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Does the Dayside Equatorial Ionospheric Electric Field Respond to Isolated Substorms?
by
Hayashi, M
, Ohtani, S
, Yoshikawa, A
in
Electric field
/ Electric fields
/ Electrojets
/ Electromagnetic fields
/ Equatorial electrojet
/ Equatorial regions
/ Ionosphere
/ Ionospheric electric fields
/ Magnetic field
/ Magnetic fields
/ Magnetosphere-ionosphere coupling
/ Statistical analysis
/ Statistical methods
2025
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Does the Dayside Equatorial Ionospheric Electric Field Respond to Isolated Substorms?
by
Hayashi, M
, Ohtani, S
, Yoshikawa, A
in
Electric field
/ Electric fields
/ Electrojets
/ Electromagnetic fields
/ Equatorial electrojet
/ Equatorial regions
/ Ionosphere
/ Ionospheric electric fields
/ Magnetic field
/ Magnetic fields
/ Magnetosphere-ionosphere coupling
/ Statistical analysis
/ Statistical methods
2025
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Do you wish to request the book?
Does the Dayside Equatorial Ionospheric Electric Field Respond to Isolated Substorms?
by
Hayashi, M
, Ohtani, S
, Yoshikawa, A
in
Electric field
/ Electric fields
/ Electrojets
/ Electromagnetic fields
/ Equatorial electrojet
/ Equatorial regions
/ Ionosphere
/ Ionospheric electric fields
/ Magnetic field
/ Magnetic fields
/ Magnetosphere-ionosphere coupling
/ Statistical analysis
/ Statistical methods
2025
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Does the Dayside Equatorial Ionospheric Electric Field Respond to Isolated Substorms?
Journal Article
Does the Dayside Equatorial Ionospheric Electric Field Respond to Isolated Substorms?
2025
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Overview
Substorms are known to induce global magnetosphere‐ionosphere coupling. However, the specific response of the dayside ionospheric electric field and its influence on the equatorial electrojet (EEJ) remain controversial. This study investigates the electromagnetic field response in the dayside equatorial region during isolated substorms using ground magnetic field data. Statistical analysis revealed that the H component decreased at equatorial and low‐latitude stations during isolated substorms. These decreases were of similar magnitude on average, indicating that significant changes in the EEJ caused by penetrating electric fields were not observed. However, individual events showed slight positive and negative variations. These results suggest that substorm‐associated electric fields can reach equatorial regions, but additional conditions determine the positive and negative variations. This finding provides new insights into the spatial extent of substorm‐induced electric fields.
Publisher
John Wiley & Sons, Inc
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