inertia wave 中文意思是什麼

inertia wave 解釋
慣性波
  • inertia : n. 1. 【物理學】慣性，惰性，慣量。2. 不活動，不活潑，遲鈍，惰性。3. 【醫學】無力。adj. -less 無慣性的，無慣量的。
  • wave : n 〈美海軍〉女志願軍人〈見 WAVES 條〉。n 1 波浪；碎浪； 〈the wave（s）〉 〈詩〉海。2 波動；波狀...
  1. The southern spread of low - layer inertia - gravity wave was benefited for coming into being of excessive strip rain belt

    低層向南傳播的重力慣性波有利於多條雨帶的形成。
  2. It was benefited for southern spread of inertia - gravity wave in the symmetric instability region of the south of the high layer of rain belt

    高層雨帶南部的對稱不穩定區，有利於重力慣性波的向南傳播。
  3. The northern spread of high - layer inertia - gravity wave could result in the development and northern moving of low - layer vortex and precipitation

    高層向北傳播的重力慣性波可導致低層的渦旋和降水發展和北移。
  4. The north of the low - layer of rain belt was mainly convection instability. so the northern inertia - gravity wave was not easy to develop and to spread

    雨區的北部低層以對流不穩定為主，因此向北的重力慣性波不易發展傳播。
  5. By analyzing the differentiae of the total cross sections ( tcs ), the differential cross sections ( dcs ), the partial wave cross sections ( pcs ), the change patterns of the cross sections and the influence on the cross sections because of the var iations in the mass of systems and the relative kinetic energy of incoming atoms for symmetric isotopically substituted systems he, ne, ar, kr, xe - h2, d2, t2 have been obtained. in this paper, we use the tang - toennies potential model for the inertia gas atoms - h2 systems, the murrell - sorbie potential surface with five parameters for the molecules h2, d2, t2. for the inertia gas atoms - d2, t2 systems, we use the same potential surface with the inertia gas atoms - h2 systems

    通過分析he 、 ne 、 ar 、 kr 、 xe ? h _ 2 、 d _ 2 、 t _ 2各碰撞體系在總截面、微分截面和分波截面等方面的差異，總結出在h _ 2分子的對稱同位素替代情形下惰性氣體原子與h _ 2分子體系碰撞截面的變化規律；通過比較he 、 ne 、 ar 、 kr 、 xe ? h _ 2 、 d _ 2 、 t _ 2各體系在碰撞總截面、微分截面、分波截面等方面的不同，詳細討論了同位素替代碰撞體系中體系約化質量及入射原子的相對碰撞能量的變化對碰撞截面的影響，得出了這種影響的規律性。
  6. The moment of inertia, damp and comeback can be adjusted. two electro - hydraulic servo systems analog rolling moment and swaying force of wave respectively. the two systems both use electro - hydraulic servo valves, in which the analog rolling moment system adopts gear - rack swing hydraulic - pressure oil vat with torque sensor, while the analog swaying force system employs double shanks hydraulic - pressure oil vat with two pressure sensors and a placement sensor

    兩套電液伺服系統均使用流量電液伺服閥（採用外供油方式） ，其中模擬橫搖力矩的伺服系統採用齒輪齒條擺動液壓油缸，配有扭矩傳感器，模擬橫蕩力的伺服系統採用雙出桿液壓油缸，配有兩個壓力傳感器和一個位移傳感器。
  7. We analyzed the meso - scale disturbance field and found that the development and spread of inertia - gravity wave had a close relationship with the development and spread of the rain belt. at the initial stages of precipitation, convection instability was strong in the low level above rain region. convection instability could inspire inertia - gravity wave

    對中尺度擾動場分析發現重力慣性波的發展和傳播與雨帶的發展與傳播有密切的聯系：在降水初期，雨區上空低層的對流不穩定較強，對流不穩定可激發出重力慣性波。
  8. Furthermore using the variation principle in the elasticity, the wave - motion equation is derived in the finite deformation elastic thin rod with viscous and transverse inertia effects, and the characteristic curves and their characteristic relations are obtained by characteristic line method, and the influence of viscous and geometrical - dispersive effects on the propagation of wave is analyzed

    再利用彈性力學中的變分原理，導出了同時計及粘性和橫向慣性效應時的彈性細桿的幾何非線性波的波動方程，用特徵線法得到它的特徵線和特徵線上的相容關系，分析了粘性耗散和幾何彌散效應對波的傳播速度的影響。
  9. In these equations, the compression wave propagation and the transverse inertia effect were taken into consideration

    通過引入圓柱殼動力失穩時的波前約束條件實現了此類問題的有限元特徵值解法。
  10. In this paper, the multi - scale technology is introduced to study the wave - motion equations with viscous or transverse inertia effects or both of them. burgers equation, k - dv equation and kdv - burgers equation are deduced respectively, and correspondingly the steady shock - wave solutions, solitary wave solutions and oscillation solitary wave or shock - wave solutions are obtained

    接著，又採用奇異攝動理論中的多尺度變換法分析並簡化了分別計入粘性、橫向慣性效應以及同時計入這兩種因素時的幾何非線性波的波動方程，分別得到了經典的burgers方程、 k - dv方程和kdv - burgers方程；並求出它們相應的穩態解分別為激波解、孤波解和振蕩孤波解或激波解。
  11. In the metaphase of precipitation, the high - layer inertia - gravity wave presented indirect circulation posture circling the center of low - layer vortex. at this time precipitation became stronger and moved towards the east

    在降水的中期，高層的重力慣性波出現圍繞低層渦旋中心逆時針旋轉的形勢，此時降水開始加大並東移。
  12. The appearance of southern spread of inertia - gravity wave in high layer was earlier than the one in low layer. the vorticity and divergence belt take on eight as time processes. the high - layer northeast - southwest vorticity and divergence belt spread towards the south and northwest - southeast vorticity and divergence belt spread towards the north

    渦度、散度帶隨時間出現八字形分佈，高層東北?西南向的渦度、散度帶有向南的傳播，西北?東南向的渦度、散度帶有向北的傳播。
  13. So we found that convection instability could inspire inertia - gravity wave. symmetry instability was benefited for spread of inertia - gravity wave and further influenced the development and motion of precipitation

    可見對流不穩定可激發重力慣性波，對稱不穩定可使重力慣性波發展與傳播，從而影響到降水的發展與活動。
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