首页> 外文会议>2015 1st URSI Atlantic Radio Science Conference >22 July 2009 total solar eclipse induced wave-like-signatures (WLS) in the lower ionosphere: Inferred using VLF observations
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22 July 2009 total solar eclipse induced wave-like-signatures (WLS) in the lower ionosphere: Inferred using VLF observations

机译:2009年7月22日,日食在电离层下部的总波状签名(WLS):使用VLF观测资料推断

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In the present work, we have focused on the generation and detection of solar eclipse caused wave-like-signature (WLS) in the lower ionosphere using VLF navigation signal form NWC (19.2 kHz) VLF transmitter recorded at three low latitude Indian stations Allahabad (Geog. lat., 25.4° N; long. 81.9° E; Geomag. lat. 16.3° N) Varanasi (Geog. lat., 25.3° N; long. 83.0° E; Geomag. lat. 16.03° N) and Nainital (Geog. lat., 29.4° N; long. 79.5° E; Geomag. lat. 20.5° N) located in 100%; 100% and 84 % totality respectively. This work further contributed to the important aspect of generation of wave-like-signature (WLS) in the lower ionosphere during eclipse. The transmitter receiver great circle path (TRGCP) from NWC to observing sites in India intersected totality path and passed through variable ellipse conditions from no eclipse to partial 84% at Nainital and 100% totality at Allahabad and Varanasi. The wavelet analysis shows (Fig. 1) the presence of WLS with period ∼16–64 min during nighttime ∼04:00–06:00 LT at all the stations. However, during eclipse time we have observed variable WLS signature at different stations. At Allahabad with period ∼20–40 min are present after eclipse totality (∼6:30–07:20 LT) whereas at Varanasi, nighttime WLS were continued during eclipse duration (up to ∼7:20 LT). But no WLS were seen at Nainital during eclipse period despite 84% totality. The presence of WLS during night hours could be interpreted due to nighttime lower ionospheric variability which causes discontinuity/irregularities in lower ionospheric parameters such as temperature, electron density. The WLS during eclipse time have similar features as seen during nighttime and hence could be generated by sudden cutoff of the photoionization creating nighttime like conditions in the D region ionosphere and solar eclipse induced gravity waves. But variability in W- S features at different stations suggest that their observations at given station depend on the various factors such as location, day-night conditions, geometry of eclipse, eclipse magnitude, totality duration and TRGCP length, path direction.
机译:在目前的工作中,我们专注于使用三个低纬度印度台站阿拉哈巴德记录的NWC(19.2 kHz)VLF发射机的VLF导航信号在下电离层中产生和检测日食引起的波状信号(WLS)。纬度,北纬25.4°;东经81.9°;纬度北纬16.3°)瓦拉纳西(纬度,南纬25.3°;东经83.0°;纬度北纬16.03°)和奈尼塔尔(位于纬度29.4°N;纬度79.5°E;地磁纬度20.5°N)位于100%;总计分别为100%和84%。这项工作进一步促进了日食下层电离层中产生波状签名(WLS)的重要方面。从NWC到印度观测站的发射器接收器大圆路径(TRGCP)与总路径相交,并经过各种椭圆条件,从无食到奈尼塔尔的84%,在阿拉哈巴德和瓦拉纳西达到100%。小波分析表明(图1),在所有测站的夜间〜04:00-06:00 LT,存在WLS的时间为〜16-64 min。但是,在日食期间,我们在不同的站点观测到了可变的WLS签名。在全月蚀之后(约6:30–07:20 LT)出现在阿拉哈巴德,时间约为20–40分钟,而在瓦拉纳西,蚀期间持续夜间WLS(直至LT〜7:20)。尽管占总数的84%,但在日食期间奈尼塔尔仍未见到WLS。夜间WLS的存在可能是由于夜间电离层较低的可变性而引起的,这会导致较低的电离层参数(例如温度,电子密度)不连续/不规则。日食期间的WLS具有与夜间相似的特征,因此可能是由于光电离的突然截止而产生的,类似于D区电离层和日食引起的重力波,从而在夜间产生了类似的条件。但是不同站点的W-S特征的可变性表明,它们在给定站点的观测取决于各种因素,例如位置,昼夜条件,日食的几何形状,日食大小,总持续时间和TRGCP长度,路径方向。

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