TGR-foF2: TEC-Driven Graph-Based Spatial Reconstruction of Continuous foF2 Fields with Physics-Guided Learning

Dandan Che;Ying Li;Wenshuai Wang;Yuanhao He;Yi Gong
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Abstract

Spatial reconstruction of the ionospheric F2-layer (foF2) critical frequency is essential for high-frequency communication and ionospheric modeling, yet remains challenging due to the sparse distribution of ground-based ionosondes. This paper proposes a graph attention network framework that reconstructs spatially continuous foF2 fields by treating global navigation satellite system (GNSS) total electron content (TEC) as a direct spatial covariate, bypassing intermediate conversion steps. The framework is named TEC-driven graph-based spatial reconstruction of continuous foF2 fields (TGR-foF2). Each ionosonde station is modeled as a graph node with co-located TEC, coordinates, and solar-geomagnetic features; three physically motivated edge types (geographic proximity, TEC similarity, geomagnetic latitude conjugacy) govern inter-station message passing; and a physics-guided output head encodes the first-order physical scaling between foF2 and the square root of TEC while learning residual corrections. Evaluated via leave-one-station-out cross-validation across eight Australian stations using 2020 full-year data, TGR-foF2 achieves a mean root mean squared error (RMSE) of 0.840 MHz, outperforming inverse distance weighting (0.912 MHz, −7.9%), IRI-2020 (0.976 MHz, −13.9%), and polynomial TEC-to-foF2 conversion (1.227 MHz, −31.5%). Ablation experiments confirm that TEC features, graph topology, and the attention mechanism are the three most impactful components. The strong correlation between station isolation distance and RMSE (r = 0.886, p = 0.003) identifies network sparsity as the primary remaining limitation.
TGR-foF2:基于tec驱动图的连续foF2场空间重构与物理引导学习
电离层f2层(foF2)临界频率的空间重建对于高频通信和电离层建模至关重要,但由于地面电离层探空仪的稀疏分布,仍然具有挑战性。本文提出了一种图关注网络框架,将全球导航卫星系统(GNSS)总电子含量(TEC)作为直接的空间协变量,绕过中间转换步骤,重构空间连续的foF2场。该框架被命名为基于tec驱动图的连续foF2域空间重构(TGR-foF2)。将每个电离层探空站建模为一个图节点,该节点具有共同定位的TEC、坐标和太阳地磁特征;三种物理驱动的边缘类型(地理邻近、TEC相似、地磁纬度共轭)控制着站间信息的传递;物理导向输出头在学习残差校正的同时编码foF2和TEC平方根之间的一阶物理缩放。通过对8个澳大利亚站点使用2020年全年数据的留一站交叉验证进行评估,TGR-foF2的平均均方根误差(RMSE)为0.840 MHz,优于反向距离加权(0.912 MHz,−7.9%)、IRI-2020 (0.976 MHz,−13.9%)和多项式TEC-to-foF2转换(1.227 MHz,−31.5%)。消融实验证实,TEC特征、图拓扑和注意机制是三个最具影响力的组成部分。站点隔离距离与RMSE之间的强相关性(r = 0.886, p = 0.003)表明网络稀疏性是剩余的主要限制。
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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