annual rainfall 中文意思是什麼

annual rainfall 解釋
年降水量
  • annual : adj. 1. 每年的；年度的；一年（一次）的。2. （植物）一年一生的，一季生的。n. 1. 一年生[一季生]植物。2. 年刊，年報，年鑒。adv. -ly 年年，每年。
  • rainfall : 下雨，雨量。
  1. Adelaide enjoys a mediterranean climate with hot summers, cool winters, and an average annual rainfall of 530 mm

    阿德萊德屬于地中海型氣候，夏季炎熱、冬季涼爽，平均年降雨量530毫米。
  2. Crop yield correlates closely with annual rainfall

    農作物的收成與年降雨量有密切關系。
  3. This exceptionally dry month was the main contributing factor of the below - normal annual rainfall. the very dry weather in july was associated with the ridge of high pressure over the pacific being exceptionally strong and extending west to cover south china, bringing a long spell of fine weather to hong kong from late june to late july

    這主要是由於二零零三年七月是有紀錄以來最少雨的七月份，只有正常雨量的三分一左右，在六月底至七月底期間一道異常強大的高壓脊由太平洋向西伸展覆蓋中國南部，令香港長時間持續天睛。
  4. 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年保定市的長系列降雨資料，對保定市降水量進行了頻率分析、年內變化分析和多年變化分析，明確了保定市降水量年內、年際間的變化情況：保定市降水量年內分配不均，汛期（ 6 - 9月）占年降水量的81 。保定市降水量年際間變化大，豐水年和枯水年交替發生， 70年代以前以豐水年段為主； 70年代到80年代前期降水量豐枯交替頻繁，總的接近於枯水年段； 80年代後期至今以枯水年段為主。這種降水分佈規律對農業生產雨水資源的高效利用具有重要的指導意義。
  5. This year, the normal annual rainfall did not come to the state of rajasthan in northwestern india

    印度西北拉賈斯坦rajastan地區今年雨季遲遲未到，農作物無法栽種，災情嚴重。
  6. In general, the annual rainfall in these regions is less than the annual water loss by evaporation.

    總的來說，這些地區的年降雨量比一年內由於蒸騰而失去的水分要少。
  7. Based on the analysis of suzhou ' s urbanization process and annual rainfall time series analysis of suzhou and wangting precipitation stations during 1953 ~ 2000, by comparing rural precipitation ( wangting precipitation station ) with urban precipitation ( suzhou precipitation station ) and comparing rainfalls at each station in different periods, the authors analyzed the effect of urbanization on distribution of annual rainfall, precipitation, rainfall frequency etc

    在分析了蘇州城市化發展進程的特點及1953 ~ 2000年降雨時間序列特徵基礎上，採用同時期城區（蘇州站）與郊區（望亭站）雨量橫向對比、城市化發展不同時期同一站雨量縱向對比的方法，研究了城市化對該地區降雨量、降雨年內分配、降雨發生次數等的影響。
  8. The result shows that annual rainfall in the 15 coming years will increase by about 6 %, annual rainfall fluctuation will increase and rainfall concentration in a year tends to increase, which will make flood and sediment increased

    結果表明：未來降水量比多年平均值增加6 %左右，且年際波動性增大，年內分佈更加集中，洪水量和輸沙量有增大的趨勢。
  9. The correlations between the phenotypic traits of wintersweet and geographical and ecological factors are not significant except for latitude and annual rainfall

    蠟梅表型性狀與地理生態因子的相關分析表明：除緯度、年降雨量和部分性狀有相關性外，其它性狀和地理生態因子的相關性均不顯著。
  10. 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。
  11. 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。
  12. Through the annual rainfall of some counties in zhejiang province, the interrelated dimension of rainfall is calculated by the time - series method and rainfall characteristics arc analyzed

    摘要以浙江省某縣年降雨時間序列為例，運用分形理論汁算了該區域降雨的分形維數，並分析了所反映的降雨特徵。
  13. 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。
  14. Distribution map of mean annual rainfall in hong kong

    香港平均年雨量分布圖
  15. Mean annual rainfall distribution map

    香港平均年雨量分布圖
  16. Fig. 3 annual rainfall distribution for 1963, the driest year

    圖三歷來最少雨年份（一九六三年）的年雨量分布圖
  17. Fig. 1 annual rainfall distribution for 1997, the wettest year

    圖一歷來最多雨年份（一九九七年）的年雨量分布圖
  18. Fig. 1 annual rainfall distribution for 1997, the wettest year. fig

    圖一歷來最多雨年份一九九七年的年雨量分布圖
  19. 2 mean annual rainfall distribution 1961 - 1990. fig. 3 annual rainfall distribution for 1963, the driest year

    圖二平均年雨量分布圖一九六一年至一九九零年
  20. O in the century. annual rainfall in hong kong was found to be inversely related to the strength of the monsoon in the preceding winter ( figure 3 ), e. g., following the weak monsoon in december 1994 - february 1995 ( preceding winter of 1995 ), 2754 mm of rainfall were recorded in 1995, 540 mm more than the normal rainfall of 2214 mm. figure 2

    假若冬季季候風偏弱，隨后一年雨量偏多的機會亦會較高（見圖三） ，例如1994年12月至1995年2月期間的冬季（即1995年的前期冬季）季候風偏弱， 1995年錄得的年雨量達到2754毫米，比氣候平均的2214毫米多了540毫米。
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