Open AccessHigh‐Resolution 3‐D Imaging of Daytime Sporadic‐E Over Japan by Using GNSS TEC and Ionosondes
Author(s) -
Fu Weizheng,
Ssessanga Nicholas,
Yokoyama Tatsuhiro,
Yamamoto Mamoru
Publication year - 2021
Publication title -
space weather
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.254
H-Index - 56
ISSN - 1542-7390
DOI - 10.1029/2021sw002878
Subject(s) - tec , gnss applications , daytime , empirical orthogonal functions , ionosonde , geology , total electron content , geodesy , algebraic reconstruction technique , ionosphere , remote sensing , sporadic e propagation , middle latitudes , meteorology , geography , computer science , climatology , iterative reconstruction , global positioning system , electron density , physics , artificial intelligence , geophysics , telecommunications , atmospheric sciences , quantum mechanics , electron
A novel two‐step three‐dimensional (3‐D) computerized ionospheric tomography (CIT) technique has been developed to image the structure of daytime midlatitude sporadic‐E ( E s ). The CIT relies on total electron content (TEC) from a dense ground‐based Global Navigation Satellite System (GNSS) receiver network over the Japan area. First, on a coarse grid, the TEC data and a multiplicative algebraic reconstruction technique (MART) are used to reconstruct the F region from a smooth background. Then, on a fine grid and using singular value decomposition (SVD), the residues after deducting the F region contribution to TEC are utilized in reconstructing the E region, extending 80–180 km in altitude. To vertically constrain the E region solution, we introduced a family of subsets of time‐dependent empirical orthogonal functions (EOFs) from a Chapman model function tuned to manually scaled ionosonde observations. We analyzed three event days to validate the results. East‐West (E‐W) aligned frontal structures, spanning several hundred kilometers, migrating northward in the morning and southward in the afternoon, were observed. The new technique effectively tracks the E s ‐height variation over time, which had proved difficult to reproduce in earlier tempts at 3‐D E s reconstructions.