A technique to reconstruct the electron density of the ionosphere starting from total electron content values has been developed using the NeQuick ionospheric electron density model driven by its effective ionization parameter Az. The technique is based on the computation of Az values for a suitable worldwide grid of points. A simple way to obtain relevant Az grids is to use global vertical Total Electron Content (TEC) maps to define for each grid point as Az value, the one that minimizes the difference between the experimental and the modeled vertical TEC. Having a global grid of Az values it is possible to compute the electron density at any point in the ionosphere using NeQuick. As a consequence, slant TEC values for specific ground stat...
Presented is a new method for retrieving the topside electron density distribution from space-based ...
International audienceThe reconstruction of the vertical electron-density profile is a fundamental p...
The ionosphere is the upper part of the atmosphere where sufficient free electrons exist to affect t...
A technique to reconstruct the electron density of the ionosphere starting from total electron conte...
A technique to reconstruct the electron density of the ionosphere starting from total electron conte...
A technique to reconstruct the electron density of the ionosphere starting from total electron conte...
Ground-based ionosphere sounding measurements alone are incapable of reliably modeling the topside e...
New formulae based on the Sech-squared, Exponential and Chapman layers are introduced for a TEC-base...
Presented is a new operational model for real-time reconstruction of the vertical electron density d...
The reconstruction of the vertical electron-density profile is a fundamental problem in ionospheric ...
The reconstruction of the vertical electron-density profile is a fundamental problem in ionospheric ...
The reconstruction of the vertical electron-density profile is a fundamental problem in ionospheric...
The tomographic reconstruction technique generates a two-dimensional latitude versus height electro...
An electron density model, which permits a three-dimensional specification of the ionospheric struct...
New methods to generate global maps of the F2 layer peak electron density of the ionosphere (NmF2) a...
Presented is a new method for retrieving the topside electron density distribution from space-based ...
International audienceThe reconstruction of the vertical electron-density profile is a fundamental p...
The ionosphere is the upper part of the atmosphere where sufficient free electrons exist to affect t...
A technique to reconstruct the electron density of the ionosphere starting from total electron conte...
A technique to reconstruct the electron density of the ionosphere starting from total electron conte...
A technique to reconstruct the electron density of the ionosphere starting from total electron conte...
Ground-based ionosphere sounding measurements alone are incapable of reliably modeling the topside e...
New formulae based on the Sech-squared, Exponential and Chapman layers are introduced for a TEC-base...
Presented is a new operational model for real-time reconstruction of the vertical electron density d...
The reconstruction of the vertical electron-density profile is a fundamental problem in ionospheric ...
The reconstruction of the vertical electron-density profile is a fundamental problem in ionospheric ...
The reconstruction of the vertical electron-density profile is a fundamental problem in ionospheric...
The tomographic reconstruction technique generates a two-dimensional latitude versus height electro...
An electron density model, which permits a three-dimensional specification of the ionospheric struct...
New methods to generate global maps of the F2 layer peak electron density of the ionosphere (NmF2) a...
Presented is a new method for retrieving the topside electron density distribution from space-based ...
International audienceThe reconstruction of the vertical electron-density profile is a fundamental p...
The ionosphere is the upper part of the atmosphere where sufficient free electrons exist to affect t...