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Python Implementation of European Space Agency's Galileo Ionospheric Model

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Nequick-G

This is a python implementation of the Nequick-G ionospheric correction model described in European Space Agency's Galileo Ionospheric Model. Ionospheric disturbance flags are not implemented

Reference: Ionospheric correction Algorithm for galileo single frequency users (2016) https://www.gsc-europa.eu/system/files/galileo_documents/Galileo_Ionospheric_Model.pdf

Installation

This module depends on numpy for computation, and matplotlib and Basemap for plotting. In ubuntu they can be installed via:

sudp apt-get install python-numpy
sudo apt-get install python-matplotlib
sudo apt-get install python-mpltoolkits.basemap

This module doesn't require installation to your python environment's site-packages. Simply write scripts in the same directory as this project and import the necessary classes

Main classes

NequickG_global:

The global ionosphere's electron density, as described by the Nequick model, is fully defined by two types of inputs: time (month and universal time) and broadcast coefficients (a01, a02, a03). Once the NequickG_global object is instantiated, it can be used to calculate slant TECs and act as a factory for "local" NequickG objects

NequickG:

NequickG objects are models of the ionosphere localised to a particular longitude and latitude. It is generated by giving a position input to the Nequick_global's get_Nequick_local method. Internally, it contains the topside and bottomside models that constitutes the NequickG model. NequickG objects allows calculation of vertical electron density profiles and vertical TEC

Ray:

Ray objects specify a straight line propagation path. Used mainly with NequickG_global objects for slant TEC calculations. Relevant routines, such as determining the validity of the propagation path or the altitude along the path, are contained in this class.

NEQTime / Position / GalileoBroadcast:

These classes wrap and group the input parameters of the Nequick-G model into meaningful concepts. Also used to implement "approximate equality" just in case it is needed.

Example of approximate equality: [40.2N 0.3W] == [40N 0E]

Usage

Example usages of these classes are provided in the task folder.

If you need any more information, have any suggestions or noticed any bugs, do open a new Issue on this repository

Known issues

For low solar activities, like that listed in the validation table. F1 critical frequency can become negative. This is unphysical and likely to mean that there is a bug in the implementation.

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