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首页> 外文期刊>Geophysical Research Letters >Low altitude quasi-periodic radar echoes observed by the Gadanki VHF radar - art. no. 1530
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Low altitude quasi-periodic radar echoes observed by the Gadanki VHF radar - art. no. 1530

机译:Gadanki VHF雷达观测到的低空准周期雷达回波-艺术没有。 1530

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1] We report here on the low altitude quasi-periodic (LQP) radar echoes from low latitude sporadic E layer (Es) observed by the Gadanki (13.5degreesN, 79.2degreesE; geomagnetic latitude 6.3degreesN) VHF radar. The LQP echoes occurred both during daytime and nighttime and are confined to a slowly descending layer with a thickness of about 2-4 km in the height range of 90-100 km. The periods are found to range from tens of seconds to less than about 3 minutes. The Doppler velocities vary over a range of - 20 to +20 m/s during daytime and 0 to 10 m/s during nighttime and are known to be sensitive to the layer height, being dominated by the effect of zonal electric field above and meridional neutral wind below a height of similar to 97 km for the type 2 irregularities [Krishna Murthy et al., 1998]. The spectral widths are found to be of the order of 50 to 75 m/s during daytime and 30 to 60 m/s during nighttime. The LQP echoes reported here are similar to that observed recently over midlatitudes [Rao et al., 2000; Urbina et al., 2000], but distinctly different from the widely reported quasi-periodic (QP) echoes occurring at higher altitudes (> 100 km). The observations are discussed briefly in terms of the potential source mechanisms. [References: 21
机译:1]我们在此报告由Gadanki(13.5°N,79.2°E;地磁纬度6.3°N)VHF雷达观测到的低纬度零星E层(Es)产生的低空准周期(LQP)雷达回波。 LQP回波在白天和夜间都发生,并被限制在90-100 km高度范围内厚度约2-4 km的缓慢下降层中。发现周期范围从几十秒到少于大约3分钟。白天的多普勒速度在-20至+20 m / s的范围内变化,夜间则在0至10 m / s的范围内变化,已知对层高敏感,主要受上方和子午经纬向电场的影响对于2型不规则现象,高度低于97 km的中性风[Krishna Murthy等,1998]。发现光谱宽度在白天约为50至75m / s,而在夜间约为30至60m / s。此处报道的LQP回波与最近在中纬度观测到的回波相似[Rao等,2000; Urbina et al。,2000],但与在较高高度(> 100 km)发生的准周期性(QP)回波明显不同。根据潜在的源机制简要讨论了这些观察结果。 [参考:21

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