Abstract
采用武汉(30°N,114°E)MF雷达在2001年冬季的风场观测数据研究中纬度低热层大气潮汐水平风分量之间的相位关系.统一用弧度定义的各潮汐经纬向分量的拟合初相位在三个连续的高度上分别显示出相同的时间变化倾向和相近的相位差,但是在绝大多数观测时间△ψ24和△ψ12准正交,而△ψ8出乎意料地准同相.周日、半日和8 h潮汐经纬向分量的二次相位耦合(QPC)方程被分别估计出来,利用它们相减还得到一个潮汐相位差相关方程.推测的8 h潮汐相位和相位差与相应的观测值很好地符合.在第14个时间窗内,三个潮汐一般表现为椭圆偏振而不是圆偏振或线偏振,但是△ψ24和△ψ12在三个连续的高度上准正交,而△ψ8在92.0和94.0 km上准同相.因此估计的潮汐QPC方程、推导的潮汐相位差相关方程、观测的8 h潮汐准同相相位差以及典型的潮汐偏振图都是观测的周日、半日和8 h潮汐之间真实QPC的反映.
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