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Seasonal dependence of MSTIDs obtained from 630.0 nm airglow imaging at Arecibo

机译:从阿雷西博630.0 nm气辉成像获得的MSTID的季节性依赖性

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摘要

All-sky imaging data of 630.0 nm airglow emissions are used to study the seasonal and solar activity dependence of medium-scale traveling ionospheric disturbances (MSTIDs) over Arecibo, Puerto Rico (18.3° N, 66.7° W, 28° N mag lat). MSTIDs are typical F-region signatures at midlatitudes, yet limited statistical results in the American sector hindered the progress in our understanding of these dynamical structures. This study compiles data from 2002 to 2007 and shows for the first time that optically-determined MSTIDs at Arecibo present a semiannual pattern with peak occurrence at both solstices. In the Japanese longitude sector, a similar pattern has been found, but one with a main peak during local summer. This paper explains the high occurrence rate during local winter at Arecibo via E-layer/F-layer coupling and inter-hemispheric coupling, thus accounting for a consistent morphology between the two longitude sectors.
机译:630.0 nm气辉发射的全天空成像数据用于研究波多黎各阿雷西博(18.3°N,66.7°W,28°N磁纬)上中等尺度电离层扰动(MSTID)的季节和太阳活动依赖性。 MSTID是中纬度地区的典型F区域特征,但美国部门的统计结果有限,阻碍了我们对这些动力结构的理解。这项研究汇总了2002年至2007年的数据,并首次表明,用光学方法测定的Arecibo的MSTID呈半年度模式,且在两个溶胶点均出现峰值。在日本经度地区,也发现了类似的模式,但其中一个在当地夏季达到峰值。本文通过E层/ F层耦合和半球间耦合解释了Arecibo局部冬季的高发生率,从而解释了两个经度扇区之间的形态一致。

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