Variation of foF2 during low and high solar activity over Thailand equatorial latitude station

N. Wichaipanich
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Abstract

This paper presents the variation of the F2 layer critical frequency (foF2) in different phases of the 24th solar cycle at Thailand equatorial latitude station, namely Chumphon (10.72°N, 99.37°E and magnetic dip 3.3°N). Monthly median of foF2 values every 15 minutes in March, June, September and December are manually scaled from the FM-CW ionosonde of the year 2009 and 2014 for investigating the diurnal and seasonal variation during low and high solar activity. The observed foF2 results show a similar feature in diurnal and seasonal variations with higher during daytime, lower during nighttime. The maximum values occur during equinox (March and September) seasons while the minimum levels occur in solstice (June and December) seasons. The advantages of this study are much important for understanding, managing and designating the HF communication systems. Furthermore, it can be used to improve the ionospheric model and map at the magnetic equator.
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泰国赤道纬度站太阳活动低峰和高峰期间foF2的变化
本文研究了泰国赤道纬度站Chumphon(10.72°N, 99.37°E,磁倾3.3°N)第24太阳周期不同阶段F2层临界频率(foF2)的变化。在2009年和2014年3月、6月、9月和12月,每15分钟的foF2值的月中位数是由FM-CW电离空探空仪手动换算的,用于研究太阳活动低峰和高峰期间的日变化和季节变化。观测到的foF2在日变化和季节变化中表现出相似的特征,即白天较高,夜间较低。最大值出现在春分(3月和9月)季节,最小值出现在冬至(6月和12月)季节。本研究的优点对于了解、管理和指定高频通信系统具有重要意义。此外,它还可用于改进磁赤道电离层模型和地图。
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