The Dedicated Ionospheric Field Inversion (DIFI) model is a Swarm-based, global model of the Sq and equatorial electrojet magnetic fields at mid and low-latitudes. It describes variations with local time, season and solar flux and separates primary and induced magnetic fields. The latest version of DIFI is DIFI-7. Please see the DIFI-7 for the detail.
- DIFI 7 is developed and tested in Python 3.11.2 environment
- Prequirements: numpy
- There is
examples.pyprovides the example to use the module.