNES, concluding that there is a high correlation between thefloods season precipitation in.本文在对中国西北地区降水气候特征及其与北方气旋相关关系的分析基础之上，重点对青藏高原东北侧汛期降水异常以及其同期和前期的影响因子进行了分析研究，并侧重寻求前期SSTA对青藏高原东北侧降水的影响，结果发现澳大利亚东侧SSTA及分布型与高原东北侧汛期降水异常有较好的对应关系。
3)diverting water in flood season调汛期水
4)rainy season precipitation汛期降水
1.(2) The general interdecadal variations period of therainy season precipitation is 20-25a in the past 58 years.结果表明:近58a来柳州市汛期降水主要呈波动性变化,线性趋势变化不明显,但前汛期降水总体呈上升趋势,降水量约增加87mm;后汛期降水量总体呈下降趋势,约减少了89mm。
5)flood period (duaration)汛期;洪水期
6)precipitation amount in flood period汛期降水量
延伸阅读
华南前汛期暴雨华南前汛期暴雨rainstorm during pre-rainy season in South Chinahua’nan qianxunqi baoyu华南前汛期暴雨(rainstorm during Pre-rainy season in South China)每年4一6月发生在中国南岭以南地区(包括广东、广西和福建三省、区)的暴雨。华南地处亚热带，受夏季风影响较中国其他地区为早，3月末至4月初即进入汛期，4月至9月为暴雨季节，其中4一6月称为前汛期，这时产生暴雨主要为锋面、低空急流、切变线、低涡等温带天气系统;7一9月为后汛期，·暴雨主要由台风和东风波等热带天气系统所造成;华南前汛期多年平均暴雨日数可达4天以上，以5月最多，6月次之、4月最少。特大暴雨几乎都出现在5月和6月。暴雨中心与年雨量的多雨中心一致。在广西暴雨中心位于桂林附近的桂北地区，在广东省有3个暴雨中心;第一个在云开大山的迎风坡恩平、阳红附近;第二个在九连山的迎风坡清远、佛岗和龙门一带;第三个在粤东沿海和莲花山迎风坡一侧的潮汕平原一带。在福建暴雨中心位于闽北武夷山区。暴雨中心区，暴雨量约占全年降雨量的三分之一。前汛期暴雨过程短的不足1天。长的可达5一7天。华南地区降雨强度一般比内陆地区大得多，24小时暴雨量达100一200毫米比较常见，特大暴雨可达800毫米以上，暴雨过程总量可达1000毫米以上，前汛期暴雨是一次次冷暖空气交绥的结果。当东亚大气环流由冬季形势向夏季形势调整时，西太平洋副热带高压逐渐加强，西南和东南暖湿气流进入华南地区;由北方南下的冷锋移至华南趋于准静止状态，形成华南静止锋。高空西风槽在华南形成切变线，在锋后槽(切变线)前容易形成暴雨。地形作用促使华南前汛期暴雨中心多半集中于山脉的迎风坡。 (黄忠怒)
