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(Reference retrieved automatically from Web of Science through information on FAPESP grant and its corresponding number as mentioned in the publication by the authors.)

Linear Vary-Chap Topside Electron Density Model with Topside Sounder and Radio-Occultation Data

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Author(s):
Prol, Fabricio dos Santos [1, 2] ; Themens, David R. [3] ; Hernandez-Pajares, Manuel [2] ; Camargo, Paulo de Oliveira [1] ; de Assis Honorato Muella, Marcio Tadeu [4]
Total Authors: 5
Affiliation:
[1] Univ Estadual Paulista UNESP, Dept Cartog, BR-19060900 Sao Paulo - Brazil
[2] Univ Politecn Cataluna, IOnospher Determinat & Nav Based Satellite & Terr, Dept Math, E-08034 Barcelona - Spain
[3] Univ New Brunswick, Dept Phys, Fredericton, NB - Canada
[4] Univ Vale Paraiba, IP&D, Lab Fis & Astron, BR-12244000 Sao Paulo - Brazil
Total Affiliations: 4
Document type: Review article
Source: SURVEYS IN GEOPHYSICS; v. 40, n. 2, p. 277-293, MAR 2019.
Web of Science Citations: 1
Abstract

The Linear Vary-Chap function has received increased attention in describing the topside ionosphere due to its good performance for predicting and extrapolating radio-occultation (RO) electron density ionospheric profiles. The systematic increase in the scale height is consistent with first principles corresponding to the increase in the electron temperature; however, the altitude where the linear scale height approximation does not stay valid has not been explicitly discussed in the literature. In order to demonstrate up to what extent the linear behavior of the scale height is still valid, this work analyzes more than 50,000 manually scaled ionospheric profiles measured by topside sounders on board Alouette and International Satellites for Ionospheric Studies satellites. Based on this initial analysis, a new topside model is proposed to take into consideration the nonlinear behavior of the topside scale height. The proposed climatological model, a fit of spherical harmonics to parameters derived from topside RO profiles, is used to predict topside sounder measurements. An assessment of the predicted, RO-derived, topside is carried out and the experimental results are discussed in order to show the viability of extrapolating RO ionospheric profiles for altitudes above the low Earth orbit. (AU)

FAPESP's process: 16/22011-2 - Data assimilation for three-dimensional modelling of the ionosphere in Brazil
Grantee:Fabricio dos Santos Prol
Support Opportunities: Scholarships abroad - Research Internship - Doctorate
FAPESP's process: 15/15027-7 - Data assimilation for three-dimensional modelling of the ionosphere in Brazil
Grantee:Fabricio dos Santos Prol
Support Opportunities: Scholarships in Brazil - Doctorate