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首页> 外文期刊>Geophysical Research Letters >Daytime 150-km echoes observed with the Equatorial Atmosphere Radar in Indonesia: First results
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Daytime 150-km echoes observed with the Equatorial Atmosphere Radar in Indonesia: First results

机译:印尼赤道大气雷达在白天观测到的150公里回声:初步结果

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摘要

Results of the daytime 150-km echoes from 10.36 degrees S magnetic latitude observed using the Equatorial Atmosphere Radar (EAR), which are first of its kind from magnetic southern hemisphere, are presented. The echoing region of 145-165 km shows forenoon descent and afternoon ascent with signal intensity modulation with time resembling a necklace and the Doppler spectra are narrow, which are quite similar to those reported earlier from other locations. Westward and upward/southward irregularity drifts are found to be consistent with daytime background electric fields, providing a tool to investigate low latitude daytime electrodynamics. Detectability of these echoes suggests the absence of strong latitudinal dependence in contrast to the earlier belief, suggesting a possibility of their detection at mid-latitudes. Also the echoes show zonal anisotropy that is opposite to that observed over Pohnpei. The implications of these observations are discussed in the light of present understanding of 150-km echoing phenomenon.
机译:呈现了使用赤道大气雷达(EAR)观测到的,来自10.36度南纬的白天150公里回波的结果,这是南半球的磁性首次出现。 145-165 km的回波区域显示前下降和午后上升,信号强度的调制时间类似于一条项链,多普勒频谱很窄,这与之前从其他地方报道的情况非常相似。发现向西和向上/向南的不规则漂移与白天背景电场一致,为研究低纬度白天电动力学提供了一种工具。这些回波的可探测性表明,与早期的信念相比,没有强烈的纬度依赖性,这表明在中纬度地区有可能探测到它们。回波也显示出与波恩培上观察到的相反的纬向各向异性。根据目前对150公里回声现象的理解,讨论了这些观测结果的含义。

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