著者名 | Authors | 所属機関名 | 所属機関名(欧文) | |
1 | #A1 | Bargatze/L. F. | 名古屋大学太陽地球環境研究所 | Solar-Terrestrial Environment Laboratory, Nagoya University |
2 | 荻野オギノ/タツキ | Ogino/Tatsuki | 名古屋大学太陽地球環境研究所 | Solar-Terrestrial Environment Laboratory, Nagoya University |
講演予稿:
太陽風の条件の突然の変化が、サブストームの開始をトリガーで
きるかどうかは磁気圏物理において最近興味が持たれるようにな
ってきた。特に、惑星間磁場の北向きへの変化がサブストームを
トリガーする可能性について多くの経験的な研究が行われた。私
たちはその可能性を太陽風と地球磁気圏相互作用の3次元グロー
バルMHDシミュレーションから調べた。IMFを北向きから南
向きに変化させて、南向きを保つ場合と約40分後再び北向きに
変化させた場合の尾部リコネクションの開始時間の差は大きくは
なかった。IMFのみの北向き変化は、サブストームのトリガー
にMHDモデルの範囲では効果的ではないことが示唆される。
abstract:
Recently, there has been a strong interest in determining
whether abrupt changes in solar wind conditions can trigger
substorm expansion onsets. In particular, the triggering
capability of northward IMF turnings has been the topic
of many empirical studies. Here, the question is addressed
from the standpoint of global magnetohydrodynamic (MHD)
simulation. A set of MHD simulation runs have been compiled
to test whether step-like changes in solar wind dynamic
pressure and/or IMF Bz conditions can trigger an early onset
of the substorm expansion phase. A reference simulation is
run to estimate the standard length of a substorm growth
phase. The growth phase duration is found by measuring the
length of the time interval marked at the beginning by
southward turning of the IMF at the dayside magnetopause and
at the end by formation of the near-Earth neutral line. The
baseline simulation run is initiated by setting the IMF
northward at +5 nT for 4-hr then by flipping the IMF
southward to -5 nT. For this run, the expansion onset time
occurred about 60-min after southward IMF reached the nose
of the magnetosphere. In later simulations, a solar wind
trigger (a northward IMF turning and/or solar wind pressure
step) is introduced at the 40-min mark of the baseline run
and diagnostics are checked to see if the onset timing is
affected. For a northward turning without an associated
solar wind pressure change, the results show that onset
timing is unchanged. This suggest that northward triggers
are not effective expansion phase triggers for an MHD
magnetosphere. In fact, the dynamics following onset for
the northward turning case are weaker, the associated flows
are slower and a smaller plasmoid is produced which stalls
in the deep tail. The simulation run with a step-like solar
wind pressure increase (also introduced 40-min after the IMF
southward turning) induces the near-Earth neutral line to
form about 10 minutes faster the formation time found for
the reference case run with no external trigger. The onset
time delay is shortened by compression of the tail plasma
sheet as the magnetosphere reconfigures in response to the
increase in solar wind dynamic pressure. A case run with a
solar wind pressure increase and a northward turning, both
introduced at the 40-min time step, produces an accelerated
onset time matching that for an isolated pressure step
change.
キーワード:
サブストーム開始、太陽風の変化、惑星間磁場の北向き変化、電磁流体力学的シミュレーション、トリガー
Keywords:
substorm onset, solar wind pressure changes, IMF northward turnings, MHD simulation, triggering