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中文核心期刊

随机浅海信道中信号场横向相干理论

THEORY OF HORIZONTAL COHERENCE OF SIGNAL FIELD IN SHALLOW-WATER

  • 摘要: 本文将准平面波在随机信道中受到的横向随机扰动考虑为平稳高斯过程,分析计算了均匀浅海信道中由温度微结构及随机起伏界面所引起的信号场横向相干性减弱的情况.在实际感兴趣的“3/2次方”场区,给出大横向距离的相关系数为\beginarrayl R(\infty ) = \exp - Ak_0^2,\\ A \equiv \left \sqrt \pi \mu ^2 ar + 0.3\frac\sigma _H^2Q^2.5\rm\cdot\left( \fracH_0r \right)^1/2 \right, \endarray其中k0为波数,\overline \mu ^2,a为水团参数,σ2H为随机界面的起伏方差,Ω为海底反射损失随掠角变化的平均斜率,H0为平均海深,r为传播距离.

     

    Abstract: The horizontal random perturbation on a qudsi-plane wave field in a random channel was treated as a stationary Gaussian process. The degradation of horizontal coherence in shallow water homogeneous layer due to the influences of micro-structure of water masses and random boundary was calculated for field region of "three-half":\beginarrayl R(\infty ) = \exp - Ak_0^2,\\ A \equiv \left \sqrt \pi \mu ^2 ar + 0.3\frac\sigma _H^2Q^2.5\rm\cdot\left( \fracH_0r \right)^1/2 \right, \endarrayherek0 is wave number ;\overline \mu ^2 and a are parameters of micro-structure, O2H is the standard deviation of the fluctuated boundary,H0is the average water depth, r is the transmission range and Q is the parameter of bottom loss.

     

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