Japan Geoscience Union Meeting 2021

Presentation information

[E] Oral

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

[P-EM08] Space Weather and Space Climate

Fri. Jun 4, 2021 3:30 PM - 5:00 PM Ch.06 (Zoom Room 06)

convener:Ryuho Kataoka(National Institute of Polar Research), A Antti Pulkkinen(NASA Goddard Space Flight Center), Kanya Kusano(Institute for Space-Earth Environmental Research, Nagoya University), Kaori Sakaguchi(National Institute of Information and Communications Technology), Chairperson:Antti A Pulkkinen(NASA Goddard Space Flight Center), Ryuho Kataoka(National Institute of Polar Research)

4:15 PM - 4:30 PM

[PEM08-10] Numerical Proton Flux Response in South Atlantic Anomaly during Geomagnetic Storm

*Kirolosse Mina Girgis1,2, Tohru Hada1,4, Shuichi Matsukiyo1,4, Akimasa Yoshikawa3,4 (1.Department of Earth System Science and Technology, Interdisciplinary Graduate School of Engineering Sciences, Kyushu University, 2.Aerospace Engineering Department, Faculty of Engineering, Cairo University, Egypt, 3.Department of Earth and Planetary Sciences, Graduate School of Sciences, Kyushu University, 4.International Center for Space Weather Science and Education (ICSWSE), Kyushu University, Fukuoka, Japan)

Keywords:South Atlantic Anomaly, Inner Proton Belt, Test Particle Simulations, Geomagnetic Storm, Inductive Electric Field, Tsyganenko Model

In this research, we have developed a test particle simulation code to study the inner proton belt dynamics and the proton flux variations inside the South Atlantic Anomaly (SAA) during the geomagnetic storm event of 15 May 2005. The Tao-Chan-Brizard guiding center model was implemented to evaluate the trajectories of 140-400 MeV protons. The time-varying magnetic field model was evaluated by the Tsyganenko model TS05 with the corresponding inductive electric field. The South Atlantic Anomaly is an important feature of the Low-Earth Orbit (LEO) environment which creates a significant radiation source affecting most of the LEO mission performance. Numerical results showed that during the storm main phase, the SAA proton flux was decreased, while during the initial and recovery phases, the SAA proton flux was increased at most of the altitudes. The latter conclusion was confirmed using satellite measurements.