武汉上空(30°N,114°E)潮汐及其相互作用的MF雷达观测
doi: 10.11728/cjss2003.06.20030604 cstr: 32142.14.cjss2003.06.20030604
MF RADAR OBSERVATIONS OF TIDES AND THEIR INTERACTIONS OVER WUHAN (30°N, 114°E)
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摘要: 利用武汉(30°N,114°E)MF雷达2000年2月11日至25日,以及2月28日至3月13日的观测数据,研究中层顶(80-98 km)区域冬季潮汐振荡及其共振相互作用.水平风场扰动的动态谱显示出在所有的观测高度上都持续存在很强的24 h潮汐波动;偶尔也会出现较强的12 h和弱的8 h潮汐振荡,这说明在中纬地区的冬季, 24 h潮汐是中层顶区域主要的潮汐成分.潮汐振幅及其相关动能随时间的变化表明,在24 h,12 h和8 h潮汐之间可能存在强的共振相互作用.另外,24h潮汐的相位随高度的增加呈现出明显的增加趋势,表明观测到的24h潮汐是向上传播的.由相位剖面计算出24h潮汐纬向和经向风场的垂直波长分别为45km和47km,其向下的相位传播速度分别为1.88km/h和1.97km/h.Abstract: Data obtained from the medium-frequency (MF) radar at Wuhan (30°N, 114°E) from 11 to 25 February and from 28 February to 13 March have been used to study the tidal oscillations and their interactions at mesopause (80-98km) region over Wuhan in winter. A dynamic spectral variation of disturbance amplitude illustrates a prominent peak at a period of 24 hours at all heights and almost uninterrupted, and there are occasionally slightly strong semidiurnal and weak terdiurnal tidal disturbances. These indicate that in the mid-latitude regions, the diurnal tide is the dominant tidal disturbance at mesopause in winter. A detailed analysis of tidal amplitudes and their wave kinematical energies implies that there may be significant resonant interaction among the diurnal, semidiurnal and terdiurnal tides. The phase profiles of the diurnal tides show obvious increase trend with the increasing heights in both the zonal and meridional directions, which indicate that the observed diurnal tides are propagating upward. The mean vertical wavelengths of the diurnal tides obtained from the zonal and meridional phases are 45km and 47km, respectively, and the corresponding downward phase velocities are 1.88km/h and 1.97km/h, respectively.
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Key words:
- MF radar observation /
- Tides /
- Interaction
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