Ionospheric profilers using data grids

R. Leitinger , B. Nava , G. Hochegger , S. Radicella
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引用次数: 11

Abstract

Most of the empirical ionospheric models which use maps of ionosonde parameters can be considered to be “profilers” in the sense that they use “anchor points” (e.g., E, F1 and F2 peaks) and provide the height profile of electron density between the anchor points and for the topside of the F layer. We present a modelling approach which replaces the global or regional maps (e.g., the ITU-R maps) by data grids and two dimensional third order interpolation for geographic locations between the grid points. The width of the data grids in latitude and longitude can easily be adapted to the intended use of a profiler, e.g., combination of smaller scale structures with a smooth background. The data grids can be constructed entirely from measured data but also from a combination of maps for monthly averages with measured data. In the latter case it is necessary to use buffer zones around the areas where measured data exist to ensure a smooth interface with the outside grid. We demonstrate the data grid method with several different profilers, especially with the “family” of ionospheric models developed at Graz and Trieste.

使用数据网格的电离层剖面仪
大多数使用电离层探空仪参数图的经验电离层模型可以被认为是“剖面仪”,因为它们使用“锚点”(例如E、F1和F2峰),并提供锚点之间和F层顶部的电子密度高度剖面。我们提出了一种建模方法,用数据网格和网格点之间地理位置的二维三阶插值取代全球或区域地图(例如ITU-R地图)。纬度和经度数据网格的宽度可以很容易地适应剖面仪的预期用途,例如,将较小规模的结构与光滑背景相结合。数据网格可以完全由测量数据构成,也可以由月平均值图与测量数据的组合构成。在后一种情况下,有必要在测量数据存在的区域周围使用缓冲区,以确保与外部网格的平滑接口。我们用几种不同的分析器来演示数据网格方法,特别是在格拉茨和的里雅斯特开发的电离层模型“家族”。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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