枯水年的英文

• dry year
• low flow year
• low-flow year
• year with low flow
• year with low water
• year with shortage of rainfall

• "枯水"英文翻译    low water
• "年"英文翻译    year
• "连续枯水年" 英文翻译 :    continuous dry years
• "平均枯水年" 英文翻译 :    mean dry year
• "特枯水年" 英文翻译 :    extraordinary dry year
• "水年" 英文翻译 :    year， water
• "枯水" 英文翻译 :    low water◇枯水河 oued; wadi; 枯水径流 low water flow; low water runoff; 枯水年 low flow year; 枯水期 dry season; drought period; 枯水位 low water level; dry season water level; low water
• "平水年（中水年）" 英文翻译 :    normal year
• "多水年" 英文翻译 :    high flow year; wet year
• "丰水年" 英文翻译 :    high flow year; high-flow year; wet year; year of abundance; year with abundance of water
• "立水年" 英文翻译 :    rainy year
• "平水年" 英文翻译 :    average water year; median flow year; normal year
• "双水年" 英文翻译 :    high flow year
• "中水年" 英文翻译 :    moderate flow year
• "枯水河" 英文翻译 :    oued
• "枯水季" 英文翻译 :    dry season; low water season; low-water season
• "枯水量" 英文翻译 :    low flow; low water discharge; low water flow; lowflow
• "枯水流" 英文翻译 :    low-flow
• "枯水期" 英文翻译 :    dry period; dry season; low flow period; low water period; low water season; low-water season; period of low flow; time of low water
• "枯水滩" 英文翻译 :    rapids at low water
• "枯水位" 英文翻译 :    draughty water level; low water level; lw; scanty water level
• "大洪水年" 英文翻译 :    massive flood year
• "地表水年鉴" 英文翻译 :    surface-water yearbook
• "国际水年" 英文翻译 :    international water year
• "连续丰水年" 英文翻译 :    continuous wet years

• Especially , river retreat in drying year becomes one of the main causes of desertification because of the decrease of runoff
  尤其枯水年径流量的减少可能成为影响盆地荒漠化的原因之一。
• It is found , through further study on the water temperature distribution in the high flow year , the low flow year and the cold year , that the influences of discharge and weather are limited on the water tem
  又就丰水年、枯水年和低气温年的水温分布作的进一步研究发现，水量和气象条件对大型深水温结构影响有限，其水温结构具有较强的稳定性。
• 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。
• The outcomes show that the two methods can separate the basin pollution load from different sides , the two separation results are close to each other and can be provided as references for drafting pollution prevention policies and ; the proportion of the two pollution loads in the basin is more or less the same , point source is slightly heavier in a dry year and the proportion of non - point source pollution is greater in a wet year
  结果表明，两种方法可以从不同的侧面分别对流域污染负荷进行分割，且两者分割结果相近，可以为流域污染防治政策的制定提供参考；流域内两类污染负荷所占比重大体相当，枯水年点源污染比重略高，而丰水年非点源污染比重较大。
• The runoff has been created in mountain and waters or neighboring regions , and it is 90 percent of the total in rainy season ; the total amount of precipitation is 7 . 08x109m3 in accordance with real amount , about 6 . 46 x 109m3or so , and it is 9 . 06 x 109m3in the rainy years , 5 . 66 x 109m3 in the drying years . there is 3 . 46 x 109m3 difference between them . so precipitation has a great influence on runoff
  在青海共和盆地，降雨产流主要在山区和水域附近，而且雨季产流占总径流量的90 ；盆地降雨的总产流量为7 . 08亿m ~ 3 ，丰水年为9 . 06亿m ~ 3 ，枯水年为5 . 66亿m ~ 3 ，因此径流量受降雨量年变率的影响很大。
• In consideration of the crises of both the industrial water and the domestic water in the estuarial areas of the yangtze river caused by the decrease of the channel runoff and the intrusion of the sea water during the dry season in dry year , the concept , method and planning framework of the water resources allocation for the areas mentioned above along the main stem of the river are put forward herein based on the preliminary prediction of the future water demands by taking the water resources allocation therein during the dry seasons as the actual case in combination with the status quo of the water environment and water resources utilization concerned
  摘要针对枯水年枯水季，因河道径流量较少，盐水入侵的频率和强度显著提高而引起的长江河口沿岸地区生产生活用水安全，文中结合长江口地区水资源利用和水环境现状，以大通以下长江干流地区在枯水季水量分配为实例，在初步预测未来河口地区水资源需求的基础上，提出长江口地区水资源配置的思路、方法及方案框架。
• Based on an analysis of causes and basic characteristics of drought in north and south areas of china , it is pointed out that drought in north areas , such as the yellow river basin and the huaihe river basin , was characterized by the severe systematic demand - supply contradiction resulted from the shortage of water resources , and successive drought disasters intensified by hot and dry weather , and that drought in south areas was characterized by the occurrence or successive occurrence of dry years due to hot and dry weather and the seasonal water shortage induced by their geographic and climatic features and insufficient water supply capacity
  摘要以区域干旱特征分析以及干旱灾害应对策略研究为目的，阐述我国南、北方两种不同地域类型的区域干旱成因和基本特征，指出黄淮海区域的干旱特征主要表现在天然水资源短缺引发的系统性深度供需矛盾，以及晴热少雨气候加剧这种矛盾而产生的持续干旱灾害；南方地区的干旱特征主要表现在晴热少雨气候导致枯水年或连续枯水年出现，以及地理气候特征和供水工程容量不足等因素产生的年内季节性干旱缺水。
• The results are as follows : ( 1 ) if we increase the pumping water by 493 x 104m3 , the amount of leakage recharge of rubber dam will rise by 231x 104m3 ; which indicates pumping by rubber dam can excite much more surface water infiltrate so as to supply groundwater . thus the utilization ratio of water source is increased , and it provides the reliable guaranty for enough supply of the groundwater storage in wet year . ( 2 ) under the condition of present status , the groundwater exploitable resource in wet year is 3670 104m3
  最后，通过数值法反复调算计算出本区地下水的允许开采量，计算结果表明，在现状开采的条件下，大沽河地下水库丰水年( p = 20 )时地下水允许开采量为13670 10 ~ 4m ~ 3 ，平水年( p = 50 )时地下水允许开采量为12054 10 ~ 4m ~ 3 ，枯水年( p =加% )时地下水允许开采量为10951xl了砰。

• 枯水年什么意思：枯水年 基本解释：又称“少水年”。指年径流量小于多年平均值的年份。在枯水年份降雨量少，河流水量小。