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Simultaneous observations of F_2 layer stratification and spread F at postmidnight over a northern equatorial anomaly region

机译:同时观察₂层F在postmidnight分层和传播北赤道异常区

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Simultaneous observations of F_2 layer stratification and spread F at postmidnight (00:00 LT to 05:00 LT) were carried out on 22, 23, and 28 November 2013, using ionosondes distributed over a northern equatorial anomaly region at three specific locations, i.e., Puer (PUR, 22.7°N, 101.05°E, dip latitude 12.9°N), Chiang Mai (CMU, 18.8°N, 98.9°E, dip latitude 9.04°N), and Chumphon (CPN, 10.7°N, 99.4°E, dip latitude 0.93°N). The results show that both the PUR and CMU stations observed the F_2 layer stratification at postmidnight in the Northern Hemisphere, frequently accompanied with gravity waves (the periods~30–100min). It is reported that F_2 layer stratification at postmidnight can be observed in the Northern Hemisphere for the first time. It is suggested that the thermospheric neutral wind triggered by gravity waves strongly contribute to the altitude dependence of the combined vertical plasma velocity, which consequently poses significant impacts on the occurrence of the low-latitude F_2 layer stratification at postmidnight. In addition, the spread F other than F_2 layer stratification was observed at the CPN station located at the geomagnetic equator, suggesting that smaller geomagnetic inclination tend to inhibit the postmidnight F_2 layer stratification in the equatorial region. Furthermore, on 23 November 2013 a good correlation was identified between the F_2 layer stratification at PUR and the spread F at both CMU and CPN, possibly due to that the large-scale gravity waves originating atmiddle latitudes contribute to the nighttime spread F observed in the low-latitude and equatorial regions.
机译:同时观察₂层分层和传播在postmidnight F(LT凌晨00:00 LT) 22日进行,23岁,2013年11月28日,使用ionosondes分布在赤道北部异常地区三个具体的地点,例如,普洱茶(PUR 22.7°N, 101.05°E,蘸纬度12.9°N),清迈(CMU、18.8°N, 98.9°E,纬度纬度0.93°N)。PUR和CMU站观测₂层分层postmidnight在北方半球,经常伴随着重力波(时间~ 30 - 100分钟)。在postmidnight₂层分层在北半球的中被观察到已经不是第一次了。thermospheric中性风引起的重力波强烈的高度依赖的垂直的等离子体速度,因此带来了显著对低纬度₂的发生的影响在postmidnight层分层。此外,传播F₂层在尼泊尔共产党车站分层观察位于赤道地磁,暗示较小的地磁倾向往往抑制postmidnight₂层分层在赤道地区。2013年11月一个良好的相关性被发现在PUR₂层分层,之间传播F卡耐基-梅隆和尼共,可能由于大规模的重力波原始atmiddle纬度为夜间作出贡献F在低纬度和传播赤道地区。

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