The Simplified Ionospheric Regional Model (SIRM) for HF Prediction: Basic Theory, Its Evolution and Applications

• Published in: Surveys in geophysics Vol. 41; no. 5; pp. 1143 - 1178
• Main Authors: Pietrella, M., Pezzopane, M., Zolesi, B., Cander, Lj. R., Pignalberi, A.
• Format: Journal Article
• Language: English
• Published: Dordrecht Springer Netherlands 01.09.2020; Springer Nature B.V
• Subjects: Algorithms; Astronomy; Critical frequencies; Earth and Environmental Science; Earth Sciences; Electron density; F 2 region; F region; foF2; Geophysics; Geophysics/Geodesy; Ionosphere; Ionospheric electron density; Ionospheric electrons; Ionospheric layers; Ionospheric models; Nowcasting; Observations and Techniques; Prototypes; Regional development; Research projects; Synthesis; SIRMUP; F2; SIRM; Regional modelling
• ISSN: 0169-3298; 1573-0956
• DOI: 10.1007/s10712-020-09600-w

This paper is a final review of the Simplified Ionospheric Regional Model (SIRM) developed as a prototype in the early 1990s and improved in the following years. By means of an algorithm based on the Fourier synthesis, the SIRM model in its prototype version provides predicted monthly median values of the main ionospheric characteristics such as: the ordinary wave critical frequencies ( fo E, fo F1, and fo F2) of the E, F1, and F2 ionospheric layers; the lowest virtual height ( h’ F) of the ordinary trace of the F region; the obliquity factor for a distance of 3000 km ( M (3000)F2). Instead, the improved version focuses only on fo F2 and M (3000)F2. The SIRM model has been largely employed in the framework of different international research projects as the climatological reference to output fo F2 and M (3000)F2 monthly median predictions, but in its SIRMUP version is used also as a nowcasting model and as an intermediate step of complex procedures for a near real-time three-dimensional representation of the ionospheric electron density. In this regard, some results provided by both SIRM and SIRMUP for telecommunication applications are shown. Moreover, the mathematical treatment concerning both the phase correction of the Fourier synthesis and the fundamental steps carried out to define the SIRM algorithm in its final version, never published so far, will be described in detail in dedicated Appendices. Finally, for the first time the SIRM code is now downloadable for the benefit of users.