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VHF radar observations of nighttime F-region field-aligned irregularities over Kototabang, Indonesia

机译:甚高频雷达观测印度尼西亚科托班邦夜间F区域场对准的不规则性

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摘要

We report, for the first time, continuous observations of the nighttime F-region field-aligned irregularities (FAIs) over Indonesia. A VHF radar with operating frequency of 30.8 MHz and peak power of 20 kW has been operated at Kolotabang (0.20 degrees S, 100.32 degrees E; dip latitude 10.4 degrees S), Indonesia since February 2006. Five beams were allocated between +/- 54 degrees in azimuth around geographic South (126 degrees-234 degrees). From the Continuous observation from February 2006 to November 2007, we found that FAIs appeared frequently at pre-midnight between March and May and Lit post-midnight between May and August. The pre-midnight FAIs coincided well with GPS scintillation observed at the same site. Seasonal and local time variations of the pre-midnight FAI Occurrence are consistent with those of equatorial plasma bubbles reported in previous studies (e.g., Maruyama and Matuura, 1984). These results indicate that the pre-midnight FAIs could be associated with the equatorial plasma bubbles. On the other hand, seasonal and local time variations of the post-midnight FAIs were inconsistent with those of the plasma bubbles. The features of the post-midnight FAIs can be summarized as follows: (1) The post-midnight FAIs are not accompanied by GPS scintillations. (2) Most of the post-midnight FAI regions do not show propagation, but some of them propagate westward. (3) Echo intensity of the post-midnight FAIs was weaker than that of the pre-midnight FAIs. These features are similar to those of the FAI echoes that have been observed at mid-latitude (e.g., Fukao et, al., 1991). At Kototabang, Fukao et al. (2004) have firstly observed FAIs that resemble those Lit mid-latitude. The present paper reports statistical characteristics of the mid-latitude-type FAIs observed at Kototabang.
机译:我们首次报告了对印度尼西亚上空的夜间F区域场对准不规则现象(FAI)的连续观察。自2006年2月以来,印度尼西亚的Kolotabang(0.20度,E。100.32度;倾角为10.4度)已运行了工作频率为30.8 MHz,峰值功率为20 kW的VHF雷达。在+/- 54之间分配了五个波束地理南部(126度至234度)周围的方位角。从2006年2月至2007年11月的连续观测中,我们发现FAI频繁出现在3月至5月的午夜前和5月至8月的午夜后升。午夜前的FAI与在同一地点观测到的GPS闪烁非常吻合。午夜前FAI发生的季节和当地时间变化与先前研究中报道的赤道血浆气泡的变化一致(例如Maruyama和Matuura,1984)。这些结果表明,午夜前的FAI可能与赤道血浆气泡有关。另一方面,午夜后固定资产投资的季节和当地时间变化与等离子气泡的变化不一致。午夜后FAI的特征可归纳如下:(1)午夜后FAI不伴有GPS闪烁。 (2)大多数午夜之后的固定资产投资区域都没有传播,但其中一些向西传播。 (3)午夜后固定资产投资的回声强度弱于午夜前固定资产投资的回音强度。这些特征与在中纬度观测到的FAI回波相似(例如Fukao等,1991)。在Fotoo等人的Kototabang。 (2004)首先观察到了类似于中纬度的固定资产投资。本文报道了在科塔邦观测到的中纬度固定资产投资的统计特征。

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