日降雨量 的英文怎麼說

中文拼音 [rìjiàngyǔliáng]
日降雨量 英文
daily precipitation
  • 日 : Ⅰ名詞1 （太陽） sun 2 （白天） daytime; day 3 （一晝夜; 天） day 4 （泛指某一段時間） time 5 （日...
  • 降 : 降動詞1. （投降） surrender; capitulate 2. （降伏） subdue; vanquish; tame
  • 雨 : 雨名詞（從雲層中降向地面的水） rain
  • 量 : 量動1. （度量） measure 2. （估量） estimate; size up
  • 降雨量 : rainfall
  • 降雨 : rainfall降雨持續時間 time of the duration of rainfall; 降雨歷時 rainfall duration; 降雨時數 rainf...
  1. Then, six evaluation methods ( double ratio analysis evaluation method using regional rainfall tendency control for single cloud seeding operation case, regression analysis evaluation effects on the bases of regional correlation and developing tendency of rainfall, multiple regression analysis evaluation effects on the bases of regional developing tendency of rainfall, cluster - analysis - based floating control historical regression method with uniform precipitation and atmospheric precipitable water as meteorological covariates, cluster - analysis - based floating control historical regression method with uniform precipitation used as meteorological covariate, and float ing control historical regression method ) were compared and analyzed with the case of the cloud seeding operation on 5 april 2002 in henan province

    然後，以河南省2002年4月5日飛機增雨作業為個例，對作業區域趨勢對比雙比分析評估方案、區域趨勢相關回歸分析方案、區域趨勢多元回歸分析方案、以降水量為協變量的ca - fcm方法、以降水量和整層大氣可降水量為協變量的ca - fcm方法和fcm方法6種評價方案進行分析比較。
  2. So this article analyses deeply in the method of ensur ' my designing food rolume which is an important element to affect the " designimy height of bridge " it brings forward an " arverage optiminmy suiting line " method which is a bondage discommode series at the same time it puts forward a ensurmy principle for rough coefficient " and " fallimy flood proportion which are both suitable to heilongjiang province at last this article introduces the " three - days rainimy rolume " method

    本文立足於黑龍江省各種河流的洪水特點，結合以往工程實際，對影響跨河橋梁設計高度的主要因素? ?設計洪水流量及其相應洪水位的確定方法加以詳細分析。提出有約束不連序系列的加權優化適線法及適合於黑龍江省的河流粗糙系數和洪水比降的確定原則，並介紹了三日降雨量法。
  3. Yueyang is a wettish area of confienental subtropical monsoon with mild climate, plenty of rainfall and four distinct seasons. annually, the average temperature is about 17, the average precipitation is 1387. 93. mm, the average sunlight time is 1680 hours, and the frost - free period lasts 270 days

    岳陽市屬亞熱帶季風濕潤氣候區、氣候溫和、雨量充沛、四季分明，年平均氣溫17左右，多年平均降雨量1387 . 93毫米，年平均日照1680小時，無霜期270天。
  4. By surveying the sample plot, the relations between the stabil ity of the mountai n slope of soil preparation for planting by using explosion and other factors s uch as precipitation, terrain ， were studied. by using the method of quantitative t heory i, the interrelation between the damaged degrees of soil preparation progra ms by using explosion in low mountain area with abundant precipitation and terrain factors was systematically analysed, and the mathematical models relate d were developed. the results show that the precipitation in early days and the m aximum precipitation per day are the primary factors causing the soil prepara tion program damaged. the main terrain factors of the mountain slope that affect the program stability are according to their importance, slope, position and dir ection. the suitable mountain slope for soil preparation by using explosion is th e slope of less than 25

    通過典型標準樣地調查資料，探討了造林爆破整地工程的坡地穩定性與降水、地形等因子的相互關系，應用數量化理論，對在有充分降水條件下的低山丘陵區的爆破整地工程損失程度與地形因子之間的關系進行了系統分析，並建立了相應的數學模型，研究指出，充分的前期降水和日最大降雨量是引起爆破整地工程損失的激發因素；影響爆破整地工程穩定性的主要地形因子是地面坡度，其次為坡位、坡向，實施爆破整地工程的地面坡度以不超過25為宜。
  5. Sunshine, temperature, wind speeds and rainfall all affect the growth and cropping of apple trees.

    日照、溫度、風速和降雨量都能影響蘋果的生長和結實。
  6. The analysis of the large - scale synoptic situation shows that strong precipitation is closely related to the explosion of monsoon and the intensification of cross - equatorial flow which bring a lot of vapor and meet with cold masses at the eastern of northwest district on 8th, june causing extremely heavy rainfall ; that subtropical high - level jet at 200hpa, subtropical high at 500hpa and low - level jet at 850hpa are the weather backgrounds favorable to strong precipitation ; that the pattern of eastern highs and western lows and the establishment of a low - level jet and the coupling between upper - and low - level patterns that determine that the rain occurred in the east of the northwest china ( on average, this is the rainy season for the south of china, but not for the northwest china ) ; that water vapor comes from southerly and easterly flow which converge at the eastern of northwest district with convergence mainly in lower levels and pbl ; that the high value of the whole - level apparent heat source < q1 > is near the area of large rainfall in the direction of northeasterly - southwesterly agreeable to shear line very well and the condensation latent heat releasing is main heat source with vertical advection item playing key role in q1 and q2 ; that there is a vertical secondary circulation crossing low - lever jet whose ascending branch is at the area of large rainfall ; that the construction of convection instability and conditional symmetry instability results that there is not only deep thermal instability, but also moisture influx and triggering mechanism of thermal instability causing strong torrential rain

    作為對比，本文還對2002年6月24 - 25日發生在北京地區的強地形雨進行了分析，並討論陜南、北京地區兩地暴雨的異同點以及地形作用的共性和個性，為兩地暴雨預報提供有益的參考，得出了一些很有意義的結果： 1大尺度環流背景分析表明： （ 1 ） 「 02 . 6 」強降水與6月上旬越赤道氣流和季風爆發密切相關，攜帶大量水汽的偏南氣流與冷空氣於6月8日交匯在西北地區東部，導致了這次強降水的發生； （ 2 ） 200hpa的副熱帶西風急流、 500hpa副高以及850hpa的低空急流的配置非常有利於本文分析之陜西強降水的發展與維持。大尺度形勢分析表明，東高西低形勢場、低空急流的建立和高低空形勢的配置決定了這場降雨出現在西北地區東部。與暴雨區相聯系，存在一支橫越低空急流的經向垂直環流，暴雨區處于該垂直環流的上升支； （ 3 ）偏南和偏東氣流水汽通道在西北地區東部交匯，水汽的輻合積聚主要在對流層低層和行星邊界層內完成； （ 4 ）整層的視熱源< q _ 1 >高值區在暴雨區附近呈東北-西南向分佈，與切變線走向非常一致，降水產生的凝結潛熱釋放是強降水區大氣的主要熱源。
  7. In this paper aircraft has made vertical and synthetic detecting flying purposefully on 9. 17, 2003 according to cloud ' s macro and microstructure. vertical layers and representative places of stratiform cloud on 9. 17, 2003 are analyzed using the observational data of particle measurement system ( pms ), combined with satellite data, radar data, and precipitation data on ground. by this we have got cloud ' s microphysical structure and physical process of the natural precipitation, and the physical effect evidence has been testified according to observational data after lco2 seeding

    本文用綜合觀測的方法，利用機載pms雲粒子探測系統，根據雲系的宏微觀結構特徵進行有針對性的垂直探測飛行，配合衛星、雷達、地面雨量、雨強計網觀測資料對2003年9月17日延安降水性層狀雲系中那些有代表性的部位或垂直分層做細致的觀測分析，獲得雲系的微物理結構和自然降水形成的物理過程，並用觀測事實來驗證人工增雨引晶催化后的物理響應判據。
  8. The statistics for the summer months ( see panel hereafter ), show more deficient sun hours than excessive rainfall or cold temperatures, just like in 2002 and 1998

    根據夏季的氣候統計數據（見后附表） ，日照時間不足的年份要比象2002年和1998年那樣降雨量過多或寒冷的年份多。
  9. Shannon airport ' s station recorded rainfall of 48mm on september 21st, which was its highest daily fall for autumn in over 50 years, but it also recorded the highest daily temperature for the season on september 11th, when it was 23. 1 degrees

    夏農機場氣象站9月21日的日降雨量記錄為48毫米，這是這個地方50年來秋季最高的日降雨記錄，但9月11日也是此地這個季節最高的日溫記錄，當天是23 . 1度。
  10. There are two greater value centers : one is the valley region in northeast of the plateau, the other is the north of sichuan province

    外流河谷地區兩側山脈的年降雨量較大，年均大到暴雨日數較多，河源處相對較小，具有河谷地形的特點。
  11. Lasting a month starting from 17 may 2005, students will make an observation of cloud and rain after school each day, and record the information and remark on the designated

    由2005年5月17日開始的一個月，同學每天下課后進行一次天氣觀測，以肉眼觀察當時的雲量及降雨情況，並將觀測所得資料及有關感想輸入指定的網頁內。
  12. However, even during the wet season, yangon normally receives morning and afternoon showers while rainfall in bagan and mandalay is very low

    不過在雨季中，即便仰光每日早晚驟雨，蒲甘和瓦城的降雨量卻顯得非常的少。
  13. Connecting with country ' s natural scientific fund item and water resources and environmental important experiment item of shann ' xi province, on the basis of large sum of reading about domestic and overseas relative literatures, according to the rainfall data, including per day and per hour rainfall data of 21 years ( from 1980 to 2000 ), the paper analyzed the rainfall characters

    本文結合國家自然科學基金項目和陜西省水資源與環境重點實驗室建設項目，在閱讀並綜述了大量國內外相關文獻基礎上，根據西安市馬渡王水文站的21年（ 1980年- 2000年）降雨時、日資料，分析了西安市降雨特性。
  14. The heavy - hard rain in northeast qinghai - xizang plateau is that precipitation in 24h 25. 0 mm. the regional one is that there are three stations whose precipitation in 24h 25

    論文中高原地區的大到暴雨是指24h降水量25 . 0mm的降水，若同日有3個或3個以上站點出現大到暴雨時則稱為1次區域性大到暴雨。
  15. In 1977, owing to insufficient rainfall, hong kong again had to impose stage ii water restrictions. in order to increase the supply of fresh water, the lok on pai desalter put 4 units into production and by september, all 6 units were in operation. during this year the desalination plant was working at its maximum capacity, with 200 workers in the desalter, production was planned to increase to 60, 000, 000 gallons

    化淡廠的第一組鍋爐於1975年10月正式投產， 1977年，香港再次因降雨量不足實行二級制水，為增加食水供應量，樂安排海水化淡廠的四組鍋爐同時投入生產， 1977年9月， 6組鍋爐全面使用，是年政府擴充化淡廠規模，增聘工人至200名，計劃將海水化淡每日產量增至6千萬加侖。
  16. Each hopi clan perpetuates a unique ceremony, and the ceremonies together maintain the balance of natural forces of sunlight, rain and winds, and reaffirm the hopi respect for all life and trust in the great spirit

    每個霍皮人部落使特定的儀式保存下來，而儀式共同保持日光、降雨和風自然力量的平衡，重申了尊敬所有生命和信仰偉大的靈魂。
  17. Project i, project ii and project iii that are different in processing precipitation data as the input of hydrological model were built to model day hydrograph and flood hydrograph, so as to analyze the effect of spatial precipitation heterogeneity on runoff process

    本文建立了雨量輸入處理方法不同的方案、方案和方案三種方案，用這三個方案分別作日流量模擬與洪水過程模擬，來分析降水空間分異性對模擬水文過程的影響。
  18. A severe rainstorm over liaoning occurring from august 19th to 21st in 1997 by a landing northward tropical cyclone ( 9711 ) was simulated by mm5 non - hydrostatic model. through comparing the simulate results with the real weather, the different layer synoptic - scale circulation, height field, temperature field and precipitation were successfully reappeared. the main synoptic background in the case was as follow

    使用psu ncarmm5v3非靜力模式，對1997年登陸北上的11號臺風， 8月20日夜間在遼寧登陸前後，給遼寧帶來的大范圍大暴雨進行了數值模擬，並通過模擬的高、中、低空形勢場（高度場、溫度場） ，降雨量以及降雨強度與實況進行對比分析，是一次比較成功模擬，基本再現了遼寧大暴雨過程物理量場變化的全貌。
  19. Each year central american nations such as costa rica receive large amounts of rainfall during the wet season typical of tropical regions. however on january 11, 2005, the limon and caribbean areas along costa ricas atlantic coast experienced more than their usual levels of precipitation as the heaviest storm in forty years struck, causing severe damage and displacing many residents

    不過， 2005年1月11日，哥斯大黎加的利蒙省limon及其他位於加勒比海沿岸的地區，卻遭到40年來最嚴重的暴風雨侵襲，驚人的雨勢遠超過往常的降雨量，造成非常嚴重的災害，很多民眾被迫撤離家園。
  20. Although california is famous for its many hours of sunshine, there are large differences between regions and subregions in temperature, rainfall, soil types and other natural features

    盡管加州以日照時間長而聞名，但在不同區域的氣溫、降雨量、土壤和其他自然條件有很大的不同。
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