降水距平的英文

• precipitation anomalies

• "降水"英文翻译    precipitation; rainfall; rai ...
• "距"英文翻译    distance
• "平"英文翻译    flat; level; even; smooth
• "水距" 英文翻译 :    water distance
• "距平" 英文翻译 :    departure
• "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
• "等距平" 英文翻译 :    equideparture
• "年距平" 英文翻译 :    annual anomaly
• "隔水距离" 英文翻译 :    water clearance
• "回水距离" 英文翻译 :    backwater distance; backwater length
• "每次划水距离" 英文翻译 :    dps=distance per stroke
• "变距平面" 英文翻译 :    betapiston
• "等距平线" 英文翻译 :    isabnormal line; isanomalline; isanomalous line; isanomaly; iso-abnormal line; isoanomaly
• "气候距平" 英文翻译 :    climatic anomaly
• "气温距平" 英文翻译 :    temperature departure
• "气压距平" 英文翻译 :    pressure anomalies; pressure anomaly
• "全距平均" 英文翻译 :    average of range
• "全距平均值" 英文翻译 :    ar averary range
• "温度距平" 英文翻译 :    temperature anomalies; temperature anomaly
• "正距平区" 英文翻译 :    pleion
• "正距平中心" 英文翻译 :    pleion
• "降水；降水量" 英文翻译 :    precipitation
• "长跨距平地机" 英文翻译 :    long-span land smoother
• "等温比容距平" 英文翻译 :    thermosteric anomaly
• "最大间距平面" 英文翻译 :    planes of greatest spacing

• The singular value decomposition analysis between theanomal of monthly mean ozone over kunming and theprecipitation anomaly field in yunnan province
  昆明月平均臭氧总量距平与云南地区月平均降水距平场的奇异值分解法分析
• A method is brought forward to identify the dry and flood years for precipitation during september to november in global and large scale areas . the way to test the method is also given
  提出了利用降水距平指数和旱涝面积指数对全球及大尺度区域9 - 11月进行旱涝年的划分，以及蒙特卡罗检验方法。
• There is the same characteristics of interannual and interdecadal variation between the first characteristic vecter and corresponding percent of the rainfall anomaly ; the second characteristic vecter which is the most obvious in may has interannual variable characteristics in each month
  华北春季及各月降水量第一特征向量和相应时期的降水距平百分率具有相同的年际及年代际变化特征；春季及各月的第二特征向量均存在年际变化特征， 5月最明显。
• 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
• The characteristics of precipitation anomalies in summer , previous and simultaneous ssta and preceding winter accumulated snow depth anomalies corresponding to positive and negative phases of 10 - yr mode and 25 - 30 - yr mode are discussed respectively . no matter for 10 - yr mode or for 25 - 30 - yr mode , reverse characteristics corresponding to positive phases and negative phases appear in the above fields . it proves that the decadal variation of sah have a good relation to the decadal variation of other key element of climate system and we can regard sah as a strong signal of the anomalies in the climate system
  ( 4 )夏季南亚高压东西振荡具有明显的年代际变化特征，本文分别讨论了对应于10年周期态的正位相年和负位相年及25 - 30年周期态的正位相年和负位相年时夏季我国降水距平、前期及同期海温距平及前冬青藏高原积雪距平的分布特征，发现无论是10年周期态还是25 - 30年周期态，对于夏季南亚高压东西振荡的正位相年和负位相年以上各要素场呈现为很好的反位相特征，说明夏季南亚高压的年代际变化与气候系统中其他要素的年代际变化具有很好的关联性，可将南亚高压看作气候系统中大气子系统异常的强信号，通过分析南亚高压的年代际异常可以更直接地研究和预测区域气候异常。
• The approaches establish a relationship between monthly precipitation abnormality and monthly circulation , soil moisture and temperature on the shallow and deep layers . the relationship is the precipitation diagnostic equation and its coefficients and dimensions are determined by using the observed data of huai river basin . then we select the main soil moisture and temperature attributing factors by the dimensional analysis to establish a forecasting equation of summer precipitation over huai river basin with the statistic approach
  通过将大气中的热量、水汽收支方程与一个简化的两层土壤温度、湿度方程相结合，并依据月尺度大气环流的演变特征，推导出月降水距平与500hp月平均高度距平场、土壤深浅两层温、湿度的关系；利用台站观测资料，使用统计反演方法确定方程中各项的系数和量级，从而找出影响降水的主要土壤温、湿因子；利用统计方法建立这些因子与淮河流域夏季降水异常之间的简单线性预报方程，并对1992 - 2000年淮河流域夏季降水趋势进行回报。