月降水量 的英文怎麼說

中文拼音 [yuèjiàngshuǐliáng]
月降水量 英文
monthly precipitation
  • 月 : Ⅰ名詞1 （月球; 月亮） the moon 2 （計時的單位） month 3 （姓氏） a surname Ⅱ形容詞1 （每月的） mo...
  • 降 : 降動詞1. （投降） surrender; capitulate 2. （降伏） subdue; vanquish; tame
  • 水 : 名詞1 （由兩個氫原子和一個氧原子結合而成的液體） water 2 （河流） river 3 （指江、河、湖、海、洋...
  • 量 : 量動1. （度量） measure 2. （估量） estimate; size up
  • 降水量 : precipitation; amount of precipitation降水量計 precipitation gage; 降水量學 hyetology
  1. Reof analysis was carried out for summer and autumn rainfall field over zhejiang province. the results indicate that the rainfall fields spatially are classified 3 subregions in summer and autumn, but they include some different place in each subregion

    就夏季降水量而言，浙江北部區降水最少，浙江東南沿海降水最多，無論從季節還是月降水量看，浙江北部區夏季降水都表現出非常明顯的正趨勢。
  2. With the model and the gis technology, the high - resolution dimensional grid - layer chart of monthly temperature and precipitation in viet nam is built. 3

    利用該模型和地理信息系統技術，建立了越南各月氣溫、各月降水量高解析度空間分佈柵格圖層。
  3. The paper in the context of the statistic - dynamic analyses the heterogeneity of spatial distribution of the precipitation. the generality of the spatial probability distribution model of the precipitation was explored

    本文從陸面過程的物理機制出發，利用統計? ?動力學方法，闡述了中國區域的月降水量和日降水量的空間分佈非均勻性，並尋求適宜的空間分佈概率密度函數進行描述。
  4. Using the daily and monthly ncep / ncar reanalysis data from 1951 to 2000 and monthly precipitation of 160 stations in china in summer from 1951 to 2000, the climatic distribution of heat source are computed. the responses of the asian monsoon circulation to the annual anomaly of the heat source over the bay of bengal in summer and the annual relationship between the heat source and the precipitation of china in summer are analyzed

    摘要利用1951 - 2000年ncep / ncar再分析逐日及月平均資料和我國160個測站1951 - 2000年月降水量資料，計算了夏季大氣熱源氣候分佈，分析了夏季孟加拉灣地區熱源年際異常及亞洲季風環流系統的響應，以及夏季孟加拉灣地區熱源與中國夏季降水的年際關系。
  5. Within the same year, precipitation mainly concentrates in june, july, august and september, april and november were the turning point of annual rainfall ; the dates of effective rainfall are less, and the dates of ineffective rainfall are more. there is significant or highly significantly correlations between annual precipitation and rainfall from july to october

    年降水量在時間分佈上，主要集中在6 9月， 4月和11月為一年中降水量變化的轉折點；年均降水日數88天，顯效降水日數少，占同期的13 . 6 ；無效降水量占年降水量的比例高，近47 ； 7 10月的月降水量與其年降水量都有顯著或極顯著的相關性。
  6. 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

    華北春季及各月降水量第一特徵向量和相應時期的降水距平百分率具有相同的年際及年代際變化特徵；春季及各月的第二特徵向量均存在年際變化特徵， 5月最明顯。
  7. Although the annual rainfall in counties of ningnan mountainous area fluctuates in time scales ( year, month, and 10 - days ), the rainfall is on the trend of decreasing in forty years

    以40年為尺度比較年降水量變化都呈降低趨勢；各月降水量隨時序的變化趨勢與年降水量隨時間變化的趨勢有不一致性。
  8. Through analysing the correlation between the annual rainfall in years ( annual rainfall > ( x. - 1s ) mm ; and annual rainfall > ( x - 1s ) mm ) with notable rainfall variation from the average and monthly precipitation, we found that, apparent correlation not only exists between the monthly rainfall in rainy season and the annual rainfall, it also exists between the monthly rainfall in some

    通過對偏離平均降水量較大的年份{年降水量偏多的年份： [ （ x + 1s ） mm ]年降水量偏少的年份:延x一ls ~ }年降水量與各月降水量相關性分析發現，除通常雨季月份降水量與年降水量存在顯著的相關性外，在一些地區雨季前某些月份的降水量也與年降水量存在顯著或極顯著的相關性。
  9. Second, the bar of the frequency - distribution and the curve of lorenz and the g coefficient are talked about the spatial distribution of day to day precipitation. the results show that the heterogeneous of day precipitation is strong on every day in a year. the spatial distribution model is left skew all in four seasons and it is different from the monthly precipitation

    其次利用全國700個測站逐日降水資料的空間分佈頻數直方圖及洛倫茲曲線和基尼系數闡述了我國逐日（ 24小時）降水非均勻性的事實，直方圖顯示全國范圍內逐日降水的水平空間分佈型在四季都是一種明顯左偏態型，與月降水量的水平空間分佈型略有不同；基尼系數值的月際變化也與月降水量的變化相反。
  10. By precipitation data of 42 gansu stations of loess plateau in march to july from 1961 to 2000 year and the soil weight information of moisture content at 11 agricultural meteorology stations from build station to 2000 year in march to november

    摘要利用甘肅黃土高原42個氣象站1961 - 2000年3 ~ 7月降水量和11個農業氣象觀測站逐年3 ~ 11月上旬的土壤重量含水率資料，分析了甘肅黃土高原土壤水分的地域和時間分佈特徵。
  11. Taking 1951 ~ 2000 monthly rainfall data in the zhanjiang area as the time series and using the gaussian radial base function and a delayed input window chosen at 6, a new intelligent forecast system is developed based on radio basic function neural network ( rbfnn ) to predict monthly rainfall from 1991 to 2003

    摘要以湛江地區50年來的月降水量為時間序列，利用高斯徑向基函數，選擇輸入窗口（時滯）大小為6 ，建立了一種智能型的徑向基函數神經網路預測系統，並分別對1991 ~ 2000年和2001 ~ 2003年的月降水量進行了測試預報和獨立樣本預測。
  12. 3. there exists distinct statistical relationship between precipitation of each summer month and prophase atmosphere general circulation in troposphere and low stratosphere

    青藏高原東北側地區夏季各月降水量同對流層、平流層前期環流特徵之間存在明顯的統計相關。
  13. The main contents and results are as follows. the distributive feature of global land rainfall for jja during 1948 - 2001 is analyzed

    主要研究內容和結論如下：分析了全球陸地6 - 8月降水量的分佈特點。
  14. Meanwhile, the january precipitation of the mid - lower yangtze tends to increase, and the el - nino events have occurred more frequently since late l970s

    此外，長江中下游1月降水量增多；厄爾尼諾事件從20世紀70年代末開始也明顯增多。
  15. In the most of areas in global land, the average precipitation in einino years is decreasing, the average precipitation in lanina years is increasing

    Elnino年全球大部分區域3 - 5月降水量偏少， lanina年全球大部分區域3 - 5月降水量偏多。
  16. The results indicate that the precipitation of global, nh and sh experienced decadal change : a minus - trend from 1974s global precipitation for djf, regression coefficient is - 0. 017mm / a

    結果表明：全球、南、北半球的12 - 2月的陸面降水有明顯的年代際變化，全球12 - 2月降水量從1975年開始的明顯的下降趨勢，回歸系數約為- 0 . 017mm a 。
  17. The study on the distribution feature of global land rainfall for march - may during 1948 - 2001 points out that the maximum precipitation occurs in the monsoon areas, and their standard deviation is bigger in monsoon areas than the others

    分析了全球陸地3 - 5月降水量的分佈特點。指出降水量最大區域主要在季風區，而且季風區降水均方差較大，降水在緯帶分佈上有著較大的連貫性。
  18. With the analysis methods of eof, reof, wavelet, correlation, running mean, and synthesis, sanxia summer precipitation ( sxsp ) anomaly rules and its reasons is studied. the results show that : ( 1 ) sxsp anomalies exhibit remarkable variation cycle of 15 years, 6 - 7 years and 2 ~ 3 years. the distribution of sxsp is in phase with the middle - low reaches of the yangtze river, while it is out of phase with that of middle and west of sichuan basin

    本文採用1959 2001年三峽庫區44個觀測站夏季（ 6 8月）降水量資料、 1959 2001年ncep ncar逐月、逐日資料， 1959 2000年中國160站降水資料、全球逐月海溫資料等，利用eof 、 reof 、小波變換、合成分析、相關分析、滑動平均等方法，研究了三峽庫區夏季降水異常規律及其成因。
  19. At first, based on the 272 station monthly precipitation in china, the paper described the heterogeneous of the spatial distribution precipitation by use of the curve of lorenz and the coefficient of g. the results show that the heterogeneous of the spatial monthly precipitation in summer is stronger than in winter. based on this describing, the probability distributions function of the spatial distributions are fitted by use of the gamma distribution model, and this general principle is examined. the results show that the gamma distribution is good on describing the heterogeneous of the spatial distribution precipitation in china

    並以分佈擬合中國區域月降水量的空間概率分佈，擬合效果優良，表明描述中國區域月降水量水平空間分佈非均勻性的普適分佈律以分佈的pdf最為適宜；以1 、 4 、 7 、 10月具有代表性的資料為例分析了各季月降水量空間分佈型的主要特徵及其形成原因，並從一個側面表明我國月降水量空間分佈的偏態性正是我國降水氣候的最顯著統計特徵之一，這也與我國大陸性季風氣候特點密切相關；並且月降水量的基尼系數和分佈模式形狀參數值都是夏季大於冬季，說明月降水量的空間分佈非均勻性夏季比冬季弱。
  20. The results of eof analysis of the rainfall anomaly in sping and respective month over north china indicate : spatial distribution of the first characteristic vecter is consistent in all areas ; the second characteristic vecter which is positive ( negative ) anomaly in north east, and is negative ( positive ) anomaly in south west in april is east west anomaly in each of spring., march and may ; the third characteristic vecter is north south anomaly in march

    華北春季及各月降水量距平場eof分解的結果表明：華北春季及各月降水量的第一特徵向量的空間分佈均為全區一致型；第二特徵向量除4月為東北正（負） 、西南負（正）異常外，春季、 3 、 5月均為東、西區異常符號相反； 3月第三特徵向量為南、北區異常符號相反。
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