槽中槽地形 的英文怎麼說

中文拼音 [cáozhōngcáodexíng]
槽中槽地形 英文
trough-in-trough form
  • : 名詞1 (盛牲口飼料或飲料等液體的器具) trough; manger (for water animal feed wine vat) 2 (兩邊...
  1. These meters find wide use in open channel measurement and are usually a type of weir or flume.

    這些流量計在明渠測量得到廣泛應用,通常是以水或堰的式出現。
  2. Through the study above, a refined description and modeling to flow field and water surface near the groyne in river is conducted with 2 - d and 3 - d mathematical models. the results by simulation are consistent well with experiment data

    通過上述研究,作者採用二維和三維數學模型對水試驗和天然河道丁壩附近流場和水面態進行了精細描述和模擬,計算結果和實測結果吻合良好。
  3. We can use the mm5 model in definite time, definite area weather forecasting. we conclude that : : the moving route of this necw in its developing progress was direct - south along latitude, the cold air is rough, and just this made the rough vertical velocity ; the necw southern moving and conflicting with the west pacification sub - tropical high makes rough jet steam. the plenty south - west warm and wet air made by the jet stream gave the rainstorm demanded vapor ;. the rough vertical velocity by jet stream is a main reason in this rainstorm ; the mm5 model uses four - direction analysis data as its input, this avoids some errors occurred in observe and transfer, thus made the result more useful

    綜合分析認為: ( 1 ) 、這次冷渦在其發生發展過程,其移動路徑是沿經圈直線南壓,攜帶的冷空氣勢力較強,后較強的垂直運動; ( 2 ) 、西太平洋副熱帶高壓偏北位置與東北冷渦南壓成的急流軸,把源源不斷的西南暖濕氣流輸送到遼西區,也就是急流軸的左前方位置,為這次暴雨的產生提供了充足的水汽來源; ( 3 ) 、低空急流不但為暴雨輸送水汽,其造成的較強的垂直環流也是產生強降水的一個主要原因; ( 4 ) 、 mm5模式以四維同化資料作為初始場,最大限度避免了觀測誤差可能造成的積分不穩定,提高了模擬結果的參考價值。
  4. 3 in the years of cold spring, the inner mongolia high and the aliushen low are strengthened with the low index of the east asia trough and the negative anomaly center of temperature over northeast china from surface to tropopause while the contrary conditions occur in the years of warm spring

    3 、東北區出現春季低溫的主要環流特徵是:內蒙古高壓,阿留申低壓的強度加強;阿流申低壓指數以及東亞大強度指數減弱,東北區從面到對流層頂處在溫度負距平心內,東北區春季高溫時則出現與上面相反的變化式。
  5. Some conclusions are listed as follows : the plateform cover cap of ordos basin and its circumference areas can be divided into five tectonic sequences. the tectonic evolution of ordos basin can be classified in six stages : the basement formation phase ( from archeozoic to paleoproterozoic ) ; the aulacogen phase ( from mesoproterozoic to neoproterozoic ) ; the north china continental sea phase ( from sinian to early - paleozoic ) ; the north china intracratonic depression phase ( from late - paleozoic to early mesozoic ) ; large ordos inland basin phase and the formation of independent ordos basin ( mid - late mesozoic ) ; fault basin phase around the ordos basin ( cenozoic )

    通過研究有以下成果及認識:鄂爾多斯盆及其周緣區沉積蓋層可劃分為五大構造層序,盆成和演化分為六大構造階段:太古代至古元古代基底成階段、新元古代克拉通內裂陷或坳拉演化階段、震旦紀?早古生代華北陸表海盆演化階段、晚古生代?早生代華北克拉通坳陷演化階段、生代晚期大鄂爾多斯內陸盆演化階段及獨立鄂爾多斯盆成、新生代周緣斷陷盆演化階段。
  6. As a result, we find that in winter when the kuroshio is cooler than the normal, at following summer, the continental cyclone deepen and the east asia monsoon strengthen, that the mid - latitude blocking high weaken and zonal circulation develop, the east asia teleconnection of " - + - " is stired up, so that subtropical high weaken and diminish, and tend to east north, tropical monsoon trough strengthen and mei - yu front weaken, and tend to north, meanwhile south asia high weaken and diminish, and tend to eastvnorth, is easy to form eastern region type

    結果發現當黑潮海溫冷異常時,後期夏季大陸熱低壓加深,東亞夏季風偏強。緯度阻塞高壓減弱,東亞區緯向環流發展,在東亞-西太平洋區激發「 - + - 」的東亞遙相關型,從而西太平洋副高強度偏弱,面積偏小,位置偏東、偏北,東亞梅雨鋒也偏弱,季風則變強,位置偏北。同時南亞高壓偏弱,位置偏北、偏東,易成東部型。
  7. From the model experiments, riffles in observed channel disappeared and were replaced by narrow depth channel with deeper stages

    在實驗過程,河道之河灘相繼消失,取而代之是明顯的深,使水深相對的提高。
  8. In this part, the first work is pretreatment of a numerical model, including creating calculating grids automatically, improvement of the linear boundary technique and so on. the second work is to estimate the siltation of a basin or channel by liu ' s equation. the third work is to build an edbms ( engineering data base management system ) for the result of mathematical model

    主要的工作是:其主要的工作一是數學模型的前處理,計算網格自動生成,線邊界法的優化;二是應用劉家駒公式在長江口深水航道治理工程理信息系統的支持下實現港池、航開挖的實時回淤估算;三是將計算成果成gis管理和支持下的工程數據庫系統( engineeringdatabasemanagementsystem ) ,同時嘗試解決時間序列數據如沖淤變化,潮位、流速過程的分析、查詢和顯示問題,並實現實時、互動的動態演示及三維可視化。
  9. The mesoproterozoic mafic dyke swarms are extensively distributed in the central north china craton, which are not deformed and metamorphic, emplacing the pre - existed fractures, so the dyke swarms become the conspicuous marks to reconstruct the mesoproterozoic tectonic stress field of the central ncc. the mafic dykes in the northern block are transtensional while the dykes in the central and southern blocks are extensional. the mesoproterozoic tectonic stress field could be simulated on the analysis of the distribution and mechanical origin of the mesoproterozoic mafic dyke swarms in the central ncc. the simulation result shows that the mafic dyke swarms were formed in the extensional tectonic setting in the ncc in the mesoproterozoic time, which are related to the extension of the mesoproterozoic yanliao - zhongtiao aulacogens cross the central ncc

    克拉通北部塊的鎂鐵質巖墻群為張剪性,而部和南部塊為張性。根據華北克拉通元古代鎂鐵質巖墻群的分佈和成因機制分析,來恢復模擬元古代的構造應力場。數值模擬結果表明鎂鐵質巖墻群在元古代成於伸展的大構造背景,與橫穿華北克拉通部的燕遼-條拗拉系的伸展作用有一定的聯系。
  10. This paper approaches reinforcement fabric cover, reinforcement fabric joint, reinforcement fabric embedded inserts, wall anchorage depth and wall joint form during the design of underground continuous walls, meanwhile, some problems affecting wall quality in the various sectors during construction are also discussed, including reinforcement fabric installation, groove bottom hole cleaning and quality testing equipment

    本文對下連續墻設計過程的鋼筋網保護層、鋼筋網接駁、鋼筋網預埋件、墻體錨固深度、墻體接頭式以及施工過程鋼筋網安裝、底清孔、質量檢測設備等各個環節影響墻體質量的一些問題進行了探討。
  11. Wujin huaheng wiring plastic factory is one underling factory of joint venture company of hongkong industry things conpany. we speciality produce all kinds of wiring accessories and electrician tools, etc

    常州市華恆電器塑料有限公司是專業生產經營行線、尼龍扎帶、纏繞管、梅花管、扁管、異管、配線器材等各種電器附件,產品在國內同行處于領先位。
  12. In 1999, the dipole existed in between the okhotsk high and the depression in the north of northeast china, thus the okhotsk high became active and maintained, the subh was located to an area quite further south than usual. the high persisted in the east region of nw china, the cold air flowed to the mid - lower reaches of the yangtze river along the high. in the east region of nw china, air steam under troposphere was strong sinking motion, and formatted the negative vorticity region, the vapour flux divergence was divgence. lt was apparently that the rain could n ' t occur in the eastern portin of nw china. in 2000 year, okhotsk high was very weak or did n ' t exist in, there was high in the east asia - japan, the subh is located to an area further north than usual. in the east region of nw china, the trough maintained, air stream under troposphere was strong ascending motion, the cycolonic circulation was prevailing, the vapour flux divergence was intensive convergences the rain easy happened in the east areas of northwest china

    4多梅雨1999年鄂霍茨克海阻塞高壓與我國東北北部低壓成偶極子,使得阻塞高壓穩定少動,西太副高位置偏南,西北區東部持續受高壓控制,冷空氣沿此高壓流經長江下游區上空;在西北區東部對流層下層氣流下沉運動較強,呈反氣旋渦度,水汽通量散度輻散,不利於西北區東部降水。空梅雨2000年相反,鄂霍茨克海高壓減弱甚至不存在,東亞-日本為高壓,西太副高位置偏西偏北,西北區東部處于西風,對流層下層氣流上升運動增強,盛行低壓環流,水汽通量散度強烈輻合,有利於降水生成。
  13. Regional difference in lower - level temperature dv and pressure dv are greatly weakened and dv of llj is distinctly faint without the nanling ridge. this result show that nanling ridge acts as a critical role in the establishment of dv of the lower - level temperature and pressure, which give rise to the dv of llj in south china

    而當模式僅僅去掉南嶺和武夷山山脈后,低層大氣溫度場日變化的區域性差異明顯變弱,梅雨低壓帶南側原南嶺山脈所在的溫度日較差明顯減小,使得梅雨低壓與華南區之間的南北向水平溫度梯度和水平氣壓梯度的日較差顯著變小,導致華南低空急流日變化的顯著減弱。
  14. The millimeter has the largest frequency band and the highest velocity of communication, but it has the highest cost and technical defaults : multi - path effect, reflect and scatter caused by cloud, smoke, water - dropping, the buildings, the grounds and its shape, the interference caus ed by the thunder, the complexity of device, difficult maintenance, and so on. now the band of the leakage coaxial line is up to 3ghz, leakage coaxial line has some advantages : good adaptability to cloud, smoke, water - dropping, the buildings, the grounds and its shapes, good steady field, it has some technical defaults : lower resolution for location and measuring velocity, the more complex of its sending - receiving relay devices, weak anti - interference, the strict demand for the hole size in the line, the cleaner work environment and the higher cost

    毫米波具有最大的帶寬和最高的通信速率,但也有最高的成本要求和較難克服的技術問題,即傳播的多徑效應,降水、雲霧、貌、建築物等的反射散射,打雷時的嚴重干擾,設備復雜,維護困難等等;泄漏同軸電纜的帶寬目前已做到3ghz ,具有對貌建築物的適應性強,場強穩定,但它的定位測速精度低,它的收發繼設備較復雜,抗干擾能力低,電纜上的開有著嚴格的尺寸要求,工作環境要求清潔,成本較高;傳統無線感應技術具有結構簡單,成本低廉,維護方便,定位精度較高的優點,但是,它沒有抗干擾能力。
  15. Tests of ship models ascending rapids with different hydraulic conditions were carried out in a flume with a generalized topography of rapids

    摘要在急流灘概化了的試驗水,進行了多種水力條件下的船模上灘試驗。
  16. Abstract : the mountain wave induced by a ridge in two - layer stratifiedfliud has been successfully simulated in a tank. the wave pattern is almost the same compared with the linear theory result qualitatively

    文摘:利用不同密度分層的鹽水模擬穩定層結大氣條件,在水成功模擬了兩層大氣分層流二維山脊引起的波,得到的波動圖像與線性理論模式結果在定性上基本一致。
  17. Because of the existence of meiyu precipitating cloud band the temperature dv is faint inside the meiyu trough and on account of large - scale prominent terrain available, significant temperature dv occurs on both sides of the trough, leading to the reinforcement of the subtropical high and middle latitude transformed high, and the deepening and narrowing of the trough in the night with the result that the relative intensity and precipitating function of the meiyu frontal rainfall system are changed at day and night, resulting in precipitation dv

    由於梅雨雲帶的存在,梅雨鋒低壓內溫度日變化很微弱;由於梅雨系統四圍高大的存在,梅雨鋒低壓南北兩側溫度日變化非常明顯,使南海副高和緯度變性高壓在夜間增強,梅雨鋒低壓也在夜間變深、變窄,改變了早、晚時刻梅雨系統的相對強度和降水功能,導致降水日變化。
  18. In the physical experiments, two incident wave heights, fifteen wave periods and four different boundaries on the end of the wave tank are selected for both plain and sinusoidal sandbar topography

    物理模型試驗,選取了2個入射波高、 15個波浪周期和四種水末端邊界條件,分別設置了平底和正弦沙壩
  19. In the numerical simulation, the open boundary and 1 : 1 slope on the end of the wave tank are considered with the other conditions same as the physical experiment ; the interaction between surface waves and the triangle / trapezium sandbars on the seabed is also studied

    數值模擬,除了對水末端為開邊界及1 : 1斜坡、其餘條件與物理模型試驗相同的情進行了研究之外,也對波浪與三角和梯沙壩的相互作用進行了研究。
  20. Based on the analysis of the temperature test result of the landing rectangle aqueduct of caohe river for the emergency water supply project of the beijing - shijiazhuang section on the middle route of the south - to - north water diversion project, the temperature developing feature of the early - age hydration heat of the thin - wall concrete is described, and then the main effecting factors of the hydration heat temperature on the landing rectangle aqueduct and the control measures concerned are put forward herein

    摘要通過對南水北調線京石段應急供水工程漕河渡段落溫度測試結果的分析,闡述了薄壁混凝土早期水化熱溫度發展的特點,提出了影響落水化熱溫度的主要因素與控制措施。
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