雨量分佈 的英文怎麼說

中文拼音 [yǔliángfēnbù]
雨量分佈 英文
rainfall distribution
  • 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
  • 分 : 分Ⅰ名詞1. （成分） component 2. （職責和權利的限度） what is within one's duty or rights Ⅱ同 「份」Ⅲ動詞[書面語] （料想） judge
  • 雨量 : rainfall; hyetal
  1. Figure 1 official weather observations - global distribution of cloudiness and rain

    圖一官方天氣觀測-雲量和降雨全球分佈形勢
  2. The interannual and decadal variability of precipitation for yunnan province in rainy season and its relationship with tropical upper layer heat content

    雲南省雨季降水的年際年代際變化特徵及其與熱帶上層海洋熱含量分佈的關系
  3. Figure 3. 1. 2 rainfall distribution on 3 - 6 august 2002 ( isohyets are in millimetres )

    日至六日的雨量分佈（等雨量線單位為毫米） 。
  4. Figure 3. 2. 2 rainfall distribution on 17 - 20 august 2002 ( isohyets are in millimetres )

    月十七至二十日的雨量分佈（等雨量線單位為毫米） 。
  5. Figure 3. 4. 2 rainfall distribution on 1 - 3 september 2003 ( isohyets are in millimetres )

    年九月一日至三日的雨量分佈（等雨量線單位為毫米） 。
  6. Chapter ii : latent capacity and present conditions of water resource. first, the author introduced the total amount and distribution of water resource in the east and central area of gansu, and then discussed the current utilization and contradiction between supply and demand of water resource. and last, the author posed the measures and countermeasures of exploiting water resource. chapter iii : latent capacity and present conditions of land resource. first the author introduced the total amount and distribution of land resource. and then discussed the current conditions utilization and latent capacity of land resource

    對東中部地區的水資源總量、分佈和特點進行定量和定性的分析，以灌區水資源利用及供需矛盾為突破口，對水資源潛力開發的幾個關鍵問題進行了分析：加強與水資源相關的基礎問題的研究；強化水資源危機的意識，建立節水工農生產體系；建立流域水資源統一管理機構；強化節水農業科技成果的推廣轉化；逐步推行噴、微灌高新節水技術；充分利用化學調控技術提高作物抗旱性和水分利用效率；大力發展以集雨節灌技術為核心的集水農業。
  7. Detailed diagnoses is made on a heavy - hard rain in the northeast qinghai - xizang plateau using ncep data of 1 x 1 with 6h intervals, more complete and integrated conventional observational data and the data set of automatic meteorological stations in plateau and new generation doppler radar data and satellite images and etc. the following conclusions can be drawn : 1. the distribution of heavy - hard rain, which is characteristics of valley topography in northeast qinghai - xizang plateau is obviously effected by topography. the distribution of yearly mean precipitation and the frequencies of heavy - hard rain in this area are descending from east to west

    本文首先利用ncep時間間隔為6小時的1 1的格點資料、更全面、更為完整的常規探測資料和高原地區布設的自動氣象站資料、新一代多卜勒天氣雷達資料、衛星雲圖資料等對高原東北部地區大到暴雨的天氣、氣候特徵及大尺度環流背景進行分析，形成對高原暴雨的整體認識，並為以後的數值模擬提供大尺度環流背景及依據，分析中發現： 1 、高原東北部地區大到暴雨的分佈明顯受到地形影響，年降水量和大到暴雨次數自東向西呈階梯性遞減趨勢，分別在高原東北部的外流河谷地區和四川北部地區存在大值中心。
  8. For surface rainfall distribution over hong kong, please visit

    有關香港地面的降雨量分佈，請參看
  9. But uneven rainfall distribution, rapid draining down of surface runoff, the lacking of subterranean sources, and terrace - type developments all over the foothills on the northern part of the island were major constraints. water resource development in the lower half of he 19th century was indeed a formidable task

    在降雨量分佈不平均、地表水源容易流失、地質不能儲存大量地下水、可開發的平地面積少，以及平地分散等種種障礙下，香港在十九世紀下半期要開發水資源，可謂困難重重。
  10. Using the mm5 model to conduct investigation of numerical simulation for this case, it was basically possessed of a capability to reproduce the genesis, development and evolution of the large - scale and mesoscale weather systems

    本文以mm5模式模擬分析「雅安天漏」為代表，著重研究了不同邊界層參數化方案對雨量中心強度、雨區分佈的影響以及雅安暴雨時的緯向垂直環流結構。
  11. The wetting front moved nearly parallel to the soil surface, and its length could be described by a power function of time, when the distribution of initial soil water was uniform

    當初始含水量分佈均勻時，降雨入滲過程中濕潤鋒面幾乎平行坡面運移，濕潤鋒深度與時間的關系可用冪函數描述。
  12. A map showing the rainfall distribution over the territory up to 1 p. m. today is attached in

    顯示本港今天直至下午1時的雨量分佈情況。
  13. For the rainfall distribution in hong kong today, please refer to the rainfall distribution map below

    有關本港今日雨量分佈情況（至下午7時） ，可參考以下雨量分布圖。
  14. 5 - day weather forecast ). a rainfall distribution map for today ( wednesday, 11 june 2003 ) up to 6 p. m

    本港今天（ 2003年6月11日星期三）雨量分佈情況（至今日下午6時為止）
  15. Rain was heaviest around 10 a. m. to 11 a. m. figure 1 shows the rainfall distribution over hong kong today till 6 p. m.

    有關本港今日雨量分佈情況至下午六時為止，可參考圖一。
  16. Rainfall distribution in the past hour

    過去一小時本港雨量分佈
  17. They do not occur in isolation from the rest of the landscape. the type of forest in a given area depends on many elements, including climate, soil, water source, rainfall patterns, seed sources and human influence

    森林並不可與周圍的環境分割，它們的存在乃取決于多個環境因素，例如天氣泥土水源雨量分佈種子來源及人類影響。
  18. Whether in the aspect of total rain days or total rainfall amount in a year, ya ' an is always an extreme range, which has been called " ya - an - tian - lou " in chinese. the predicted average physical structures in the raining process are as follows : ( l ) positive vortex and convergent center in the lower and middle troposphere and negative vortex and divergent center in upper troposphere ; ( 2 ) the superposition of the low layer zonal - vertical circulation and the up layer zonal - vertical circulation forms a strong upward current

    從6種不同方案對暴雨過程預報的實驗看，不同的邊界層參數化方案對雨帶特徵的模擬都具有一定的能力，同時模式模擬的降水對參數化方案的選取是敏感的，不同的參數化方案模擬出的降水范圍和雨量分佈有所差異，主要表現在降雨量中心強度及雨區分佈上。
  19. However, the effect of global warming may affect the atmospheric general circulation and thus altering the global precipitation pattern as well as changing the soil moisture contents over various continents

    但是，全球變暖的結果可會影響大氣環流，繼而改變全球的雨量分佈與及各大洲表面土壤的含水量。
  20. Figure 3. 1. 2 rainfall distribution on 20 - 21 july 2003 ( isohyets are in millimetres )

    年七月二十日至二十一日的雨量分佈（等雨量線單位為毫米） 。
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