Related Experiment Video
Updated: Oct 13, 2025

Sputter Growth and Characterization of Metamagnetic B2-ordered FeRh Epilayers
Published on: October 5, 2013
B2 Thickness Parameter Response to Equinoctial Geomagnetic Storms
Yenca Migoya-Orué1, Katy Alazo-Cuartas1, Anton Kashcheyev2
1The Abdus Salam International Centre for Theoretical Physics (ICTP), Strada Costiera 11, I-34151 Trieste, Italy.
Geomagnetic storms significantly impact the ionosphere
Area of Science:
- Space Physics
- Ionospheric Physics
- Geophysics
Background:
- Empirical models often define ionospheric thickness parameters using ionogram characteristics.
- The NeQuick model uses the B2 parameter, representing F2 bottomside electron density profile thickness, derived from an inflection point below the F2 layer peak.
- Understanding ionospheric responses to geomagnetic storms is crucial for space weather prediction.
Purpose of the Study:
- To investigate the effects of geomagnetic storms on the B2 thickness parameter.
- To analyze the temporal relationship between the B2 parameter, vertical total electron content (VTEC), and maximum electron density (NmF2) during storm events.
- To assess the potential of incorporating the B2 parameter into empirical models for improved storm-time predictions.
Main Methods:
- Analysis of three major equinoctial geomagnetic storms (March 17, 2013; October 2, 2013; March 17, 2015).
- Utilized GNSS-derived VTEC and NmF2 data from manually scaled ionograms across 20 stations in middle and low latitudes.
- Examined B2 parameter variations before, during, and after storm events in Asian, Euro-African, and American longitude sectors.
Main Results:
- Observed two primary B2 responses post-storm onset: a peak preceding VTEC/NmF2 increases (~60% of cases) and fluctuations linked to VTEC/NmF2 decreases (~25% of cases).
- The B2 parameter consistently reacted earlier than NmF2 and VTEC following storm onset across all analyzed locations.
- Storm-induced B2 behavior was correlated with dominant factors associated with positive and negative storm effects.
Conclusions:
- The B2 thickness parameter exhibits significant sensitivity to geomagnetic storm disturbances.
- Experimental B2 data shows a precursor response to changes in VTEC and NmF2 during storms.
- Incorporating the B2 parameter into empirical models like NeQuick could enhance their capability to model extreme ionospheric conditions during space weather events.
More Related Videos
06:49Radio Frequency Magnetron Sputtering of GdBa2Cu3O7âˆ'ÃŽ ´/ La0.67Sr0.33MnO3 Quasi-bilayer Films on SrTiO3 STO Single-crystal Substrates
Published on: April 12, 2019
04:35Author Spotlight: Simulation and Analysis of the Temperature Rise of Ring Main Unit Equipment
Published on: July 5, 2024
Related Concept Videos
Magnetostatic Boundary Conditions
Plane Electromagnetic Waves II
Diamagnetic Shielding of Nuclei: Local Diamagnetic Current
Atomic Nuclei: Larmor Precession Frequency
Electrostatic Boundary Conditions
The surface integral of an electric field is given by Gauss's law in integral form and is related to...
Magnetic Field Lines
Magnetic field lines follow several hard-and-fast rules: