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首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >An energy balance study of the lower topside ionosphere using the Arecibo incoherent scatter radar and heating facilities
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An energy balance study of the lower topside ionosphere using the Arecibo incoherent scatter radar and heating facilities

机译:使用Arecibo非相干散射雷达和供暖设施对下顶电离层进行能量平衡研究

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In this paper we describe the results of an experiment to study electron and ion temperature enhancements during an HF modification experiment at the Arecibo Observatory. This experiment is unique in that we pointed the radar away from the interaction region in the F region in order to study heat conduction along the field lines. Although electron temperature enhancements have been frequently observed when high-power radio waves are injected into the ionosphere, observations generally have occurred in the interaction region and the regions of elevated electron temperatures have been accompanied by small ion temperature increases (50–200 K). Like many such experiments, this one was conducted during winter solar minimum, when f 0 F 2 is low during the night at midlatitudes, but this experiment also had the advantage of the upgraded Arecibo HF facility, first used in 1997. The electron temperature enhancements were accompanied by a significant increase in the ion temperature (nearly 500 K). The observation away from the interaction region allowed the application of the time-dependent heating equation without having to estimate local heating effects (i.e., by keeping the conduction and loss terms in the energy balance calculation and neglecting the source term). More specifically, the heating rate of conduction was quantified by manipulating the heat equation. Thus the primary purpose was to observe the temperatures as the heat was conducted away from the F region ionosphere. We have observed the gradients in the electron temperature caused by the heater, estimated the conduction along the field lines, and studied the transfer of energy from the hot electrons to the ions and neutrals. At lower altitudes, near the electron-temperature peak, we show that O+ cooling is dominant, whereas in the lower topside H+ cooling is the most important. Experiments of the type described here could be enhanced with the new dual-beam system at Arecibo in conjunction with a heating facility.
机译:在本文中,我们描述了在Arecibo天文台进行HF改性实验期间研究电子和离子温度升高的实验结果。该实验的独特之处在于,我们将雷达指向远离F区域的相互作用区域,以便研究沿磁力线的热传导。尽管在将高功率无线电波注入电离层时经常观察到电子温度升高,但通常在相互作用区域进行观察,并且在电子温度升高的区域伴有较小的离子温度升高(50-200 K)。像许多此类实验一样,该实验是在冬季最低太阳时进行的,中纬度地区夜间夜间f 0 F 2较低,但该实验还具有升级后的Arecibo HF设备的优势,该设备于1997年首次使用。电子温度提高伴随着离子温度的显着升高(接近500 K)。远离相互作用区域的观察允许应用与时间有关的加热方程式,而不必估计局部加热效应(即,通过在能量平衡计算中保持传导和损耗项而忽略源项)。更具体地,通过操纵热方程来定量传导的加热速率。因此,主要目的是观察热量从F区电离层传导出去时的温度。我们已经观察到了由加热器引起的电子温度梯度,估计了沿磁力线的传导,并研究了从热电子到离子和中性粒子的能量转移。在较低的高度,靠近电子温度峰值,我们表明O +冷却是主要的,而在较低的上侧,H +冷却是最重要的。此处描述的类型的实验可以通过Arecibo的新型双光束系统以及加热设备得到增强。

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