Swarm A/B/C neutral mass density normalized to 400 km to be assimilated by the CTIPe physics based model coupled with the thermosphere ionosphere data assimilation scheme (TIDA). Swarm-A is assimilated and B/C are used for validation purposes. The selected period is March 2015 that contains the St. Patrick's Day storm 2015 between 16-18 of that month
The magnetosphere is a major source of energy for the Earth's ionosphere and thermosphere (IT) syste...
These are the results of assimilating neutral density measurements from GRACE-A, GRACE-B, and CHAMP ...
The perturbations in the magnetosphere-ionosphere-thermosphere system are significant during geomagn...
Dynamical changes in the ionosphere and thermosphere during geomagnetic storm times can have a signi...
During geomagnetic storms, communication and navigation instruments can be dramatically affected by ...
The response of the Ionosphere - Thermosphere (IT) system to severe storm conditions is of great imp...
During geomagnetic storms, rapid changes in the upper atmosphere can dramatically affect communicati...
Knowledge about the variability of the Thermosphere – Ionosphere (TI) system is essential for many c...
To improve Thermosphere–Ionosphere modeling during disturbed conditions, data assimilation schemes t...
Since the ionosphere is impacting various communication and navigation applications relying on radio...
The Coupled Thermosphere Ionosphere Plasmasphere electrodynamics (CTIPe) model is a global physics-b...
The complexity of the Sun-Earth system increases during magnetically disturbed conditions, caused by...
The specification and prediction of density fluctuations in the thermosphere, especially during geom...
Accurately predicting the thermospheric neutral mass density is crucial for estimating the trajector...
The magnetosphere is a major source of energy for the Earth’s ionosphere and thermosphere (IT) syste...
The magnetosphere is a major source of energy for the Earth's ionosphere and thermosphere (IT) syste...
These are the results of assimilating neutral density measurements from GRACE-A, GRACE-B, and CHAMP ...
The perturbations in the magnetosphere-ionosphere-thermosphere system are significant during geomagn...
Dynamical changes in the ionosphere and thermosphere during geomagnetic storm times can have a signi...
During geomagnetic storms, communication and navigation instruments can be dramatically affected by ...
The response of the Ionosphere - Thermosphere (IT) system to severe storm conditions is of great imp...
During geomagnetic storms, rapid changes in the upper atmosphere can dramatically affect communicati...
Knowledge about the variability of the Thermosphere – Ionosphere (TI) system is essential for many c...
To improve Thermosphere–Ionosphere modeling during disturbed conditions, data assimilation schemes t...
Since the ionosphere is impacting various communication and navigation applications relying on radio...
The Coupled Thermosphere Ionosphere Plasmasphere electrodynamics (CTIPe) model is a global physics-b...
The complexity of the Sun-Earth system increases during magnetically disturbed conditions, caused by...
The specification and prediction of density fluctuations in the thermosphere, especially during geom...
Accurately predicting the thermospheric neutral mass density is crucial for estimating the trajector...
The magnetosphere is a major source of energy for the Earth’s ionosphere and thermosphere (IT) syste...
The magnetosphere is a major source of energy for the Earth's ionosphere and thermosphere (IT) syste...
These are the results of assimilating neutral density measurements from GRACE-A, GRACE-B, and CHAMP ...
The perturbations in the magnetosphere-ionosphere-thermosphere system are significant during geomagn...