澇的 的英文怎麼說

中文拼音 [làode]
澇的 英文
waterlogged
  • 澇 : Ⅰ動 （受淹; 淹） inundate; waterlog Ⅱ名詞（因雨水過多而積在田裡的水） water logging
  • 的 : 4次方是 The fourth power of 2 is direction
  1. The distribution of the global dry and flood years takes on decadal character

    旱澇年的分佈有明顯的年代際特徵。
  2. Rock and soil mechanics problems in flood - waterlogging prevention of yangtze river drainage basin

    洪澇災害防禦中的巖土力學問題
  3. Analysis on eurasian circulation of drought and flood in summer of chongqing

    重慶夏季旱澇的歐亞環流特徵分析
  4. A trio of researchers compared donors with a gaggle of crop - growers, spraying water hither and thither, leaving some plants parched, others deluged

    三名研究人員將捐助國比作一群作物栽培者，灑水時這邊灑一點、那邊灑一點，一些植物因沒澆到而乾燥不堪，而其它的則因過量而積水成澇。
  5. The precipitation of northern hemisphere has a significant negative trend, lapse rate of precipitation during djf is - 0. 028mm / a. for the southern hemisphere, has n ' t pass the statistical significance. the flood / drought years are pick out in 1948 - 2001 for djf over global, northern and southern hemisphere, six large - scale areas, the results point out has significant decadal change in the flood / drought years of global, nh and sh in djf, during 1940s - 1970s global flood in djf occurred frequently and from 1970s - 1990s global drought in djf occurred frequently

    北半球有明顯的降水減少，約為- 0 . 028mm a ，南半球12 - 2月降水表現為極微弱的下降趨勢，且在統計上是不顯著的。劃分出了全球、南北半球、全球6個大尺度區域12 - 2月旱澇年，指出全球及北、南半球12 - 2月的旱澇有明顯的年代際變化。 70年代中期以前是全球洪澇多發期， 80年代到90年代為全球乾旱多發期。
  6. During flood years, the center of negative anomaly is around ural mountains, the center of positive anomaly is around high - latitude of east asia and another negative and positive center are over okhotsk sea and the north - west pacific, respectively

    通過對夏季旱澇等級指數的morlet型和mexicanhat型小波變換分析，發現山東夏季旱澇指數主要存在著2 5年和7年左右的周期振蕩。
  7. The positive and negative anomaly centers at 500hpa level formed the anomaly " wave train " from lower latitude to higher latitude over east asia. the teleconnection pattern called east asia - pacific pattern ( eap ) plays important roles in the summer rainfall in shandong area. study shows that weaker okhotsk sea high, northward location of subtropical high and stronger indian low, are likely to lead to more rain in shandong province in summer

    分析對比旱澇年不同層次高度場以及高低層散度場，結果發現，在春夏季旱澇年，高度場幾個主要的距平中心以及115 130 e區域高（ 200hpa ）低（ 925hpa ）層散度場基本呈現出反位相分佈特徵，北半球夏季存在的東亞-太平洋遙相關型（ eap型）對山東夏季降水產生重要影響。
  8. Climatological characteristics, which can provide some drought or flood years with large - scale background, are investigated for large - scale water vapor transport over asian - australian monsoon region based on vertically integrated water vapor flux by pentad from 1980 to 1997. at the same time, the differences of moisture transport over the yangtze river basin between drought and flood and the moisture budgets over eastern china from april to september are examined. major results are as follows : i

    使用1980 ? 1997年垂直積分的整層水汽輸送通量資料，從氣候平均的角度分析了亞澳季風區大尺度水汽輸送演變和偏南風水汽輸送在東亞地區推進的氣候特徵，為研究異常年份旱澇事件的產生提供了相應的大尺度背景；同時還討論了長江流域旱澇年水汽輸送的差異以及4 - 9月我國東部各區域的水分收支情況。
  9. The analysis of the drought and flood in the summers of 1971 2000 in baoji

    中國東北地區夏季旱澇的分析研究
  10. The mean duration of drought and flood events also has little secular trend

    旱澇的持續時間的長期變化也很小。
  11. By using it, we find many big and rich metal ore beds, resolve floodwater and so on. by these effective practice achievements, it proves that transient electromagnetic methods has wide prospect of application and development

    實踐結果找到了多個大而富的金屬礦床，並解決了泄洪防澇的燃眉之急，從理論和實踐上證明了瞬變電磁法有著廣泛的應用和發展前景。
  12. Results show that the corresponding relations are significant between the feature of drought and flood years in significant abnormal regions of precipitation and changes of the same period three wind fields

    指出降水顯著異常區域的旱澇變化與同期三層風場變化有較好的對應關系。全球陸地3 - 5月旱澇的變化和海溫變化之間存在一定聯系。
  13. We first calculated the mean duration of drought and flood events, we found that the mean duration of drought and flood events has little spatial variability over the globe. the mean of the duration is about 1 - 1. 5 months, with a standard deviation of 0

    指出旱澇（大旱大澇）的持續時間具有很小的空間變化，大部分地區的旱澇的持續時間變化在1 - 1 . 5個月之間，具有0 . 5個月的方差。
  14. Drought and flood are two of the major disasters that human being have to face. the losses due to them may be more than 50 % of the total disaster losses in jiangsu province. many valuable researches on meteorological and agricultural drought and flood have been done in world

    江蘇省地處北亞熱帶、東臨海洋，雨量充沛，氣候濕潤，但降雨量年際間變化大，年內分佈不均勻，造成不同年份干濕狀況差異較大，常有非旱即澇的現象，給主要作物生產帶來非常不利的影響。
  15. Using monthly mean rainfall and temperature data in north - west of china ( nwc ), the characteristics of rainfall anomaly at rainy season in nwc and the inter - annual varieties of drought / flood are diagnosed by means of eof, reof and wavelet analysis et al. and the ncep / ncar monthly reanalyzed data are employed to analyse the evolution character of water vapor flux and it ' s divergence flux, 500hpa height and u, v wind field. results show that ( a ) the space distribution of rainfall anomaly can be separated into seven climate sensitive areas, the first and the third region have the same rought / flood trend

    本文使用西北（區） 168個站1961 2000年6 9月（主汛期）月平均降水、溫度資料，運用eof 、 reof 、小波分析等方法診斷了主汛期月降水異常和旱澇的年代際變化；同時利用ncep ncar月平均資料，分析了強（弱）季風年西北空中水汽通量及其散度場、 500hpa高度場、 u 、 v風場的演變特徵，結果表明： （ a ）西北汛期降水可分為七個氣候異常區，第一、三異常區旱澇趨勢相同。
  16. Using the summer rainfall data from twenty - six observatories in shandong province from 1961 to 2001, the subtropical high index data from 1961 to 2002 and the monthly mean reanalysis data of wind, moisture, height and olr of ncep / ncar from 1958 to 1998, the characteristics of abnormal circulation in the northern hemisphere, the abnormal strength and location of subtropical high, the abnormal strength of monsoon and water vapor transport over the areas of east asian were studied

    利用山東26個代表站1961 2001年夏季降水、 1961 2001年副高特徵指數以及1958 1998年ncep ncar再分析月平均風場、高度場、比濕、 olr等資料，對山東夏季發生旱澇的北半球大氣環流、副熱帶高壓、東亞夏季風以及季風區水汽輸送等異常特徵進行了合成對比分析。對山東夏季旱澇形成的原因，從季風區水汽輸送和出現降水異常的物理機制等方面進行了較深入的研究。
  17. Baced on the general circulation background, synoptic - climatological cause and external forcing predictor of rainfall of yunnan in may, the composite model of the long - term weather process of yunnan in may for rainfall and the optimum subset regression model of rank statistics applied for dryness and wetness forecasting are presented

    摘要根據影響雲南5月旱澇的大氣環流背景、天氣氣候成因以及外界強迫因子，提出了雲南5月雨量的長期天氣過程的物理概念模式和用於旱澇預測的秩序統計量最佳子集回歸模式。
  18. 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年期間的氣象和水文資料，採用相關分析，經驗正交分析等方法，討論了該流域洪澇發生的規律及其與流域內降水分佈的關系.文章指出，江流域的水位變化有明顯的階段性，且具有全流域一致的特性，目前正處在80年代以來洪澇較嚴重的階段;嫩江流域降水異常偏多對松花江洪澇的影響比第二松花江的作用要大; 1998年夏季，松花江，嫩江流域出現超歷史紀錄特大洪水的關鍵原因是嫩江流域6 8月的降水距平百分率遠遠超過了歷史上的的最大值
  19. Lake surrounding economic zone : the zone is a dryland part within the proposed ecosystem function area, which has the potential to develop eco - economic, protect the water quality in the ecosystem function area, to control eutrophication and water quality deterioration, and to regulate inner land flood

    環湖生態經濟區：在生態功能保護區規劃區域內的陸域部分，具有發展生態經濟、保護生態功能區的水環境質量，控制湖泊富營養化和水質惡化，以及調蓄內澇的生態功能。
  20. Affected by the subtropical monsoon climate, jiangsu province is one of the provinces which have much natural disaster and drought, steady rain, waterlogging are its primary meteorological disasters. using citystar 3. 0, city star gis and reasonable indicators for disaster estimation, this paper progresses evaluation and analysis for its primary meteorological disasters such as drought, steady rain and waterlogging. in this work, the frequency of disaster and the risk to agriculture are taken into accounted

    因此，本文以該地區為例，選用影響該省主要氣象災害的定量指標，從災害出現頻率以及對農業生產帶來的風險出發，採用合理的災害風險評估指標，藉助于地理信息技術gis的空間分析方法，以風險指數為區劃指標，劃分風險等級，分季節對該省的主要氣象災害乾旱、連陰雨、雨澇的嚴重程度進行了評估和分析，獲得了gis系統支持下的災害風險區劃專題地圖。
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