径流深的英文

• runoff depth

• "径流"英文翻译    runoff
• "深"英文翻译    deep
• "径流深度" 英文翻译 :    depth of runoff; height of runoff
• "年径流深" 英文翻译 :    annual runoff depth
• "流深" 英文翻译 :    flow depth
• "径流" 英文翻译 :    [水文] runoff 地表径流 surface runoff; 地下径流 groundwater runoff; 径流调节 runoff regulation; 径流涡轮 [机械工程] radial-flow turbine; 径流循环 [水文] runoff cycle
• "河流深水带" 英文翻译 :    river reach
• "河流深潭" 英文翻译 :    river pool
• "河流深泓线" 英文翻译 :    talweg
• "静水流深" 英文翻译 :    still waters run deep.; smooth water runs deep
• "水静流深" 英文翻译 :    still waters run deep.; smooth water runs deep
• "水流深度" 英文翻译 :    flow depth
• "水流深宽比" 英文翻译 :    form ratio
• "溢流深度" 英文翻译 :    overflow depth
• "比径流" 英文翻译 :    specific run off
• "表径流" 英文翻译 :    flow of ground
• "表流，径流。" 英文翻译 :    surface flow
• "第径流" 英文翻译 :    regulated flow
• "季径流" 英文翻译 :    seasonal stream flow
• "径流；流水" 英文翻译 :    running water
• "径流；溢出" 英文翻译 :    runoff
• "径流泵" 英文翻译 :    radial flow pump; radial flow （centrifugal）pump; radial flow(centrifugal)pump; radial pump
• "径流场" 英文翻译 :    runoff plot
• "径流量" 英文翻译 :    river runoff; runoff amount; runoff volume; volume of runoff
• "径流率" 英文翻译 :    percentage of runoff; rate of runoff; ratio of runoff; runoff rate

• The proportion that the main gully area accounts for the total gully area is more than 60 %
  及径流深h呈现较强的正相关性，其多元回归结果呈现明显的空间变异性。
• After computing grade , through statistic , we found flow - off deepnees and grade had exponential relation
  在计算了坡度的基础上，经过统计发现，径流深与坡度存在指数关系。
• Appling this idea , we set up exponential relation between runoff deepness and grade . finally we gained terrain surface flow - off deepnees distributing of 100m 100m grid in wenzhou
  基于此思想，建立了径流深与坡度的关系式，并做出了较好的温州地区的径流深结果。
• We applied those rainfall - rainoff relation formulas to the whole wenzhou area , and gained flat surface flow - off deepnees distributing map of 100m 100m grid in wenzhou
  经确认后又将各月的降雨径流关系应用于整个温州地区，因此得到了温州地区平地上100m 100m的径流深分布结果。
• Due to the increase of time interval and decrease of precipitation intensity within a month , no monthly runoff appears in some gridded cells as the xin ' anjiang monthly hydrological model is applied to the huaihe river basin
  由于计算时段加长，雨强均化，导致原新安江月水文模型在淮河流域的应用中，网格径流深出现了大量不合理的零值。
• The following conclusions were reached : i ) in different watershed , runoff depth and sediment transport modulus have power function ( y = axb ) relationship and the non - line regression equation can well simulate their relationship . parameter a and b can reflect difference of watershed harness degree
  通过研究，取得如下结论： ( 1 )在不同流域内，径流深与输沙模数均成幂函数( y = ax ~ b )关系，其关系方程以非线性回归拟合结果比较好。
• Ii ) runoff erosivity reflects relationship of water erosion forces and sediment yield more directly than rainfall erosivity . it intergrated ability of runoff volume and flood peak on detaching soil and transporting sediment and is more reasonable than single runoff depth or flood peak volume
  ( 2 )以径流侵蚀力代替降雨侵蚀力来反映水蚀营力与产沙量的关系更加直接，而且综合了径流量与洪峰在剥蚀土壤和搬运泥沙能力，比单独运用径流深或洪峰流量更加合理。
• It can be seen from the temporal behavior of the three aquifers that hillslopes with a larger inclination react significantly quicker to the re - charge input and tend tend to drain faster than nearly hori - zontal aquifers . this is caused by the increasing it can therefore be estimated using a finite differ - ence approximation , ststttntlqsnt where t is a discrete change in time . so the subsurface runoff parameterization with wa - ter storage and recharge based on the boussinesq - storage equation is founded
  很显然对于同样的入渗强度,地下径流深随着坡度的增大而变化明显,这里面关science in china ser . d earth sciences第4期? ?田向军等:基于boussinesq - storage方程同时考虑水分储存和入渗的地下径流机制379图2模型参数的敏感性键的原因在于随着坡度的增大,重力的因素起到了更大的作用
• Lesson engineering measure for research mainly from the sloping fields flow recycling potential analysis with gathering the water technique the both side collecting the region ' s rain - storm flood the data , year declining the water year the flow the data and water and soil conservation data , analysis combine intoing the small river valley flood the path comparing coefficient , water and soil conservation not flow coefficient , revising the new concept of deep etc . flow of year path , establishing synthesizing solving the sloping fields flow recycling the potential computing the model , bring upping gathering the water technique is with the
  课题研究主要从坡地径流资源化潜力分析和集水技术两方面入手，以典型区域为代表，收集了该地区暴雨洪水资料、年降水年径流资料及水土保持资料，分析并引入了小流域洪径比系数、水土保持不产流系数、修正年径流深等新概念，建立了综合解决坡地径流资源化潜力计算模型，提出了集水技术的工程措施和方法。
• Also to get some new conclusion of glacial lakes burst floods , in possibility study of glacial lake burst , and in qualitified study of the safety of the glacial lakes . the first character of this paper introduce the background of this paper , set the goal , content and methodlogy of the study work in this paper . the second chapter of this paper focuses on the meterological character , runoff composition character , why not correspondency of ratio of rainfall and runoff in same period to annual value for nianchu river , lasha river , niyang river and the middle reach of yalu - zangbu river
  本文第一章介绍了课题的研究背景，提出了研究目标、内容和方法；第二章重点分析了年楚河、拉萨河、尼洋河和雅鲁藏布江干流中游段的气候特征，径流组成特性，同期降水、径流占年总量比例的不对应特性和原因，径流年内年际变化规律及径流深分布特性，分析了天然洪水的特点和洪水参数；第三章介绍了冰川终碛湖的特点，结合已经发生溃决的冰川终碛湖的有关调查资料和考察资料，分析提出了危险冰湖判别指标和发生溃决的气候条件、周期性特征，提出了冰湖溃决洪水的计算途径。

• 径流深的日语：りゅうしゅつだか