風暴波浪 的英文怎麼說

中文拼音 [fēngbàobōlàng]
風暴波浪 英文
storm tide
  • 風 : Ⅰ名詞1 （空氣流動） wind 2 （風氣; 風俗） practice; atmosphere; custom 3 （景象） scene; view 4 ...
  • 暴 : Ⅰ形容詞1 （突然而且猛烈） sudden and violent 2 （兇狠; 殘酷） harsh and tyrannical; cruel; fierce...
  • 波 : Ⅰ名詞1 （波浪） wave 2 [物理學] （振動傳播的過程） wave 3 （意外變化） an unexpected turn of even...
  • 浪 : Ⅰ名詞1 （波浪）wave; swell; billow; breaker 2 （像波浪起伏的東西） things undulating like waves 3...
  • 風暴 : storm; windstorm; tempest
  • 波浪 : wave
  1. In consideration of studying island coast hydrodynamic factors is in order to build breakwater engineering, design waves, astronomic - tide and storm - tide which increases water level are computed to offer design parameters, discuss and analyze the influence of engineering safety aroused by those factors

    考慮到研究海島周圍海岸動力因素的目的是為了建設海島工程，還進行了設計波浪以及天文潮、風暴潮增水的計算，分析了這些因素對工程安全性的影響。
  2. This kind of spurious echoes is called sea clutter and is caused by reflection from rough seas, a result of the storm s gale force winds

    這類假的回波被稱為海雜波，是由風暴的烈風颳起的大浪反射所引致。
  3. Oceanographic information is indispensable in many activities including astronomical tides for maritime operations, storm surge levels to warn of possible sea flooding and for reclamation projects, and wave heights for shore protection, sea wall design and offshore operations

    例如海上作業要參考潮汐資料和填海工程要考慮風暴潮可能導致的水浸威脅。此外，海岸防護工作、防波堤設計和離岸工程都要應用到海浪高度資料。
  4. Mosquitoes came buzzing in and hummed sullenly round the room ; the sea, which i could hear from thence, rumbled dull like an earthquake - black clouds were casting up over it ; the moon was setting in the waves, broad and red, like a hot cannon - ball - she threw her last bloody glance over a world quivering with the ferment of tempest

    蚊子嗡嗡的飛進來，陰沉地在房間里打轉。在那兒我能聽到大海之聲，像地震一般沉悶地隆隆響著。黑雲在大海上空集結，月亮沉落在寬闊的紅色波浪上，像一個滾燙的炮彈一向顫抖著正醞釀風暴的海洋，投去血色的目光。
  5. Study on the wave - tide - surge interaction in shallow sea is one of the up - to - date active research areas around the world. this research has studied the bohai sea wave - tide - surge interactions and the laws of substance transport

    本項研究針對典型淺海海域渤海，研究了在這個海域的波浪、潮汐風暴潮的相互作用以及物質輸運規律。
  6. 5 ) it is more reasonable when the numerical model including the wave - tide - surge interactions, and the numerical results are close to the measured data. 6 ) tha laws of substance transport under the tide are different from that of the wave - tide - surge

    6 、浪、潮汐風暴潮作用下的物質輸運規律明顯不同於單純潮流作用下的物質輸運規律；在考慮物質輸運的時候，必須重視波浪的影響。
  7. By adoption this numerical model, the study has emphases on the effect of wave on the wind stress, wave on the bottom stress and radiation stress on the sea level. the study also has researched the effect of tide - surge to wave

    運用這個模式，重點研究了波浪對表面拖曳系數的影響；波浪對底摩擦應力的作用；輻射應力對潮汐風暴潮水位的影響以及潮汐風暴潮對波浪的作用。
  8. The combined wave - tide - surge numerical model which is composed of two components : a third generation shallow water wave model and a two - dimensional tide - surge model

    模式主要由兩部分組成：一個物理上先進的第三代淺海波浪數值模式和一個二維潮汐風暴潮數值模式，實現了兩個模式耦合。
  9. Subsequently, the waves induced forces and their driven effects on currents are studied in detail. in the discussion of the effects of currents on waves, according to the wave radiation theory and the law of wave action conservation, the equivalence of none vorticity condition of the vector of wave number in constant wave field and fermat theory is testified. the dynamic and kinematics effects of background currents on waves are introduced concisely

    在流對浪的作用討論中，依據波動的射線理論和由變分原理導出的波作用量守恆定律，闡明了穩定波場波數矢量的無旋條件與費馬原理的等價性，扼要討論了背景流場影響海浪的運動學效應和動力學效應，首次指出水位（包括天文潮位與風暴潮位）變化對海浪成長與消衰的影響，為流浪潮聯合數值模式的發展提供必要的理論依據。
  10. In the storm, the part on surface layer of the underlying bed will produce the liquefaction, the absolute standing wave that form the front of the structure may bring 6. 16 meter depth of the liquefaction, so the foundation of structure will lose part of the supporting force, the structure will slide in this situation. that is to say, because of the foundation partly liquefaction, the exist of soft layer and the component force of gravity, the structure slide further to the basin and collapse, which leads to disastrous consequence

    在強暴風浪下，底床表層1 . 75米以上均有可能產生液化現象，而在構築物前形成的完全駐波，甚至能夠造成6 . 16米的液化深度，構築物地基部分失去支持力，將直接導致構築物的滑動，也就是說，在地基部分液化、軟弱層的存在以及構築物沿坡重力分力的共同影響下，構築物將向「盆」底方向發生更大的滑動，甚至可能發生倒塌。
  11. In fact, the constitutive models employed in both methods could not re - produce the dynamic behaviour of soil to non - proportional cyclic loading, such as waves loading. to simulate dynamic responses of elastic, visco - elastic and elasto - plastic sea beds, linear and / or non - linear numerical models based on generalized biot ' s theory are developed together with stable and effective algorithm. the difficulty in numerical computation made the generalized biot ' s theory be difficult to be put into practice in the field of geotechnical engineering

    上述兩種方法採用的土體本構模型都不能再現砂土在暴風浪等非比例加載條件下的動力特性，本文基於廣義biot理論提出了波浪作用下海床線性或非線性動力響應的耦合計算模型與穩定、高效數值演算法，分別針對土的彈性、粘彈性與彈塑性本構關系，對海床的動力響應進行了有限元數值模擬與分析。
  12. It also make the set - up occurs. 4 ) the sea level and current velocity have an effect on wave height, and the wave direction modulation is small

    4 、潮汐、風暴潮對波浪的作用是通過其產生的不定常水深與流場實現的；水深與流速對波向的影響很小。
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