Penetration of auroral electric fields to the equator during a substorm

By Takashi Kikuchi, Hermann Lühr, K. Schlegel, H. Tachihara, M. Shinohara, T. Kitamura. 2000

224 citations recorded by the source corpus.

Subfields: Astronomy and Astrophysics, Geophysics, Molecular Biology

View Paper: https://www.semanticscholar.org/paper/782ded17d48e7fa00baa961a19079911fad11c9a

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Astronomy and Astrophysics

1. Yuichi Otsuka
2. K. Shiokawa
3. N. Balan
4. Chaosong Huang
5. J. Foster
6. M. Kelley
7. Takuya Tsugawa
8. Akinori Saito

In Geophysics

1. K. Shiokawa
2. Yuichi Otsuka
3. N. Balan
4. Chaosong Huang
5. J. Foster
6. M. Kelley
7. Takuya Tsugawa

In Molecular Biology

1. Yuichi Otsuka
2. K. Shiokawa

Citations in the corpus

• Sq and EEJ—A Review on the Daily Variation of the Geomagnetic Field Caused by Ionospheric Dynamo Currents (2017, unknown): “The time scale for the shielding processes is typically less than one hour (Kikuchi et al. 2000; Peymirat et al. 2000) but subject to magnetospheric conditions (Senior and Blanc 1984; Maruyama et al.”
• Long‐duration penetration of the interplanetary electric field to the low‐latitude ionosphere during the main phase of magnetic storms (2005, background): “... within the ring current cannot fully develop to cancel out the magnetospheric convection electric field, and the convection electric field will continuously leak to (or penetrate to) the low-latitude ionosphere without significant decay for many hours as long as the strengthening of the magnetic”
• Equatorial Ionospheric Electric Fields During the November 2004 Magnetic Storm (2007, unknown): “They disturb the ionosphere nearly simultaneously from middle to equatorial latitudes [e.g., Kikuchi et al., 1996, 2000 ].”
• Penetration of magnetospheric electric fields to the equator during a geomagnetic storm (2008, unknown): “The second is the growth time of the shielding electric field which was several hours for the storm main phase [Huang et al., 2005], although the shielding time was about 20 min for the substorm [Somayajulu et al., 1987; Kikuchi et al., 2000b ].”
• Super plasma fountain and equatorial ionization anomaly during penetration electric field (2009, background): “This and other unusually large deviations of the drift velocity on 9 November (Figure 1) are discussed by Fejer et al. [2007] and seem to be due to eastward and westward prompt penetration and disturbance dynamo action [e.g., Kikuchi et al., 2000; Kelley et al., 2003].”