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扰动位 meaning in Chinese

disturbing potential

Examples

  1. Based on this characteristic , whether a reference field is used or not has no effects on the ls solution is explained
    在此基础上,根据不同的噪声水平,模拟了4种不同精度的沿轨扰动位观测值。
  2. The characteristics of the normal equation created in recovering the earth gravity model ( egm ) by least - squares ( ls ) adjustment from the in - situ disturbing potential has been discussed in detail
    摘要讨论了在基于能量法确定地球重力场模型的过程中,利用最小二乘方法由沿轨扰动位数据解算位系数时法方程的特性,在该问题中,法方程只与卫星轨道有关。
  3. The numerical results indicate that the deformation within the solid inner core is very small . however , in the fluid outer core , the changes of the displacement with relatively low spherical harmonic degree ( n < 10 ) is very complicated via the radius , due to the resonance near the eigenfrequenies of the core long - period oscillations . while the spherical harmonic degree of the loading is larger than 10 , the deformation and the gravitational perturbation in the core are very small , and the earth ' s deformation response is dominantly represented as the radial displacement in the elastic mantle
    研究了地球在日月引潮力和表面负荷作用下的形变特征,数值计算结果表明,在固体内核中的形变很小,由于在长周期核模本征频率附近的共振,液核中低阶( n 10 )位移随半径的变化非常复杂,当负荷阶数超过10时,地核中的形变和扰动位都很小,地球的响应主要表现为弹性地幔中的径向位移,且随深度增加急剧减弱,地表负荷love数与信号频率的依赖关系很弱,给出了体潮love数计算的一种有效的近似处理方案。

Related Words

  1. 扰动量
  2. 扰动稳定性
  3. 扰动地层
  4. 相位扰动
  5. 结构扰动
  6. 低头扰动
  7. 扰动行星
  8. 轴对称扰动
  9. 扰动误差
  10. 边界扰动
  11. 扰动湍流
  12. 扰动微晶灰岩
  13. 扰动位能
  14. 扰动稳定性
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