JpGU-AGU Joint Meeting 2020

Presentation information

[E] Poster

P (Space and Planetary Sciences ) » P-EM Solar-Terrestrial Sciences, Space Electromagnetism & Space Environment

[P-EM13] Dynamics of Magnetosphere and Ionosphere

convener:Aoi Nakamizo(Applied Electromagnetic Research Institute, National Institute of Information and Communications Technology), Mitsunori Ozaki(Faculty of Electrical and Computer Engineering, Institute of Science and Engineering, Kanazawa University), Akiko Fujimoto(Kyushu Institute of Technology), Yuka Sato(Nippon Institute of Technology)

[PEM13-P20] A Modified Magnetosphere-Ionosphere Coupling Model by Including the Hall Effects due to Thinning of the Near-Earth Plasma Sheet

*Pai-Sheng Wang1, Ling-Hsiao Lyu1 (1.Institute of Space Science and Engineering, National Central University, Taoyuan, Taiwan)

Keywords:Substrom, Field-aligned current, Magnetosphere-Ionosphere coupling

Thinning of the near-Earth plasma sheet is commonly observed during the growth phase of a substorm. If the thickness of the near-Earth plasma sheet is between the ion’s gyro radius and the electron’s gyro radius, the unmagnetized ions and the magnetized electrons will move in different directions and result in a Hall effect in the near-Earth plasma sheet. This situation is similar to the collisional ions and the collisionless electrons in the E-region ionosphere. Kan et al. (1988) have proposed a Magnetosphere-Ionosphere coupling model to simulate the field-aligned current distributions in the ionosphere before the onset of a substorm. We modify the 1988 M-I coupling model by adding the Hall effect in the near-Earth plasma sheet during the growth phase of a substorm. We find that the Hall effect in the tail can enhance the field-aligned current and change the spatial distribution of the field-aligned current. As a result, both the intensity of the field-aligned currents and the spatial distribution of the upward field-aligned currents obtained in our simulations are in good agreement with the observed field-aligned currents at the onset of a substorm.