碎波線 的英文怎麼說

中文拼音 [suìxiàn]
碎波線 英文
breaker line
  • : 動詞[書面語] (觸; 撞) strike; bump
  • : 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...
  • : 名詞1 (用絲、棉、金屬等製成的細長的東西) thread; string; wire 2 [數學] (一個點任意移動所構成的...
  1. In section one, by using fice scheme and time - gcm, a model of trace gases and oh airglow affected by gravity wave is set up, then the propagation of nonlinear gravity wave and the effect on trace gases and oh airglow are analyzed. the result shows gravity wave excited by tropospause forcing can propagate stably to the mesosphere through the stratosphere so that energy and momentum can be transferred from one region to another. in this process, gravity wave undergoes growth, overturning, convection and breaking

    在第一部分的工作中,利用全隱歐拉格式和全球熱層-電離層-中間層-電動力學環流耦合模式( time - gcm ) ,對重力的非性傳播及其在傳播過程中對中高層大氣中氧族和氫族成分和與之密切相關的oh氣輝輻射的影響進行了數值模擬,結果表明,從對流層向上傳播的重力經歷了產生、發展、飽和、對流產生直至破的非性演化,大氣的非等溫結構加速了重力在中層頂區的破,重力的非性傳播是小尺度對流和湍流產生的一個重要的源。
  2. Under the assumption of linear ocean waves, and in the light of the theoretical framework about the probabilistic distribution of wave characteristics ( sun fu 1988 ), several probabilistic distributions of wave characteristics that is necessary for the estimation of breaking probability and whitecap coverage are derived. afterwards, the models of breaking probability and whitecap coverage are set up with these distributions in addition to the kinematical criterion

    性海浪假設下,基於孫孚( 1988 )關於三維海浪要素統計分佈的理論框架,具體給出二維海浪峰處質點水平速度和表觀相速的聯合分佈等分佈函數,在此基礎上,根據運動學判據,分別建立起風浪破率和白浪覆蓋率的理論模式。
  3. And the no - isothermal structure can accelerate the breaking of gravity wave in mesospause, and the breaking of gravity wave is an important source of convection and small - scale waves. the propagation of gravity wave will affect the distribution of minor species. the breaking of gravity wave accelerates the downward transport of atomic oxygen, some smaller - scale structures appear on the horizontal distribution of atomic oxygen number density, and other chemical species are also affected due to the chemical reaction with atomic oxygen and the propagation of gravity wave

    在重力的傳播過程中,氫氧大氣成分的水平和垂直分佈均受到了不同程度的影響,以氧原子的響應最為明顯,而其中重力在氧原子水平分佈上的反應則是非性重力過程的一個重要表現;另外,分析顯示,重力的非性傳播對oh氣輝的峰值分佈由明顯影響,小尺度重力的傳播有時會引起oh氣輝出現奇異的雙峰分佈,重力的破現象也可以從對氣輝的觀測中反映應出來,這對利用氣輝觀測研究重力傳播特性有非常重要的指示意義。
  4. Based on the nonlinear parabolic approximate wave reflection - diffraction equation of mild slope, a model of wave propagation on a fan - shaped coordinate is put forward considering winds, bottom friction and wave breaking, etc. the existing calculation shows that the model can be employed to determine wave fields in large water areas

    接著以非性的拋物型近似浪緩坡方程為基礎,提出了扇形坐標下的浪傳播模型,模型包括了風、底摩阻、浪破等因素的影響,可以用於大水域的浪場的確定;文章最後介紹了一些計算算例。
  5. It is showed by numerical calculation that the waves amplify becomes great and the width of waves becomes narrow after the collision or chase of two solitary gravitational waves. the results indicate that the nonlinear interaction between the gravitational waves may be one of the causes for outbreak of severe convective weather. furthermore, by comparing once shear with second shear, we find that it is easier to breaking up or energy dispersion for the solitary gravitational waves by the nonlinear action when the distributing of basic flow is once shear

    引入實際基本氣流,分別討論了具有垂直一次切變和二次切變流時兩個非性重力相互作用的數值計算過程,得到兩個重力包相遇或相追都會使包的振幅增加、寬變窄;進一步分析表明,有高空急流存在的條件下,非性重力的相互作用更易使包破、能量頻散,激發強對流天氣的形成。
  6. Finally, we rebuild a soft x - ray reflectometer in 8 - 30nm region by replacing its metal target with low - debris kr and xe aerosol spray targets. reflectivity of soft x - ray multilayer mirrors are measured by the new reflectometer, and the results show the accuracy is about 2 % %

    最後,用低屑液體微滴噴射靶lpp光源代替污染嚴重的金屬靶lpp光源,改建了一臺段范圍8 30nm的軟x射反射率計,並對軟x射多層膜的反射率進行了大量測量,反射率測量重復性達到2 。
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