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用南京、射阳的常规探空资料建立了估算折射率结构常数Ｃ２ｎ和湍能耗散率ε垂直变化理论模式。结果表明：用该理论模式计算的ε值与用天气脉冲多普勒雷达探测的速度谱宽σ２ｒ再估算得到的ε值有较好的一致性
Based on the conventional radiosonde data of Nanjing and Sheyang, the theoretical model of vertical variation of refractive index structure constant C2n and turbulent dissipation rate ε was established. The results show that there is a good agreement between the ε value calculated by this theoretical model and the ε value re-estimated by the velocity spectral width σ2r detected by the weather pulsed Doppler radar