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首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >Occurrence climatology of F region field-aligned irregularities in middle latitudes as observed by a 40.8MHz coherent scatter radar in Daejeon, South Korea
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Occurrence climatology of F region field-aligned irregularities in middle latitudes as observed by a 40.8MHz coherent scatter radar in Daejeon, South Korea

机译:韩国大田40.8MHz相干散射雷达观测到的中纬度F区域与野外对准的不规则气候

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A new 40.8 MHz coherent scatter radar was built in Daejeon, South Korea (36.18°N, 127.14°E, dip latitude: 26.7°N) on 29 December 2009 and has since been monitoring the occurrence of field-aligned irregularities (FAIs) in the northern middle latitudes. We report on the occurrence climatology of the F region FAIs as observed by the Daejeon radar between 2010 and 2014. The F region FAIs preferentially occur around 250–350km at 18:00–21:00 local time (postsunset FAI), around 350–450 km near midnight (nighttime FAI), around 250–350 km before sunrise (presunrise FAI), and around 160–300 km after 05:00 local time (postsunrise FAI). The occurrence rates of nighttime and presunrise FAIs are maximal during summer, though the occurrence rates of postsunset and postsunrise FAIs are maximal during the equinoxes. FAIs rarely occur during local winter. The occurrence rate of F region FAIs increases in concert with increases in solar activity. Medium-scale traveling ionospheric disturbances (MSTIDs) are known as an important source of the F region FAIs in middle latitudes. The high occurrence rate of the nighttime FAIs in local summer is consistent with the high occurrence rate ofMSTIDs in that season. However, the dependence of the FAI activity on the solar cycle is inconsistent with theMSTID activity. The source of the F region FAIs inmiddle latitudes is an open question. Our report of different types of FAIs and their occurrence climatology may provide a useful reference for the identification of the source of the middle latitude FAIs.
机译:2009年12月29日,在韩国大田(36.18°N,127.14°E,倾角:26.7°N)建造了新的40.8 MHz相干散射雷达,此后一直在监测韩国北中纬度。我们报告了2010年至2014年大田雷达观测到的F区FAI的发生气候。F区FAI优先发生在当地时间18:00-21:00(日落后FAI)大约250-350 km(日落后FAI),大约350-午夜附近450公里(夜间FAI),日出前250-350公里(日出前FAI),当地时间05:00后160-300公里(日出后FAI)。夏季和夜间日出前固定资产投资的发生率最高,而春分期间,未定额和未日出固定资产投资的发生率最高。固定资产投资很少在当地冬季发生。 F区FAI的发生率与太阳活动的增加一致。中等规模的电离层干扰(MSTID)是中纬度F区FAI的重要来源。当地夏季夜间FAI的高发生率与该季节MSTID的高发生率一致。但是,FAI活动对太阳周期的依赖性与MSTID活动不一致。 F地区固定资产投资中间纬度的来源是一个悬而未决的问题。我们关于不同类型的固定资产投资及其发生气候的报告可能为确定中纬度固定资产投资的来源提供有用的参考。

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