单位线的英文

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"单位线"怎么读用"单位线"造句

英文翻译手机版

unit fiber
unit hydrograph
unit line

"单位"英文翻译 unit
"线"英文翻译 thread; string; wire
"单位线段" 英文翻译 : unit segment
"单位线法" 英文翻译 : unit hydrograph method
"河网单位线" 英文翻译 : river network unit hydrograph
"经验单位线" 英文翻译 : empiricat unit hydrograph
"坡地单位线" 英文翻译 : slope unit hydrograph
"瞬时单位线" 英文翻译 : instantaneous unit hydrograph
"综合单位线" 英文翻译 : synthetic unit hydrograph
"单位纤维,单位线" 英文翻译 : unit fiber
"单位线束扎绳" 英文翻译 : unit binder
"无因次单位线" 英文翻译 : dimensionless unit hydrograph
"单位线段, 单位程序段" 英文翻译 : unit segment
"地貌瞬时单位线" 英文翻译 : geomorphologic instantaneous unit hydrograph
"价格在10单位线下且" 英文翻译 : kdj
"位线" 英文翻译 : bit line; digit line
"变位线" 英文翻译 : flexure curve
"船位线" 英文翻译 : position line
"等位线" 英文翻译 : coordinatograph; e lines; equipotential line isopotential line; equipotential pitch; equivalent line; isoline; isopleth; line of equipotential; line, equipotential
"低位线" 英文翻译 : low watermark
"电位线" 英文翻译 : equipotential
"定位线" 英文翻译 : line of position; lop; orientation line; position line
"方位线" 英文翻译 : azimuth lines; bearing line; heading line; line of azimuth; line of bearing; loxodrome; orienting line; position line; rhumb line
"分位线" 英文翻译 : lane place line
"复位线" 英文翻译 : reset line

例句与用法

Study of estimating instantaneous unit hydrograph applying genetic algorithm
遗传算法在估计瞬时单位线参数中的应用
Study on the real time checking model of procedure forecasting of unit line method
单位线法汇流过程预报的实时校正模型探讨
Application of the c . o . clark unit hydrography to the flux computation in a small scale basin of the loess plateau
单位线在黄土高原小流域汇水演算中的应用
The results show that the minus value and fluctuation of unit hydrograph can be mitigated and the error of observed discharge can be withstood using the robustified ridge estimation
最后采用抗差岭估计来推算单位线，该方法既可以解决共线性的问题，也可以抗御粗差的影响，得到比较稳定的单位线。
All the methods can calculate the flood based on the storm data . the software can be used in henan province . additionally , the rational formula method and the plain drainage method can be used in other regions near henan province , even farther regions
软件包括推理公式法、单位线法、平原排涝公式法三种由暴雨资料推求设计洪水的计算方法，除了适用于河南省中小流域设计洪水外，推理公式算法、平原区排涝公式算法也可在邻近省市和更大的范围内推广使用。
Through examination of the recession limbs of the observed hydrographs , during periods with no rain and thus no surface runoff , one can determine the value of . for this catchment , a value of 0 . 8 is obtained . the simulated subsurface runoff at each grid is routed to the outlets through a unit - hydrograph method for overland flow and the linear saint - venant equation for channel flow to get the discharge at xixian station
对所研究的流域而言,经过估算消退系数为0 . 8 .耦合着这两种不同地下径流机制的clm模型都可以计算出每个网格的地表地下径流深,采用dag lohman 34 , 35发展的汇流模型进行汇流由于是研究地下径流,所以取每个网格的地表径流为0 ,该模型采用单位线计算坡面汇流线性圣维南saint - venant equation进行河道汇流
The geomorphological instantaneous unit hydrograph ( giuh ) is viewed as the frequency distribution of the times of arrival of individual water deoplets at the catchment outlet . the travel path , for a typical hillslope cell . consists of a hillslope fraction , corresponding to overland flow and a stream fraction , corresponding to concentrated channeled flow . to obtain the time of travel , velocities must be defined . hillslope and stream velocities vary with location and must be strongly correlated with slope , and therefore a spatial distribution of velocities and hence of travel times could be obtained . the present methods of giuh neglect any time delays associated with overland flow pathways
地貌单位线被看作是流域上各水质点在弱相互作用下，到达流域出口汇流时间的频率分布。对于一个典型的山坡型网格单元，汇流路径由两部分组成，即坡地部分和河道部分，为了得到汇流时间，必须首先确定汇流速度。坡地和河道的汇流速度随着区域位置而变，并且必然与坡度有关，因此，可首先计算流速的空间分布，进而得到汇流时间的空间分布。
Geography position and meteorology character in gongboxia watershed are analyzed , according to which the excess of infiltration and instantaneous unit hydrograph are used in runoff and affluence models , and muskingum routing method in river course affluence , kalman filtering technique and least square method in real - time correction
分析公伯峡流域所处地理位置及该流域内的气象特征，确定产、汇流模型采用超渗产流和瞬时单位线，河道汇流采用马斯京根法，实时校正法由卡尔曼滤波和最小二乘法组成。