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單位線的英文

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"單位線"怎麼讀用"單位線"造句
英文翻譯手機版
  • unit fiber
  • unit hydrograph
  • unit line
例句與用法
  • Study of estimating instantaneous unit hydrograph applying genetic algorithm
    遺傳算法在估計瞬時單位線參數中的應用
  • Study on the real time checking model of procedure forecasting of unit line method
    單位線法匯流過程預報的實時校正模型探討
  • Application of the c . o . clark unit hydrography to the flux computation in a small scale basin of the loess plateau
    單位線在黃土高原小流域匯水演算中的應用
  • 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
    最后采用抗差嶺估計來推算單位線,該方法既可以解決共線性的問題,也可以抗御粗差的影響,得到比較穩定的單位線。
  • 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
    軟件包括推理公式法、單位線法、平原排澇公式法三種由暴雨資料推求設計洪水的計算方法,除了適用于河南省中小流域設計洪水外,推理公式算法、平原區排澇公式算法也可在鄰近省市和更大的范圍內推廣使用。
  • 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
    對所研究的流域而言,經過估算消退系數為0 . 8 .耦合著這兩種不同地下徑流機制的clm模型都可以計算出每個網格的地表地下徑流深,采用dag lohman 34 , 35發展的匯流模型進行匯流由于是研究地下徑流,所以取每個網格的地表徑流為0 ,該模型采用單位線計算坡面匯流線性圣維南saint - venant equation進行河道匯流
  • 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
    地貌單位線被看作是流域上各水質點在弱相互作用下,到達流域出口匯流時間的頻率分布。對于一個典型的山坡型網格單元,匯流路徑由兩部分組成,即坡地部分和河道部分,為了得到匯流時間,必須首先確定匯流速度。坡地和河道的匯流速度隨著區域位置而變,并且必然與坡度有關,因此,可首先計算流速的空間分布,進而得到匯流時間的空間分布。
  • 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
    分析公伯峽流域所處地理位置及該流域內的氣象特征,確定產、匯流模型采用超滲產流和瞬時單位線,河道匯流采用馬斯京根法,實時校正法由卡爾曼濾波和最小二乘法組成。
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