鋒區 的英文怎麼說

中文拼音 [fēngqū]
鋒區 英文
front zone
  • 鋒 : 名詞1 （銳利或尖端的部分） the sharp point or cutting edge of a sword etc 2 （在前列帶頭的） van;...
  • 區 : 區名詞（姓氏） a surname
  1. A good one - two with shevchenko seven minutes later allowed the ivorian to slide home his second from an acute angle on the edge of the six - yard box

    7分鐘后，球隊一次漂亮的二過一配合，舍甫琴科送出一記直傳，象牙海岸前鋒迅速啟動，突入禁區，在離底線6碼遠的距離斜射打入個人的第二粒進球。
  2. Radical iraq, he thought, would be used as a battering ram against all moderate pro-western regimes in the area.

    他認為奉行激進方針的伊拉克將被人利用成為攻擊該地區一切持溫和方針的親西方政權的急先鋒。
  3. Blade ' s edge mountains : players accepting the bombing run quests in blade ' s edge plateaus will no longer cause other players in the region to stand up

    刀鋒山：玩家接受刀鋒半島的「轟炸」任務將不再使此地區的其他玩家起立。
  4. Near the tip, the reflection area of the apple seed geometry spread out and gave way to the flat grind surface, forming a very sharp tip dedicated to delicate cuts and thrusts. in addition, the guard of the sword was both practical and ergonomic

    而近劍尖處，原本兩個鋒口上的反光集區漸漸地平均化起來，顯示出那裡的橫切面為平面式，造成更尖的鋒口和劍尖，可以用在小巧的刺與割上。
  5. Middle-latitude cyclones originate at the polar front.

    中緯度地區的氣旋發源於極鋒。
  6. Rthk held a press conference together with the office of the privacy commissioner of personal data yesterday ( 10 may ), announcing details of the programme. attending guests included stephen lau, privacy commissioner for personal data, cheung man - sun, controller, etv of rthk, artistes such as nicolas tse, chiu wun, lee tze - hung, lo hing - fai, kwok siu - wan and au sin - yee

    香港電臺電視部昨日（五月十日）聯同個人資料私隱專員公署舉行記者會，公布節目私隱事件簿的詳情，出席嘉賓包括個人資料私隱專員劉嘉敏、香港電臺教育電視臺長張文新、演藝人士謝霆鋒、焦媛、李子雄、盧慶輝、郭少蕓及區倩怡。
  7. The result shows that : the sand - dust storm occured in favorable climate background that is drought and rainless, the tilted trough and mongolia cyclone are the important weather systems that caused the severe sand - dust storm, tilted trough and strong frontal zone caused the mongolia cyclone developed and the clod front strengthened at surface, high jet and ferrel circulation are the main reason that momentum spreaded downward from higher level and frontal zone strengthened on lower level

    結果表明：沙塵暴是在乾旱少雨的有利的氣候背景下產生的。斜壓槽和蒙古氣旋是觸發這次強沙塵暴天氣過程的重要的天氣系統，高空斜壓槽和強鋒區促使了地面蒙古氣旋的發展和冷鋒的加強，誘發沙塵暴天氣。高空急流及其下方的ferrel環流起到了高層動量下傳和加強低層鋒區的重要作用。
  8. Below 600hpa, the front of east asia was mei - yu front ; mei - yu equatorial front and polar front from the south to the north ; while above 600hpa, there was only mei - yu front. upon these conclusions, we put forward a conception model of east - asia front

    在600hpa以下，東亞地區的經向方向鋒區從南到北依次表現為梅雨鋒，梅雨赤道縫和極鋒；而在600hpa以上，只是極鋒型的梅雨鋒的單一結構。
  9. The diagnostic analysis for the sandstorm process on the base of height, temperature, pressure and wind etc output from the model shows that the upper cold trough, low - level wind shear, surface cold anticyclonic ridge, mesoscale cyclone and cold front are the main synoptic systems, surface cold anticyclonic ridge and cold front provide condition of wind force to occurrence of the sandstorm weather, the strong mesoscale cyclone before front makes pressure gradient before and after cold front obviously strengthen, moreover, and it increases obviously the temperature of the controlled area, as a result, the updraft movement caused by convergence before front strengthens

    500hpa強鋒區、 700hpa切變和鋒前中尺度系統的強弱及位置變化是沙塵暴天氣發生發展到減弱的直接原因。地面冷高壓、地面氣旋及冷鋒是造成本次沙塵暴天氣的主要地面天氣系統。地面冷高壓及冷鋒為沙塵暴天氣的發生提供了風力條件，而中尺度氣旋使冷鋒前後氣壓梯度明顯增強外，又使所控制的區域增溫明顯，使鋒前輻合上升運動加強，為沙塵暴天氣的發生提供了熱、動力條件。
  10. For understanding the dynamic processes of the all scales cloud systems of mei yu, and the relationship between mei yu system and the summer monsoon of eastern asia, the hubex has been carried on by the cooperation of china and japan in summer since 1998. the data observed by hubex, the data observed by other monsoon experiments and the general data ( gts data ) were merged into the assimilation system of game and made into the game reanalysis data, so how the game reanalysis data

    為了更好地理解梅雨鋒區多尺度雲系的能量與水分循環過程以及他們與地面水文過程的相互作用，從而搞清梅雨區雲系的多尺度動力學及其與東亞季風的關系， 1998年夏季中日合作開展了淮河流域能量與水分循環試驗（ hubex ） ，該試驗和game其他試驗的探空加密觀測資料作為原始資料的一部分經過同化分析，得到了game再分析資料。
  11. Only above soohpa, the mei - yu front is similar when we use the two ways to analysis

    在500hpa以上，用假相當位溫確定的梅雨鋒區與用溫度場確定的梅雨鋒區才較為一致。
  12. Vertical distribution of phytoplankton biomass and numerical abundance of calanus sinicus were investigated across the tidal fronts in the yellow sea, in october 2000 and may 2001. the abundance of calanus sinicus was higher at the frontal region than at the adjacent stratified and mixed areas while the chlorophyll - a concentration was highest in the stratified area or mixed area adjacent frontal region

    結果顯示中華哲水蚤豐度在海洋鋒區比其臨近兩側的混合區與層化區高；鋒區葉綠素a濃度低於其鄰近的層化區或混合區；葉綠素a濃度高值區通常位於鋒區鄰近的層化區或混合區一側。
  13. By combining with the simulation result of the vertical circulation structure, we propose that the factors induced the distribution difference of calanus sinicus and chlorophyll - a concentration not only include the grazing activities, vertical circulation structure at the fronts also plays an important role. the circulation of bohai sea in spring is examined to provide a reliable physical environment for biological model

    首次抽出黃海海洋鋒區的垂向環流結構有利於中華哲水蚤在鋒區的聚集，葉綠素a濃度高值區偏離鋒區也與鋒區上升流結構密切相關，模型研究中首先對渤海環流的物理機制進行了研究。
  14. By analyzing the abundance distribution of the calanus sinicus at the fronts in the two surveys, we try to find the direct dominant physical processes. and on the basis of that, provide a simple coupled physical and biological model and apply it in the bohai sea. the position of the tidal fronts and vertical circulation structure near the fronts are examined using the blumberg & mellor 3d nonlinear numerical coastal circulation model incorporating with mellor & yamada level 2. 5 turbulent closure model

    論文基於目前國際上普遍使用的blumberg & melior三維非線性環流模型（ ecom ）並結合mellor & yamada的21 / 2階湍封閉模型，採用blumberg & mellor改進的半隱式數值差分格式，首先對黃海海洋鋒位置及其鋒區環流特徵、形成鋒的主要動力機制等進行了研究。
  15. The first diagnostic analyses show that the heavy rainfalls are produced together by vortex, shear line and upper and lower jets, meiyu front. the condition of high energy, saturation, potential instability is propitious to the form and maintenance of heavy rainfall. the result of numerical simulation by mm5 model shows that heavy. rainfall has close relation with meso - scale vortex pole and strong convection

    採用ncep全球譜模式和常規觀測資料對「 03 . 7 」江淮地區的兩次暴雨過程的影響系統及其可能機制進行了初步診斷分析，發現梅雨暴雨是受低槽、低渦、切變線、高、低空急流和梅雨鋒區共同影響造成的，該地區維持高能、飽和、潛在不穩定的環境，有利於暴雨的產生中尺度數值模式（ mm5 ）模擬結果表明梅雨暴雨與中尺度渦柱、強對流運動密切相關。
  16. High pseudo - potential temperature along mei - yu front area mainly presented the deep convection of mei - yu area, so there would be a front along each side of the high pseudo - potential temperature, then the pseudo front would appear

    有人單從假相當位溫場分析鋒面結構，結果在假相當位溫高值舌區兩側各產生一個鋒區，這就產生了虛假的鋒區。
  17. Potential instability that exists with conditional symmetrical stability make the vertical ascend movement in e big value area and slope ascend movement in e surface ( meiyu front area ) produce and maintain

    位勢不穩定和條件性對稱不穩定共存使得在_ e高值區域的垂直上升運動和在_ e面（梅雨鋒區）上的斜上升運動得以產生和維持。
  18. As the strong normal share of the wind, turbulent fluctuation is strengthened and the sands are raised up from the surface ground the wind speed in the atmosphere of the low level has a horizontal share and this pushes the sands in the atmosphere aggregate, so the visibility descend

    近地面風速的垂直切變和地面熱通量的加大，都可使使邊界層湍流加強揚起地面沙塵。地面鋒區附近風場的強水平切變，鋒面垂直環流及鋒后斜壓轉換的作用，將地面捲起的沙塵帶到高空，爆發強沙塵暴。
  19. Energy front has offered energy condition to produce severe convection

    能量鋒區為產生強對流提供了能量條件。
  20. It was a typical mei - yu front on the middle and upper level of the troposphere which became wider with the height increased. the temperature field of mei - yu front area looked like " sandwich " with the warmer air along the each side of the colder air of mei - yu area

    在水平方向，梅雨鋒區的溫度場在對流層中低層呈現「暖-冷-暖」的「三明治」結構，即梅雨鋒區溫度最低，而在其兩側溫度最高。
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