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The Variation Characteristics of the Spread-F Occurrences at Chongqing in China

机译:中国重庆散差发生的变化特征

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In the post-sunset ionosphere, plasma depleted bubbles with associated irregularity structures of scale sizes varying from centimeters to kilometers are generated due to plasma instability processes which causes the ionospheric irregularities. Ionospheric spread-F was discovered some decades ago. The variation in spread-F occurrence percentages continues to be an active area for scientific investigations at the present time. The spread-F presents a large dependence on the solar flux, the local time, the season, the latitude and longitude and the magnetic disturbances. In this paper, we present simultaneous ionosonde observations carried out at Chongqing (29.51°N, 106.42°E), which is located at the middle latitude in China, to study the characteristics of spread-F occurrence percentages and variations with local time, season and solar activity during 1997 to 2016. The results show that the onset time of spread-F seems to start at around 20 LT and continue till 05 LT at middle latitude. The spread-F occurs during summer most frequently at Chongqing. The spread-F occurrences decrease with the increase of solar and geomagnetic activity at middle latitude. These observations may improve our understanding of the factors responsible for the generation, growth and dynamics of the middle latitude spread-F events.
机译:在日落后电离层中,由于导致电离层不规则的等离子体不稳定工艺,产生具有相关的尺寸尺寸相关的尺寸尺寸尺寸尺寸尺寸尺寸尺寸结构的等离子体耗尽泡沫。几十年前发现了电离层普遍的差异。传播百分比的变化仍然是目前科学调查的活性区域。扩展F对太阳能通量,当地时间,季节,纬度和经度以及磁干扰呈现大依赖性。在本文中,我们在重庆(29.51°N,106.42°E)上进行了同时进行的同时进行的Ionosonde观察,该观察位于中国中部纬度,研究了普遍发生百分比和当地时间变化的特点,季节和太阳能活动在1997年至2016年期间。结果表明,扩散F的起始时间似乎从20左右开始,并在中纬度下持续到05。在重庆最常见的夏天发生差异。随着中部纬度的太阳能和地磁活动的增加,扩展F发生的发生减少。这些观察可能会改善我们对负责中间纬度蔓延事件的生成,生长和动态的因素的理解。

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