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foF2 long-term trends at the southern crest of the equatorial anomaly

机译:赤道距平南顶的foF2长期趋势

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Long-term trends in the electron density of the ionosphere for the period 1957-1986 is studied using foF2 monthly median hourly data measured at Tucuman (26.9 degrees S, 65.4 degrees W), a station located at the southern crest of the equatorial anomaly. The linear trend for each hour and each month is estimated after filtering out the effects of solar activity. For the intervals 0-2 LT and 9-23 LT, during equinoxes and summer solstice, the trend is negative. Statistically null or slightly positive trends are observed for the interval 3-8 LT for every season, and for every hour of winter months. The daily amplitude of foF2 decreases since 1957 due to the decreasing trend in the maximum daily values and almost null-trended minimum daily values. A rough estimate, based on the dip angle trend (which in Tucuman has increased during the 30-year interval at a rate of 0.35%/year), indicates that negative foF2 trends should be expected during daytime hours, and positive trends during night-time hours, behaviour observed in the foF2 data here analyzed. (C) 2006 Elsevier Ltd. All rights reserved.
机译:使用在位于赤道异常南部波峰的图库曼(南纬26.9度,西经65.4度)测得的foF2月度中值小时数据,研究了1957-1986年电离层电子密度的长期趋势。在滤除太阳活动的影响之后,估计每小时和每月的线性趋势。在春分和夏至期间,对于区间0-2 LT和9-23 LT,趋势为负。对于每个季节和冬季的每个小时,在3-8 LT的间隔中观察到统计学上零或轻微的积极趋势。 foF2的日振幅自1957年以来一直在下降,这是因为最大日值和几乎零趋势的最小日值的下降趋势。根据倾角趋势(在图库曼地区以30%的时间间隔以0.35%/年的速度增加)进行的粗略估算表明,应预期白天的foF2趋势为负,而夜间的趋势为正。时间小时,此处分析的foF2数据中观察到的行为。 (C)2006 Elsevier Ltd.保留所有权利。

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