Japan Geoscience Union Meeting 2015

Presentation information


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

[P-EM28] Dynamics in magnetosphere and ionosphere

Thu. May 28, 2015 4:15 PM - 6:00 PM 302 (3F)

Convener:*Yoshizumi Miyoshi(Solar-Terrestrial Environement Laboratory, Nagoya University), Hiroshi Hasegawa(Institute of Space and Astronautical Science, Japan Aerospace Exploration Agency), Shin'ya Nakano(The Institute of Statistical Mathematics), Yoshimasa Tanaka(National Institute of Polar Research), Tomoaki Hori(Nagoya University Solar Terrestrial Environment Laboratory Geospace Research Center), Chair:Yoshimasa Tanaka(National Institute of Polar Research)

5:15 PM - 5:30 PM

[PEM28-15] Loss processes of outer radiation belt electron: Contribution of magnetopause shadowing

*Takashi CHIBA1, Takahiro OBARA1, Satoshi KURITA2, Yoshizumi MIYOSHI2 (1.Planetary Plasma and Atmospheric Research Center,Tohoku University, 2.Solar-Terrestrial Environement Laboratory, Nagoya University)

Keywords:radiation belt, magnetopause shadowing, drift shell splitting, loss process

The Earth’s radiation belts consist of the inner and outer radiation belts, and these regions are composed of highly energetic electrons. Especially in the outer radiation belt, the energetic electron fluxes are highly variable during magnetic storms. Energetic electrons in the radiation belts sometimes cause satellite charging, resulting in gradual degradation of instruments and devices onboard satellites. Therefore, it is important to understand basic physics of the energetic electron variation in the outer radiation belt from the point of view of space weather. It has been considered that the drastic change of the outer radiation belt is controlled by the delicate balance between transport, acceleration and loss processes. However, each process has complex physical mechanisms and there remain still much outstanding questions.
In this study, we particularly focused on the loss processes. As a possible loss process, (i) precipitation to the atmosphere, (ii) Dst-effect and (iii) direct loss from the magnetopause (magnetopause shadowing) have been considered. The correlation between the magnetopause location and the outer boundary of the outer radiation belt was reported by Matsumura et al. [2011]. Turner et al. [2012] suggested that a rapid depression of outer belt electrons is caused by the sudden inward shift of the magnetopause and subsequent enhancement of outward radial diffusion. However, the regions where electrons escape and how the magnetopause shadowing effect reaches smaller L-value are still open questions.
In order to understand the effect of magnetopause shadowing, we used the concept of the drift shell splitting. Due to the asymmetric configuration of Earth’s magnetosphere, charged particles which have different pitch angles drift along the different drift shells. On the dayside, particles whose pitch angles are closer to 90 degrees have drift shells closer to the magnetopause. It is expected that, as a result of magnetopause shadowing, the pitch angle distribution will be the butterfly distribution. To investigate this hypothesis, we used Solid State Telescope (SST) onboard the THEMIS satellite and analyzed pitch angle distributions of energetic electrons.
Our result shows inward shift of dominant region of butterfly distribution when the magnetopause is compressed. We consider that this change is caused by the effect of inward shift of the magnetopause. However, the correlation coefficient between the magnetopause standoff distance and the shadowing region (the region where the effect of magnetopause shadowing is observed in the pitch angle distributions) is relatively low. It is because the effect of drift shell expansion due to the enhancement of the ring current. Then we calculate the largest L* which has last closed drift shell, L*max [Koller and Zaharia, 2011] and compared L*max with shadowing regions. The result shows good correlation and it supports the scenario that the electron loss is caused by the magnetopause shadowing.
However, our result also shows a little difference between loss and shadowing region. It means that the other loss processes are necessary to explain the total loss of outer belt electrons. We investigate this difference of the two by calculating 1-D Fokker Planck radial diffusion model. The simulation result supports the Turner’s scenario, magnetopause shadowing and subsequent enhancement of outward radial diffusion. However, strong radial diffusion coefficients are required to explain observation.
We also consider the precipitation loss to the atmosphere by using POES. POES can detect strong precipitation events. However, these precipitation events are not detected for all the events, there are some events which we can rarely detect strong precipitations. Thus, it is suggested that precipitation loss is not the main cause of loss but just the subsequent loss. However, we need to investigate further about precipitation loss.