潮流強度 的英文怎麼說

中文拼音 [cháoliúqiángdù]
潮流強度 英文
flood strength
  • 潮 : Ⅰ名詞1 （潮汐; 潮水） tide 2 （比喻大規模的社會變動或運動發展的起伏形勢） （social） upsurge; cur...
  • 流 : Ⅰ動1 （液體移動; 流動） flow 2 （移動不定） drift; move; wander 3 （流傳; 傳播） spread 4 （向壞...
  • 強 : 強形容詞（強硬不屈;固執） stubborn; unyielding
  • 度 : 度動詞[書面語] （推測; 估計） surmise; estimate
  • 潮流 : 1 （潮汐引起的水流運動） tide; tidal current; tidal wave; tideway: （船）逆潮流而上 stem the tide...
  1. Through quantitative comparison of the salinity, temperature, wind, wave, current, tide, biogenesis elements, and rare elements of coral reef in the coral reef zone of the nansha islands in china with these in the open sea, it is found that the nutrients and primary productivity in the coral reef are several dozen or several hundred times higher than those in the open sea. it is indicated that, given sufficient sunlight, the coral reef eco - environment could provide very intense photosynthesis, thus pointing to the important reason why the coral reef zone is highly productive

    根據中國南沙群島珊瑚礁區的溫度、鹽度、風、浪、流、潮、生源要素、稀有元素分析並與礁外海域定量比較，得出珊瑚礁區的營養物質和初級生產力比敞海高出幾十倍到幾百倍，表明只要有充足的陽光，珊瑚礁生態環境就可以提供十分強烈的光合作用，從而證明了珊瑚礁海區高生產力的重要原因。
  2. The results show that the strong winter monsoon will decrease the gradient of ssh, and change the characteristics of sst, which has influence on the sea current, especially in a shallow and closed sea area such as the south china sea

    結果表明：強冬季風會減弱海面高度梯度，普遍降低黑潮區海表溫度，對流場有一定的影響，尤其在南海這樣的封閉海區。
  3. From the pictures of the three - dimensional current system, we can see that the magnitude of the kuroshio current minishes as it deepens

    從三維流場圖可以看出，黑潮的強度隨深度明顯地減弱。
  4. The content including : ( 1 ) combined with the powerful matrix operation function and the abundant function computation of matlab, a load flow program is developed. due to the deeply research of admittance matrix, jacobian matrix and correction matrix, this program has a great advantage at both speed and code

    其主要內容如下： （ 1 ）結合matlab軟體強大的矩陣運算功能和豐富的函數計算功能，對潮流演算法中導納矩陣、雅可比矩陣以及修正方程求解的實現方式進行了深入研究，開發出一種速度和代碼量都具有明顯優勢的潮流程序。
  5. It also explain that the correlation between ssta of kuroshio and the change of wind field in equaroral mid - pacific is results of air - sea interaction ; however, when time comes into summer, the instance status of ocean is different from the last winter to next early springtime, the sea surface temperature turn into the definitive factor, so the increase of heat flux in may to jun month which is realized by absorbing more heat from the sun radiation results in the decrease of sst in kuroshio in the season of jun - jul. finally, during the aug to dec season of next year, the sst of kuroshio is increasing again

    最後分析了黑潮海溫與夏季東亞大氣環流及我國降水的時滯關系，發現：當前冬黑潮區域海溫異常偏高時，後期夏季亞洲低壓的強度減弱，西北太平洋副熱帶高壓強度加強，而且位置西伸、偏北，梅雨鋒位置偏南，長江中下游地區降水偏多，北太平洋冬季海域的海溫分佈呈+ 、 - 、 +趨勢（順序為赤道中東太平洋、西北太平洋、我國近海） ；反之亦然。
  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。中緯度阻塞高壓減弱，東亞地區緯向環流發展，在東亞-西太平洋地區激發「 - + - 」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，季風槽則變強，位置偏北。同時南亞高壓偏弱，位置偏北、偏東，易形成東部型。
  7. The well correlation times persist for about six months and the incidence level is reach or pass 0. 01. the meridional wind field which persistly impacting on sst in kuroshio region is near the west tropical pacafic. the result also behave as distinctly positive correlativity. afterwards we investigate the relationship between sst in kuroshio region and ninoc, 4 region and integrate the front conclusion. as a resultjt display that the sst in kuroshio region persists for positive relevance during the course of el - nino and inversely during the course of la - nina. subsequentl y the synthetic fields of kuroshio region ' s ssta in el - nino and la - nina years have proved the front outcome

    對與黑潮海溫異常變化關系密切的風場關鍵區及兩者的相互關系研究表明：黑潮本身的風場和其源地北赤道流海域的風場異常對黑潮海溫的影響僅限於同期及海溫滯后1到2個月，而能持續影響黑潮海溫異常的經向風場的關鍵區出現在赤道西太平洋（ 140 - 160e ， 5s - 5n ） ，緯向的關鍵區則在赤道中太平洋（ 160e - 150w ， 5s - 5n ） ，且緯向關鍵區的強度和范圍均大於經向，兩者對黑潮海溫的影響均能持續六個月左右。
  8. According to the data analysis, the large scale and continuous excavating sand from the riverbed, which has caused the riverbed downcutting, water level decline and relative strengthening of tidal action, is the basic and main cause that raises the saline water intrusion in the peal river network area, but the arid climate and the sea level rise only aggravate the disaster

    咸潮災害發生前和發生時期進行的大規模採掘河沙活動使三角洲河床普遍大幅度下切，河流水位下降，潮汐作用相對增強，這是引發咸潮的主要原因；而天旱和海平面上升等則使咸潮災害加重。
  9. Because of the low temperature there, water vapour condenses into small, clear crystals. a layer of glossy cirrus forms which drifts out from the centre of the tropical cyclone because of divergence at that level. so, when the outer edge of a tropical cyclone reaches hong kong, we can see cirrus high in the sky

    熱帶氣旋強烈的上升氣流會把潮濕的空氣帶到近五六千公尺以上的高空，由於溫度很低，水氣結成了透明的小冰粒，形成像絹絲一樣發光的雲彩-捲雲，這些在高層輻散流場區域的捲雲，會從熱帶氣旋中心向外流出，所以當香港還是位於熱帶氣旋邊緣時，我們便已看到那些在熱帶氣旋外圍的捲雲，並稱為臺母。
  10. On the basis of sediment concentration field, the annual back silting intensity on the approach channel of 70000 dwt at lianyungang harbor was also simulated, and the calculated results was coincident with actual data

    鑒于進港航道回淤量是當地海域潮流、波浪、泥沙長期共同作用的結果，建議採用年平均含沙量場進行回淤計算，並在此基礎上模擬了連雲港7萬噸級進港航道的年回淤強度，計算結果與實測資料吻合較好。
  11. Red tide is a natural phenomenon with complicated causes. under a favourable combination of various environmental factors, such as light intensity, temperature and nutrients in the seawater, and water velocity, microscopic phytoplanktons will bloom and create a red tide

    （三）紅潮的出現為自然現象，成因很復雜。在不同的自然環境因素如光線強度、海水溫度、水中營養物的水平、水流速度等的配合下，海水裡的微型單細胞浮遊藻類便會大量繁殖而形成紅潮。
  12. The local current disturbance after bridge being built in qiantang estuary leads to correspond changes of riverbed near bridge. but there is not any impact on astronomical tide, runoff large - scaled river shape and riverbed after bridge being built. so it does n ' t change the formation of tidal bore at all after bridge being built, but there is some impact on the shape and intensity of tidal bore because of pier resistance

    在錢塘江河口建橋將引起局部水流的擾動及近區河床的相應變化，但不會對天文潮、徑流及大范圍河勢、河床產生影響，因而，建橋不會從根本上改變涌潮的產生，但橋墩阻力對涌潮形態和強度是有影響的。
  13. The numerical simulation with complete forcing produces the main characteristics of yellow and east china seas circulation in summer. baroclinic effect plays a important role on yellow seas circulation that yellow seas cold water mass induces a anticlockwise circulation. tide also strengthens it

    夏季黃海的環流結構體現了較強的斜壓性，主要以密度流為主，黃海冷水團在黃海中部誘導了一個氣旋式環流，潮汐作用亦對這一環流有貢獻。
  14. At a given location, however, the strength of the tidal current is generally proportional to the relative tidal range for that day

    然而，在一定的地點，潮流強度一般與那一天的相對潮差成正比。
  15. The violent disorder of flooding and ebbing resulted in the release of nitrogen in tidal flat sediment and overlying water so that total nitrogen concentration raised rapid on water surface

    漲潮初和落潮末潮流對灘面的強烈擾動會導致灘面沉積物及間隙水中氮的釋放，造成上覆水體中tn濃度的迅速升高。
  16. The reason is that any country cannot be isolated outside the world on our contemporary earth, although the united states is a super - power, it is just as the other countries, because they ca n ' t exist and develop with

    其原因是，在當今世界，任何國家都不可能孤立於世界之外，美國雖然強大，仍然和其他國家一樣，他們只有在世界發展的潮流中求大同存小異，才能與中國等不同的社會制度和不同的發展水平的國家共同繁榮。
  17. The main characteristics of the tides and tidal currents and tide - induced residual currents in bohai sea are presented. the model results show that the density - reduced currents are comparatively robust and make an important contribution to the general circulation in bohai sea in summer. but in winter, the effect of the wind stress on the bohai sea general circulation is dominant

    文章較好的模擬了渤海的潮汐和潮流，給出了潮汐、潮流和潮致余流的一些主要特徵；模擬結果顯示，在夏季，渤海的密度環流相對較強，對渤海環流有重要貢獻；在冬季，渤海環流應是風應力的作用佔主導地位。
  18. When providing and untilizing contemporarg enterprise ' s strategy management theory and the theory or knowledge related, the thesis not only pay special attention to the tide of world enterprises strategy management in the world, but also bases upon chinese social reality and the enterprise characteristic, takes the particularity of the state - owned enterprise into account simultaneously. it focuses attention on deepening reformation, especially on the reformation of the property rights of enterprises and the establishment of modern enterprise system when formulating the strategic target objective and enforceable tactics. while lays stress on humanly supervision and scientific mamagement when setting forward the management theory

    本文在介紹並運用當代企業戰略管理理論及相關理論知識的同時，特別注意既緊跟世界企業戰略管理理論潮流，又立足於中國社會現實和企業自身特點，充分考慮到國有企業的特殊性，在戰略目標及實施策略上，都把深化改革，特別是產權制度改革，建立現代企業制度作為重要內容；在管理理念上，既注重人本管理，又強調科學管理，致力於為隆昌工務器材廠這樣處于困難局面的國有中型企業尋找一條可持續發展道路，也為同類企業提供借鑒。
  19. Results also indicate that the intensity of most current pattern is in general weakened by coast tide, such as yellow sea warm current ( yswc ). however tide strengthens cheju warm current and modifies east the path of yswc and deduces upwelling and descent current near the entrance of changjiang river

    潮汐因子整體上是削弱了黃東海環流各主要流系的強度，使黃海暖流強度減弱，路徑偏東，使濟州暖流加強，誘導了長江口附近的上升流和下沉流。
  20. ( 4 ) based on the ncar ccm3 simulations, the influence of the previously winter kuroshio ssta on the easm is investigated. results from the simulations are highly coincidence with the observations, namely, the winter kuroshio ssta may impacts the subsequent year east china summer rainfall by making influencing on the strength and location of the west - northern pacific high and the easm systems

    （ 4 ）利用ncarccm3模式模擬冬季黑潮區域海溫異常對東亞夏季風的影響，模式模擬的結果與統計分析結果是一致的，即前期冬季黑潮區域海溫異常可以通過影響次年夏季的西太平洋副熱帶高壓的強度和位置變化以及東亞夏季風環流的強弱，從而進一步影響我國東部地區的降水，尤其是長江中下游地區。
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