降水分布的英文

• rainfall distribution

• "降水"英文翻译    precipitation; rainfall; rai ...
• "分布"英文翻译    distribute; spread; scatter; ...
• "可降水分" 英文翻译 :    precipitable water vapor
• "云可降水分" 英文翻译 :    cloud precipitable water
• "有效可降水分" 英文翻译 :    effective precipitable water
• "降水量分布" 英文翻译 :    rainfall distribution
• "地下水分布" 英文翻译 :    groundwater occurrence
• "洪水分布" 英文翻译 :    flood distribution
• "水分分布" 英文翻译 :    moisture distribution
• "降水量分布图" 英文翻译 :    isohyetal map
• "月降水量分布" 英文翻译 :    monthly distribution of precipitation
• "地下水分布图" 英文翻译 :    map of groundwater table
• "喷水分布系统" 英文翻译 :    spray water distributing system
• "水分分布试样" 英文翻译 :    moisture distribution section
• "降水量分布特征" 英文翻译 :    precipitation characteristics
• "例如臭氧，降水的分布" 英文翻译 :    distribution
• "降水" 英文翻译 :    [气象学] precipitation; rainfall; rain; raininess 人工降水 artificial precipitation; 降水百分率 isomeric value; 降水带 precipitation zone; 降水迹 trails of precipitation; 降水区 [气象学] precipitation area; precipitation region; 降水散射干扰 precipitation scatter interference
• "水分" 英文翻译 :    1.(物体内所含的水) moisture [water] content; dew; humidity 吸收水分 absorb moisture2.(夸大的成分) exaggeration 这个报导有些水分, 需要核实。 this report seems somewhat exaggerated, and should be verified.; 水分保持力 moisture holding capacity; 水分代谢 water metabolism; 水分含量 moisture; humidity; 水分亏缺 water deficit; 水分平衡 water balance; 水分失调 water stress; 水分损失 [机械工程] moisture loss; 水分通道 passage of water; 水分循环 hydrologic cycle; damp; 水分应力 moisture stress; 水分张力 water [moisture] tension; 水分直减率 hydrolapse; 水分滞留过多 hyperhydropexis
• "降水；降水量" 英文翻译 :    precipitation
• "（基坑）降水" 英文翻译 :    dewatering
• "冰降水" 英文翻译 :    frozen precipitation
• "冻降水" 英文翻译 :    freezing precipitation
• "陡降，降水" 英文翻译 :    precipitation
• "降水场" 英文翻译 :    precipitation field
• "降水带" 英文翻译 :    precipitation zone

• The : greatest interannual precipitation variability is found in the southeast and the smallest one in the northwest of the province
  山东春季降水的年际变化与降水分布类似，东南部变化大，西北部变化小。
• The synchronization pattern is the basic one in each month of the season . the relation between the atmospheric circulation and rainfall patterns during spring in shandong province is discussed
  山东春季各月( 3 、 4 、 5月) eof分析表明，总体同旱同涝是各月降水分布的基本型。
• The difference of precipitation between the south and the north is obvious . the maximum of precipitation in the southeast is nearly twice the minimum of precipitation in the northwest
  山东春季降水分布呈现由东南向西北递减的趋势；南北差异明显，东南部的降水接近西北部的两倍。
• The three - dimensional cloud model with hail - bin microphysics could simulate the characteristics of the severe storm such as life cycle , rainfall distribution and diameter of hail well , and also could produce strong downdraft and wind shear ( downburst )
  而利用三维强冰雹云模式对此次强风暴的生命史、降水分布、降雹的大小等要素做了较好的模拟，并能够模拟出伴随强风暴过程所产生的强下沉气流和及地面强风速切变(下击暴流) 。
• Viet nam lies in south - east asia , belonging to tropical and subtropical climate region . according to geographical characteristics , it is divided into three parts . the characters of precipitation distribution of the three parts are different because of difference of climate conditions
  越南地处东南亚，属于热带和亚热带气候区，根据地理特征分为南、中和北部三个地区，由于各个地区处在不同的气候区域，因此降水分布特征彼此各不相同。
• The precipitation frequencies is analysed according to 1956 ~ 2000 years of rainfall record series in baoding area . the features of distribution of rainfall are detailed evaluated . firstly , the distribution of monthly precipitation is not even . for instance . the annual rainfall amount is about 548mm in whole year , about 80 % of them in summer season . secondly , yearly variation of rainfall is greater . thirdly , the abundant years usually are followed by short years , but the important changes have taken place in the last decades . before 70 ' s the abundant years took the dominant position , from the 70 ' s to the middle of 80 ' s the short years took place more frequently than ever . after the later of 80 ' s , the short years hold the main position . the above knowledge is instructive for guiding the rainwater resources effective utilization
  本文利用1956 2000年保定市的长系列降雨资料，对保定市降水量进行了频率分析、年内变化分析和多年变化分析，明确了保定市降水量年内、年际间的变化情况：保定市降水量年内分配不均，汛期( 6 - 9月)占年降水量的81 。保定市降水量年际间变化大，丰水年和枯水年交替发生， 70年代以前以丰水年段为主； 70年代到80年代前期降水量丰枯交替频繁，总的接近于枯水年段； 80年代后期至今以枯水年段为主。这种降水分布规律对农业生产雨水资源的高效利用具有重要的指导意义。
• In this paper , a bogused vortex with tilted vertical structure is firstly taken into account . check results of experiment b , experiment bt and experiment nb , we find that the simulated tc track , center pressure and pattern of precipitation during landing in experiment b are better than others . so , a bogused vortex with asymmetrical horizontal structure and tilted vertical structure is good for a tc moving in mid - latitude , which may be a new way to initialize this kind of tc in numerical simulation
  本文首次采用倾斜垂直结构的人造热带气旋作为初始涡旋，试验b和试验bt以及试验nb的模拟结果对比发现，前者对9806号热带气旋登陆前后的运动路径、中心气压、降水分布和初始结构的模拟能力优于后两者，因此，具有倾斜垂直结构的人造热带气旋比正压结构的人造热带气旋更适合于作为模拟中纬度运动的热带气旋的初始涡旋，从而提出解决该类热带气旋初始化问题的一种新思路。
• With the meteorological and hydrographic data in songhuajiang and nenjiang valley from 1951 to 1995 , using correlation analysis and empirical orthogonal analysis , the rule of the flood and relation between flood and precipitation distribution in this region are discussed . the results show that periodic change of water level is obvious in this region . now water level is in the serious stage from 1980 ' s . there are great relation between the water level of flood period and the precipitation . the unusual precipitation of nenjiang valley has greater impact than that of second songhuajiang valley . at the summer in 1998 , songhuajiang and nenjiang valley encountered the ghastly flood and the reason for that is the anomalous precipitation great exceeding the historic maximum
  利用松花江,嫩江流域1951 1995年期间的气象和水文资料,采用相关分析,经验正交分析等方法,讨论了该流域洪涝发生的规律及其与流域内降水分布的关系.文章指出,江流域的水位变化有明显的阶段性,且具有全流域一致的特性,目前正处在80年代以来洪涝较严重的阶段;嫩江流域降水异常偏多对松花江洪涝的影响比第二松花江的作用要大; 1998年夏季,松花江,嫩江流域出现超历史纪录特大洪水的关键原因是嫩江流域6 8月的降水距平百分率远远超过了历史上的的最大值
• ( 2 ) parts of the area show apparent local climatic properties because of the influence of topography , landcover , and so on . precipitation in mountainous and forest area is usually more affluent than in vicinity , this creates a typical mosaic structure of precipitation distribution like the islands . ( 3 ) soil water is the most significant form of water resources , which is the only water for vegetation uptake
  分析结果显示： ( 1 )黄土高原地区的降水分布自东向西、自南向北逐渐减少，东南部可达900多毫米，西北部最低则仅约100毫米，表现出显著的大陆性气候特征； ( 2 )由于地形等因素的影响，山地森林等局部地区小气候特征明显，降水量高于周围地区，结果形成降水的岛状镶嵌结构； ( 3 )土壤水是黄土高原最重要的水资源之一，它是该区植被水分利用的重要资源。
• Since the first three principal components can account for 81 % of the total variance , the three corresponding fields should be able to represent the main characters of the spring precipitation . they are : synchronized in the whole area of the province ( 63 % of the total variance ) , out of phase with southeastern part and northwestern part ( 11 % of the total variance ) , and out of phase with southwestern part and northeastern part ( 7 % of the total variance )
  发现前3个典型场就基本能反映山东省春季降水分布的主要特征，其累积方差贡献率为81 ，前3个典型场为：总体一致型(方差贡献率为63 ) 、东南-西北反位相型(方差贡献率为11 ) 、西南-东北反位相型(方差贡献率为7 ) 。

• 降水分布とは意味precipitation distribution