摘要:To study the modulation mechanism of traveling planetary wave ionospheric disturbances ( TPWIDs) on F layer during pre-reversal enhancement ( PRE) and its effect on the formation and development of spread F ( SF) , in this paper, the characteristics of planetary wave disturbance is analyzed during the high SF season in china′s low latitude region, and the influence of TPWIDs phase on the formation and development of SF is investigated by the method that TPWIDs are used to refer to oscillation of the true height, which is the day-to-day variability and one of the ionosphere characteristic parameters obtained from ionogram observed by Digital Portable Sounder 4d(DPS-4D) ionosonde at sanya in 2012. The results show that TPWIDs-type oscillations controlling the strength of the electric field during PRE, therefore, slowly push the F layer height up and down according to the TPWIDs phase in the geomagnetic quiet period. the occurrence of SF is strongly controlled by the change of post-sunset F layer height and the altitude of 250 km may be a threshold at sanya, so when the the electric PRE causes the F layer bottom side to reach heights above 250 km, it is conducive to generate SF. Also during equinox ( March, April, September and October) the onset time of SF is modulated by the TPWIDs phase in such way that, when the phase greater, SF occurs earlier and when the phase smaller, SF occurs later or no SF.%為研究在日落后反轉增強( PRE)期間行進式行星波電離層擾動( TPWIDs)對F層的調制機制以及對擴展F(SF)形成和發展的作用,利用三亞地區DPS-4D數字測高儀2012年探測的34080張數字頻高圖數據,獲取了電離層特性參數-真高,以真高的逐日變化表征行進式行星波擾動,分析了中國低緯地區SF高發季節中行星波擾動特性,并研究了行星波擾動時的不同相位對SF產生和發展的影響。結果表明:地磁平靜時期,在PRE期間,TPWID行星波擾動調制著PRE時期的電場強度,根據其相位的不同能導致F層的高度上抬或下降;日落后F層高度的變化控制著SF的發生,在三亞地區真高閾值大約為250 km,即當PRE導致F層高度上抬到大于250 km時,有利于SF產生;并且在分點季節(3月,4月,9月和10月),TPWID行星波相位也調制著SF的開始時間,即TPWID相位越大, SF發生的越早,TPWID相位越小,SF發生的越晚甚至不發生。