1)runoff[英]['r?n,?:f][美]['r?n,?f]流域径流
1.Influence of forest vegetation on runoff and sediment transport of watershed in loess area;黄土区森林植被对流域径流和输沙的影响
英文短句/例句
1.Study on Mid-and-Long Term Prediction of Runoff in ShiYang River Basin;石羊河流域径流中长期预测方法研究
2.Impacts of climate change on runoff in Shiyang river basin气候变化对石羊河流域径流量的影响
3.Runoff Simulation on Watershed of Dage River by HSPF Model基于HSPF模型的大阁河流域径流量模拟
4.Discussion on Multiple Time Scales of Runoff Variation in the Nenjiang River Basin嫩江流域径流量多时间尺度特征分析
5.Runoff Simulation in Hanjiang River Basin Based on SWAT Model基于SWAT模型的汉江流域径流模拟
6.Characteristics of Runoff Variation of Poyang Lake Watershed in the Past 50 Years近50年鄱阳湖流域径流变化特征研究
7.INFLUENCE OF RIVER NETWORK FRACTAL CHARACTERISTIC ON RUNOFF--CASE STUDY IN THE BASIN OF UPPER AND MIDDLE COURSES OF GAN RIVER水系分形特征对流域径流特性的影响——以赣江中上游流域为例
8.The Application of TOPMODEL in Runoff Simulation with Support of GIS;GIS辅助下的TOPMODEL模型在流域径流模拟中的应用
9.Study on Annual Runoff of Key Watersheds and Its Forecast in the Loess Plateau;黄土高原重点流域径流变化规律及预测研究
10.Study on relationship of soil erosion based on small watershed小流域降雨径流水土流失三因子关系
11.Runoff Simulation Based on SWAT Model in the Xixi Watershed of the Jinjiang River;晋江西溪流域降雨径流的SWAT模型模拟
12.The Characteristic Research on Rainfall and Runoff in ShannXi of WeiHe River Basin;渭河流域陕西片降雨与径流特性研究
13.Study of Rainfall-runoff Digital Simulation of Watershed in the Three Gorge Reservoir Area;三峡库区流域降雨径流数字模拟研究
14.Evolutionary Regularity of Runoff of Nenjiang River Basin in Period 1956-2000嫩江流域近45年来径流演变规律研究
15.Prediction of Rainfall and Runoff Changes in the Hanjiang Basin汉江流域未来降水径流预测分析研究
16.Evolution Characteristics of Runoff in Yellow River Basin During 500 Years黄河流域近500多年来径流量演变特征
17.Daily flow modeling in arid ungauged basin干旱区资料稀缺流域日径流过程模拟
18.The Analysis of Time-series Runoff Data of the Main Inflow Rivers in the Boston Basin;博斯腾湖流域主要入湖河流径流序列分析
相关短句/例句
watershed runoff小流域径流
3)runoff plot径流区域
4)the region of vehicle flow paths车流径路域
5)minor watershed小流域暴雨径流
1.Research purposes:Based on the geological survey for Jinzhou-Chifeng railway,the comprehensive analyses of many elements of the watershed along the railway are made for the purpose of seeking the methods for calculation of the rainstorm runoff of minor watershed.研究结果:结合本地区河流水系、水文、气象等自然特征,采用4种水文计算方法,得出不同公式计算流量的结果,经比较分析,锦州至赤峰铁路沿线,选用地方公式法计算小流域暴雨径流是适合的。
6)catchment runoff modeling流域径流模拟
延伸阅读
冰川融水径流 冰川冰和冰川表面雪融水汇入河道形成的径流。多数为季节性径流,少数大冰川末端为常年性径流,是寒冷地区的重要水资源。 形成 由0℃的冰转为0℃的液态水需要消耗的热量为335焦耳/厘米3。其热源主要来自太阳辐射,其次是冰面与近地面层大气湍流交换热和水汽凝结释放热。大陆性冰川的热量收支中,太阳辐射平衡值占80~90%以上,乱流交换热值占不到10%,凝结释放热值约占5%。海洋性冰川的热量收支中,太阳辐射平衡值仅约占60%,而乱流交换热值约占30%,凝结释放热值约占10%。 冰川融水径流多为季节性径流。在北半球每年春季融雪时,山区河流开始出现春汛(4~6月初)(冰面才开始消融,径流十分微小。6~8月为冰面的强烈消融期,形成大量径流。径流一部分沿冰面向河道下泄,一部分渗入冰内,通过冰下河道注入河流。冰内和冰下河道主要发育于冰温较高的海洋性冰川和大陆性的大山谷冰川的下段,如欧洲的阿尔卑斯山、北美的阿拉斯加以及中国西藏东南部、天山、喀喇昆仑山、喜马拉雅山等大冰川区。小规模的大陆性冰川则以冰面径流为主。冰面消融的情况通常用消融深度(A)表示,即以气温每增高1℃,冰川每日的消融深度计算。公式是: