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Effects of high-latitude atmospheric gravity wave disturbances on artificial HF radar backscatter

机译:高纬大气重力波干扰对人造HF雷达反向散射的影响

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摘要

Observations of HF radar backscatter from artificial field-aligned irregularities in an ionosphere perturbed by travelling disturbances due to atmospheric gravity waves are presented. Some features of the spatio-temporal structure of the artificial radar backscatter can be explained in terms of the distortion of the ionosphere resulting from the travelling disturbances. The distorted ionosphere can allow the HF pump wave to access upper-hybrid resonance at larger distances from the transmitter than are normally observed and can also prevent the pump wave reaching this resonance at close distances. The variation in altitude of the irregularities sometimes results in a significant variation in the elevation angle of arrival of the backscattered signal at the radar implying that the radar "sees" a target moving in altitude. We suggest that this may be evidence of off-orthogonal scattering from the irregularities.
机译:提出了由电离层中人工场对准的不规则性引起的HF雷达反向散射的观测,电离层中的不规则性受到大气重力波引起的行进干扰的干扰。人造雷达后向散射的时空结构的某些特征可以用行进干扰引起的电离层畸变来解释。变形的电离层可以使HF泵浦波在距发射器的距离比通常观察到的距离大的情况下进入上混合共振,并且还可以防止泵浦波在近距离处达到该谐振。凹凸不平的高度变化有时会导致后向散射信号到达雷达的仰角的显着变化,这意味着雷达“看到”了一个在高度上运动的目标。我们建议这可能是来自不规则现象的正交偏移的证据。

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