降水場 的英文怎麼說

中文拼音 [jiàngshuǐchǎng]
降水場 英文
precipitation field
  • 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...
  • 場 : 場Ⅰ名詞1 （平坦的空地 多用來翻曬糧食 碾軋穀物） a level open space; threshing ground 2 [方言] （...
  1. For improve site soil condition and ensure piling work safety, we have worked out dewater construction proposal

    為改善現場施工的場地條件，保證壓樁工程的安全進行，編制降水工程的施工方案
  2. Analyzing the physics structure of vorticity, divergence, vertical velocity, frontogenesis " function, apparent heat source and apparent moist sink etc. indicated the physics fields are favorable for the occurance of the heavy rain over changjiang - huaihe river basin where the physics values are well according to the heavy rainstorm positions ; the low level jet is closely subject to the moisture and the coupled system of the low and the upper level jetstreams induced the strongly " ascending motion ; the intensity of the frontogenesis varies with the development of the rainfall system and reacts the rainfall intensity

    主要分析了這次過程中的多種物理量，包括渦度、散度、垂直速度、鋒生函數、視熱源、視水汽匯等，對這一暴雨過程有了比較系統的認識。結果表明：在江淮流域存在著有利於發生暴雨的物理量場配置，渦度、散度、垂直速度等物理量，與暴雨的落區都很吻合的；低空急流的產生不僅有利於水汽的輸送，而且高低空急流的耦合造成了有利於強上升運動的配置；鋒生強度隨著降水系統的發展變化，並影響降水強度。
  3. Deep and sub fissures were advantageous fields for ascending and assembling of the ore - forming thermal fluid. in addition, gritstone and mudstone provided the condition for the atmospheric water ' s descending

    深大斷裂及次級斷裂是深部成礦熱液上升和匯集的優良場所，周圍砂巖和泥巖又為大氣降水的滲透提供了條件。
  4. This paper use the ncep / ncar day - to - day reanalysis data of 500hpa high field and so on, choose ural mountain, baikal, okhotsk as the key district, the mid - high latitude of eurasia circulation courses that have long duration ( scale of time is middle, namely during 10 - 30 day ), maybe continue continuously after being intermittence of 1 - 2 days in middle, appear repeatedly is for research object, define an index " i " of the circulation pattern over mid - high latitude of eurasia. a method is proposed to identify the summer typical persistent circulation pattern at 500hpa levels over eurasia mid - high latitude. the climate characteristics of those typical persistent circulation patterns are studied

    本文利用ncep / ncar再分析逐日500hpa高度場等資料，選擇烏拉爾山、貝加爾湖、鄂霍次克海這三個地方作為關鍵區，以夏季歐亞中高緯度持續時間長（時間尺度屬于中間時間尺度，即10 ? 30天之間） 、中間可能會間歇1 、 2天然後又繼續持續、反復出現的環流過程為研究對象，定義了一個夏季歐亞中高緯流型指數，在此基礎上提出了一種對夏季歐亞中高緯500hpa典型持續流型的界定方法，研究了典型持續流型的氣候特徵，分析了流型指數的年代際變化，以及對應不同階段、不同流型的降水場、加熱場、海溫場等的主要特徵。
  5. In this article, the essential characteristic during meiyu and how to improve the criterion of meiyu, the effect process of circulation during meiyu, the characteristic of precipitation ' s distributing and the character between the precipitation and height are construed

    文章著重探討分析了梅雨期的系統特徵及如何改進梅雨標準、梅雨期大氣環流的影響過程、梅雨期的降水場分佈特點以及梅雨期降水場與高度場的相關特徵。
  6. We divided the global june - august precipitation field into 34 subareas and pointed out that there exists evident teleconnection among the june - august precipitation in these subareas

    用reof方法將全球陸地6 - 8月降水場分成34個大尺度降水分區。
  7. The precipitation forecast was improved quantitively, the forecasted severe convection area was consistent with the observation, and the spin up was reduced as much as 25 %

    試驗表明，預報的降水場有了相當程度的改善，預報強降水落區與實況非常接近， spinup問題改進了25 。
  8. Numerical experiments results on modeling the rainfall, show that : l ) the rainfall field modeled is improved and much similar to real rain field when tbb data is assimiliated into initial fields

    同化模擬試驗結果表明，衛星雲圖資料同化后模擬預報的降水場結果有了相當程度的改善，預報的強降水與實況比較接近。
  9. The calculating circle is very near compared with the fact. and many physical diagnose quantities thus as high vertical movement, q - vector divergence, 0 - 6 km shear etc. all contact with the rainstorm

    在降水場的模擬中，降雨帶的范圍與實況接近，強降水中心位置和強度略有偏差，通過修正意見對提高預報準確率會有很大幫助。
  10. We also use the data from 1920 - 2000, which were made by chen through interpolating the data of precipitation records in global land ( prec / l ) to replace the lack records of the global land precipitation dataset updated by or

    還用到了陳綠文利用prec / l資料將hulme的資料插補為完整的1920 ? 2000年全球陸地降水場資料，研究了1920 ? 2000年期間發生enso事件年份的全球及區域降水異常特徵。
  11. We have done intensive research on the characteristics of large scale background, rainfall field, the characteristic of mei - yu front and low in 1999, also we confirm the close relationship between the mei - yu low and heavy rainfall, and the possible developing mechanism

    我們分析了1999年的環流和大尺度背景場，降水場，梅雨鋒與低渦的結構特徵，並確定了梅雨鋒低渦與降水的緊密聯系，及發展的可能機制。
  12. The circumstance calculated by mm5 forecast system is very near compared with the real one ;. the physical quantity and precipitation calculated by mm5 forecast system should be well used in work ; the area and numeric of the precipitation forecasted by mm5 have some difference compared with the fact, that needs more some more work to make progress

    該模式對這次冷渦暴雨的形勢模擬與實際形勢場極其接近，是一個成功的應用範例； （ 5 ） 、 mm5模式對各種物理量和降水場的模擬結果與實況接近，在精細化的定點定量預報實踐中具有很好的參考價值； （ 6 ） 、 mm5模式預報降水范圍和強度與實況還有一定偏差，需要進一步深入的工作來改進。
  13. In the first part of the paper, on the basis of the weather processes of huai he basin from june to august in 1998, the difference and reliability of the two reanalysis data game and ncep from the fields of basic element, derivative, precipitation, and surface flux were studied by diagnostical and statistical methods. the results showed that the game reanalysis data is more reliable than ncep / ncar reanalysis data at the bottom and mid - high levels of troposphere, and at the precipitation and surface flux fields the case is just the same. in addition, the paper revealed that the game reanalysis data can show the evolution of the southwest vortex but the ncep / ncar reanalysis data cannot do so

    在第一部分，本文以1998年6 - 8月我國江淮地區的天氣過程為背景對game和ncep兩組不同的再分析資料的基本要素場、導數場、降水量場和地面通量場用氣候診斷和統計的方法進行了對比分析，結果表明，在對流層低層和中高層game再分析資料的基本要素場及地面的降水場和通量場較ncep再分析資料更為準確； game再分析資料能很好地反映出西南渦東移並影響江淮大暴雨的重要天氣特徵，而ncep資料則反映不出這一現象。
  14. Using the global land three months monthly data ( prec / l ) created by chen et al ( 2001 ), ncep / ncar reanalyzed monthly mean wind data and global monthly sst grid data edited by british meteorological bureau, this paper investigates some problems of the climate change of global land rainfall for march - may during 1948 - 2001

    用chen等（ 2001 ）最新創建的全球陸地月降水資料（ prec l ） 、美國ncep ncar再分析月平均風場資料和英國氣象局整編的全球逐月海溫格點資料，分析了1948 - 2001年全球陸地3 - 5月降水場的若干問題。
  15. And such zones act as an important dynamic condition for low - level water transfer and also a favorable environmental condition for " seeding - water supply ". there stronger echoes are detected, meaning that bubble convection develops in the precipitating fields of the clouds that are homogeneous in the main, causing centers of > 10 mm / hr surface rainfall to occur and migrate

    這些不穩定區是低層水汽輸送摘要重要的動力條件，也是「播撒一供應」機制發生的有利的濕熱力環境條件，雲系較強降水回波在這里得到發展，使整體均勻的冷鋒層狀雲系降水場有較強回波帶和對流泡發展，帶來地面有> 10mmlh較強降雨中心產生和移動。
  16. Based on the empirical orthogonal function ( eof ), the characteristics of large scale variations of precipitation anomaly during rainy season ( from jun to aug ) in south - west china for the period 1961 1995 is analyzed, and the teleconnection distribution charac - teristics between sea surface temperature ( sst ) over india ocean and precipitation during rainy season in south - west china were studied by using the method of cca

    用自然正交函數展開方法對1961 1995年西南汛期（ 6 8月）降水大尺度變化特徵進行分析，並在此基礎上用典型相關分析方法研究了1 8月印度洋海溫距平場與西南汛期降水場的遙相關分佈特徵。
  17. Mm5 adjoint - model assimilation system not only can improve the initial field effectively and promote the coordination with the model but also can enhance the forecast on the precipitation and other elements. the assimilation of cdw has an improvement on quality of upper wind. the effect of direct numerical simulation with utilizing the cdw to amend the initial field gains the advantage over the one not

    結果表明， mm5伴隨模式同化系統能有效改善初始場與模式的協調能力，提高模式對于降水場和其它要素場的預報；使用雲導風資料修正初始場后直接模擬的效果比未使用時直接模擬的效果要好，對部分區域的強降水預報精度有一定程度的改善；使用伴隨模式同化系統后，加入雲導風資料的同化試驗對其它要素的改善與直接同化常規資料的效果相比，改善優勢不明顯，但從各要素的誤差來看，對于風場的改善最好。
  18. The positive load take absolutely advantage in the first spatial pattern of year and seasons. especially that the precipitation field load of winter is all positive. not in the southwest of china because of southwest monsoon etc. system ; the characteristics of the second spatial pattern are that most of the area is taken up by positive load in year and four seasons, the west of talimu basin is the center of negative load of the year, spring and autumn vector fields ; east of zhungeer basin is the center of positive load of the third spatial pattern of year, spring, summer and winter, the center of negative load is often in east of chaidamu basin, but the distribution center of autumn is in east of zhungeer basin ; the distribution of the fourth spatial pattern is difficult to describe and forms several centers of positive and negative load ; several centers of positive and negative load also appear, the distribution of load fields of the fifth spatial pattern of year, spring and winter represents the situation of " +, -, + " from southeast to northwest ; the complexity of the sixth spatial pattern is more stonger than that of the fourth and the fifth spatial pattern, several centers of load fields of year and each season often appears inverse situation of the positive and the negative load. but the centers are still most in zhungeer basin, chaidamu basin and talimu basin

    第一空間型中，年和四季都是正荷載占據絕對優勢，特別是冬季降水場皆為正值，只是西南地區由於受西南季風等系統的影響，表現為與其它地區的不同；第二空間型的特點如下：年和四季分佈皆為正荷載占據大部分區域，負荷載中心年、春季和秋季分佈中都是位於塔里木盆地西部地區；第三空間型正荷載高值中心除秋季外都是處在準格爾盆地以東地區，負荷載中心多在柴達木盆地以東地區，秋季卻處于準格爾盆地以東地區；第四空間型分佈就較復雜無章法可言，形成多處正負荷載中心；第五空間型特徵是這樣的，同樣是多個荷載中心出現，年、春季和冬季中的荷載場分佈從東南到西北大體呈現「 + 、 - 、 + 」的特點；第六空間型分佈的復雜程度較之第四、第五空間型更大，年和各季分佈比較中多個荷載中心常出現正負相反的情況，但中心仍以柴達木盆地、準格爾盆地和塔里木盆地為主。
  19. Based on the global land monthly rain data ( prec / l ) created by chen et al ( 2001 ), ncep / ncar reanalyzed monthly mean wind data and global monthly sst grid data edited by british meteorological bureau, this paper investigates some problems of the climate change of global land rainfall for june - august ( jja ) during 1948 - 2001

    本文採用chen等（ 2001 ）最新創建的全球陸地月降水資料（ prec / l ） 、美國ncep ncar再分析月平均風場資料和英國氣象局整編的全球逐月海溫格點資料，分析了1948 - 2001年全球陸地6 - 8月降水場氣候變化的若干問題。
  20. Horizontal well technology, have another name called the well technology of radiation, sets up perpendicular well in the precipitation place, and direction horizontal well in the different degrees of depths of perpendicular well, make groundwater pass the horizontal well to flow into the collect water perpendicular well, take water out with the water pump again, in order to achieve the goal of reducing the groundwater

    水平井技術，又稱輻射井技術，是在降水場地設置集水豎井，于豎井中的不同深度和方向打上水平井點，使地下水通過水平井點流入集水豎井中，再用水泵將水抽出，以達到降低地下水的目的。
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