Possible generation mechanisms of the Pi2 pulsations estimated from a global MHD simulation
© The Society of Geomagnetism and Earth, Planetary and Space Sciences (SGEPSS); The Seismological Society of Japan; The Volcanological Society of Japan; The Geodetic Society of Japan; The Japanese Society for Planetary Sciences; TERRAPUB. 2012
Received: 18 June 2012
Accepted: 26 November 2012
Published: 10 June 2013
The plasmaspheric virtual resonance (PVR) and the transient Alfvén wave bouncing between the ionospheres in both hemispheres (the transient response, TR) are regarded as the possible generation mechanisms of the Pi2 pulsations. However, the global MHD simulation of a substorm (Tanaka et al., 2010) did not reproduce such wave modes because of insufficient ionospheric reflection of the Alfvén wave, numerical transfer of the Alfvén wave across the field lines, and no plasmasphere. Furthermore, it is noted that the substorm current wedge (SCW) which is a driver of the TR is not reproduced in the global MHD simulation. In this study, we search the sources of the Pi2 pulsations in the global MHD simulation, namely, the compressional wave in the inner magnetosphere for the PVR and the Alfvén wave injected to the ionosphere for the TR. In conclusion, there appears a compressional signal in the inner magnetosphere when the high-speed Earthward flow at the substorm onset surges in the inner edge of the plasma sheet. This simulation result suggests that this compressional wave would be trapped in the plasmasphere as the PVR if the model has the plasmasphere. As for TR, the global MHD simulation provides suddenly increasing field-aligned current (the Alfvén wave) associated with sudden appearance of the shear flow which comes from the high-speed flow in the plasma sheet at the onset of the substorm. If the global MHD simulation correctly lets the Alfvén wave be reflected in the ionosphere and transmitted along the field line, the TR would be established. As the ballooning instability is regarded as one of candidates of the Pi2 pulsation sources, we also briefly investigate whether the simulated plasma sheet in the growth phase is unstable or not for the ballooning instability.
The Pi2 pulsation is a damped oscillation with a period of 40–150 sec. (Saito, 1969; Olson, 1999). Simultaneous occurrence of the Pi2 pulsation with the substorm onset (e.g., Saito et al., 1976) indicates that the Pi2 pulsation is one of the important ingredients in the substorm processes. Thus, when we make a numerical substorm model, it is important to investigate how the Pi2 pulsation is generated at the sub-storm onset in the model. We have a newly improved MHD simulation model that is believed to reproduce correctly the substorm onset (Tanaka et al., 2010). Thus, it is important to consider how the Pi2 pulsation is generated in the simulation. This is the motivation of the present work.
The main features of Pi2 have been summarized in reviews by Olson (1999) and Keiling and Takahashi (2011). There appears to be a latitude distribution of Pi2 spectral properties. After Yumoto et al. (2001), the Pi2 pulsation at mid- and low-latitudes tends to have latitudinally-independent and rather higher frequency, while at higher latitudes the high-latitude one shows the lower frequency that gradually decreases. The Pi2 pulsation with the common frequency at mid- and low-latitudes is explained in terms of the plasmaspheric virtual resonance (PVR) mode (Fujita and Glassmeier, 1995; Lee, 1998). Experimental evidence for the PVR was given by Takahashi et al. (2003). On the other hand, the Pi2 pulsation at higher latitudes can be regarded as a transiently bouncing wave packet of the Alfvén mode (the transient response, TR) (Baumjohann and Glassmeier, 1984). It is concluded that the Pi2 pulsation shows two different features in high-latitudes and middle-and low-latitudes. Therefore, the model of the Pi2 pulsation should explain behavior of the Pi2 pulsation both at high-latitude and at middle- and low-latitudes. Furthermore, the initial movement of the ground magnetic variation associated with the Pi2 pulsation is consistent with the magnetic variation induced from the Region 1 (R1) field-aligned current (FAC) (Yumoto et al., 1990). This result has been believed to support the model that the Pi2 pulsation is associated with the substorm current wedge (SCW) (McPherron et al., 1973). Consequently, Fujita et al. (2002) performed their numerical simulation of the Pi2 pulsation based on a simplified model of the SCW (the linear MHD-wave simulation). The linear MHD-wave simulation is explained in the next section.
Let us describe briefly the substorm scenario deduced from the global MHD simulation (Tanaka et al., 2010). In the growth phase after southward turn of the interplanetary magnetic field (IMF), the magnetic field convection in the lobe region and that in the plasma sheet are different. Thus the magnetic fields in the plasma sheet region are configured to be strongly extended tailward in the equatorial plane (the plasma sheet thinning). At the same time, electromagnetic energy is stored in the mid-tail region. As the thinning cannot continue indefinitely, there must be sudden transition of the convection system. The transition starts at time of the reconnection from which the magnetic field tension stored in the growth phase is released. The released tension yields high-speed plasma flow toward the Earth and yields enhanced pressure in the inner boundary of the plasma sheet. The simulation by Tanaka et al. (2010) reproduces sudden magnetic field depression (explosive growth phase after Ohtani et al. (1992)) and sudden enhancement of the Region 2 (R2) FAC due to enhanced pressure in the inner boundary of the plasma sheet invoked by the highspeed plasma flow from the plasma sheet at the substorm onset. Finally, the R1 FAC is also formed as a part of a loop closure current associated with the R2 FAC in the magnetosphere-ionosphere region. In the simulation, they succeeded in reproducing abrupt decrease in AL indices at auroral onset. However, the simulation does not reproduce the SCW. Therefore, the premise for the linear MHD-wave simulation of the Pi2 pulsation is not realized in the global MHD simulation. Therefore, we need to investigate how the Pi2 pulsation is thought to be produced in the situation reproduced by the global MHD simulation.
In the next section, we discuss how the Pi2 pulsation is regarded to be generated based on both the global MHD simulation of the substorm (Tanaka et al., 2010) and the linear MHD-wave simulation of the Pi2 pulsation (Fujita et al., 2000, 2001, 2002). It is noted that we do not reproduce the Pi2 signals in the coupled model of the global MHD simulation and the linear MHD-wave simulation. We just discuss how the global MHD simulation invokes plasma disturbances that are regarded as sources of the Pi2 pulsations in the linear MHD-wave simulation. In the third section, the ballooning mode that is considered to drive the Pi2 pulsation will be discussed in brief. In the last section, we summarize main results.
2. Numerical Results
First, we note that the oscillations with period of 40–150 sec are not detected at the onset of the substorm in the global MHD simulation. Therefore, we discuss possible generation mechanisms of the Pi2 pulsation based on the plasma behavior revealed from the numerical results of the global MHD simulation.
Although the global MHD simulation solves a full set of the MHD equations, it does not reproduce the Pi2 pulsation explicitly because of several assumptions in modeling the physical system, e.g., numerical transfer of the field-aligned propagating Alfvén wave in the numerical grid is not referenced to the magnetic field lines and imperfect reflection of the MHD waves injected to the ionosphere, and lack of the plasmasphere. On the other hand, the linear MHD-wave simulation (Fujita et al., 2000, 2001, 2002) reproduces the Pi2 pulsation, but it employs the hypothetical SCW as a driver of the MHD waves. Thus, if we prove that the global MHD simulation provides source disturbances necessary for the Pi2 pulsation generation employed by Fujita et al. (2002), we suggest that the global MHD simulation may be capable of reproducing the Pi2 pulsation associated with the substorm.
2.1 The Pi2 pulsation simulated by the linear MHD-wave simulation
The linear MHD model of Fujita et al. (2002) simulated Pi2 propagation in a non-uniform magnetosphere with the plasmasphere under the realistic ionosphere boundary condition by assigning explicitly a source of the Pi2 pulsation. Refection of the MHD wave incident to the ionosphere is also correctly treated unlike the global MHD simulation. The linear MHD model used a sudden formation of the SCW (McPherron et al., 1973) as a driver of the Pi2 pulsation. However, it was impossible to simulate the SCW self-consistently in the linear MHD-wave simulation. Therefore, it employed a suddenly developing dusk-to-dawn current in the midnight region at L ~ 10 R e as an external input of MHD disturbances (an equivalence of the SCW). The dusk-to-dawn current system is confined in azimuthal (local-time) direction. The simulation showed Alfvén wave packets emitted from the east- and west-end regions of the SCW bounce between the ionospheres in both hemispheres; these signals are Pi2 pulsations at high latitudes (the TR). At the same time, the compressional mode (the fast mag-netosonic mode) generated by sudden increase of the azimuthal current is launched to the inner magnetosphere. As there is a minimum of the Alfvén speed profile in the plasmasphere, the compressional mode is partly trapped there. This trapping invokes the PVR which has azimuthally nonuniform electromagnetic field because the source of this PVR is limited in the azimuthal direction. Therefore, the coupling resonance between the PVR (the compressional wave) and the field-line resonance mode (the Alfvén wave) occurs in the inner magnetosphere (Tamao, 1965).
2.2 The Pi2 pulsations at high-latitudes
2.3 The Pi2 pulsations at middle- and low-latitudes
Tanaka et al. (2010) demonstrated that the high-speed Earthward convection flow at the substorm onset suddenly stops in the region with increased ambient magnetic field intensity (the Ring current region) in the nightside magne-tosphere. Then, pressure at L ~ 7 R e is suddenly increased. In other words, the inner magnetosphere in the nightside is suddenly compressed. Then, if this sudden compression will invoke a compressional MHD wave in the inner magnetosphere and if there might have been the plasmasphere where V a (the Alfvén speed) exhibits local minimum, the conditions would be right for the PVR to be generated (Fujita and Glassmeier, 1995; Lee and Kim, 1999). Fujita et al. (2002) presented behavior of the compressional wave and that of the field line resonant wave (Alfvén wave) which are consistent with observation of MHD waves at the substorm (e.g, Teramoto et al, 2011). As the global MHD simulation does not have the plasmasphere structure, we cannot reproduce the PVR in the simulation. However, if we can detect the compressional wave in the inner magnetosphere in the simulation, this wave may lead to the PVR as obtained by Fujita et al. (2002). Consequently, we need to investigate whether the compressional wave is excited by sudden compression of the inner magnetopause at the substorm onset.
In the previous section, we have identified sources of the Pi2 pulsations employed in the MHD simulation of the sub-storm from the numerical results of the global MHD simulation. The candidates of the generation mechanisms— the TR and the PVR may be reproduced in the global MHD simulation if defects of the global MHD simulation (namely, lack of the plasmasphere, numerical diffusion of the Alfvén wave, and imperfect reflection of the MHD wave injected into the ionosphere) are resolved. Meanwhile, resent observations suggest that the high-speed plasma flow in the plasma sheet exhibits the Pi2-like oscillatory behaviors at the onset of the substorm (Kepko and Kivelson, 1999). In particular, Keiling (2012) reported that the Pi2 pulsation which appears before the auroral break-up is possibly generated by the drift ballooning instability (Miura et al., 1989). As for the theoretical study, Cheng and Zaharia (2004) investigated the ballooning instability in the plasma sheet in the growth phase of the substorm based on the ideal MHD magnetosphere model from Tyganenko. After their analysis, low-frequency MHD waves are unstable in the plasma sheet for the ballooning instability in the growth phase. This wave may be a source of the Pi2 pulsation although the nonlinear evolution of the ballooning instability in the magnetosphere has not been studied yet. Therefore, it seems meaningful to investigate that the plasma sheet in the growth phase is unstable or not for the ballooning instability based on the global MHD simulation. It is noted that the present MHD simulation does not reproduce the ballooning instability. This does not mean the plasma sheet stable for the ballooning instability, but insufficient mesh resolution of the present simulation may prevent realization of the instability (Zhu et al., 2009).
The ballooning instability should be examined with the global energy principle based on the plasma parameters along magnetic field lines or the global eigenvalue analysis. So, the local analysis done in this paper is an approximation. However, the results indicate that the ballooning instability may occur in the growth phase of the substorm.
From the linear MHD-wave simulation of the Pi2 pulsation (Fujita et al., 2001, 2002), the Pi2 pulsation is the TR at high latitudes and the PVR in middle- and low-latitudes. As the global MHD simulation does not correctly reproduce reflection of the MHD wave at the ionosphere nor field-aligned propagation of the Alfvén wave, it is difficult to reproduce the TR. In addition, the global MHD simulation does not have the plasmasphere, it is impossible to reproduce the PVR, either. Therefore, we look for plasma disturbances that are regarded as sources of the Pi2 pulsations in the linear MHD-wave simulation. Thus, rapid growth of R1 FAC and generation of the fast magnetosonic mode wave in the inner magnetosphere are two necessary conditions for the Pi2 pulsation. From these considerations, we investigated rapid growth of the R1 FAC and the fast magnetosonic wave in the inner magnetosphere.
At the substorm onset, the MHD simulation gives rapid growth of R1 FAC. This would generate the bouncing Alfvén wave between ionospheres in both hemispheres. This rapid growth of the R1 FAC is not related with the SCW. Therefore, the Pi2 pulsation at high latitudes could be generated without the SCW.
When the enhanced high-speed convection flow in the plasma sheet at the onset stops in the Ring current region (L ~ 7 R e ), we confirm that the fast magnetosonic wave is generated in the inner magnetosphere. If we consider the plasmasphere, this fast magnetosonic wave would invoke the PVR.
The plasma sheet in the growth phase of the substorm might be unstable for the ballooning instability, which might trigger the Pi2 pulsation. To confirm this possibility, we need to perform more rigorous analysis.
This paper describes only possible generation mechanisms of the Pi2 pulsations based on the global MHD simulation. As nobody has attempted such a research yet, we believe that this research is quite important for the Pi2 pulsation research. However, it should be noticed again that the present MHD simulation incompletely reproduces whole processes associated with the substorm because the simulation does not yield the waves with a period of the Pi2 pulsation. Probably, we need to improve the MHD code significantly to reproduce the Pi2 pulsations. The issues to be improved are propagation of the Alfvén wave along magnetic field lines, reflection of the MHD wave by the ionosphere, and inclusion of the plasmasphere.
This research was supported by the Trans-disciplinary Research Integration Project “Data Assimilation” through Transdisciplinary Research Integration Center in Research Organization of Information and Systems. One of the authors (S. F.) thanks A. Miura of University of Tokyo and T. Ogino of Nagoya University for discussions concerning the ballooning instability. He is also thankful to T. Uozumi of Kyushu Univ. for discussions about observations of Pi2 pulsations. Computations for this study have been done in the computers installed in National Institute of Polar Research, National Institute of Information and Communication Technology, National Institute for Fusion Sciences, and Nagoya University. Utilization of OneSpaceNet for a large storage system is also acknowledged.
- Baumjohann, W. and K.-H. Glassmeier, The transient response mechanism and Pi 2 pulsations at substorm onset—Review and outlook, Planet. Space Sci., 32, 1361–1370, 1984.View ArticleGoogle Scholar
- Cheng, C. Z. and S. Zaharia, MHD ballooning instability in the plasma sheet, Geophys. Res. Lett., 31, L06809, doi:10.1029/2003GL018823, 2004.Google Scholar
- Fujita, S. and K.-H. Glassmeier, Magnetospheric cavity resonance oscillations with energy transfer across the magnetopause, J. Geomag. Geo-electr., 47, 1277–1292, 1995.View ArticleGoogle Scholar
- Fujita, S., M. Itonaga, and H. Nakata, Relation between the Pi2 pulsations and the localized impulsive current associated with the current disruption in the magnetosphere, Earth Planets Space, 52, 267–281, 2000.View ArticleGoogle Scholar
- Fujita, S., T. Mizuta, M. Itonaga, A. Yoshikawa, and H. Nakata, Propagation property of transient MHD impulses in the magnetosphere-ionosphere system: The 2D model of the Pi2 pulsation, Geophys. Res. Lett., 28, 2161–2164, 2001.View ArticleGoogle Scholar
- Fujita, S., H. Nakata, M. Itonaga, A. Yoshikawa, and T. Mizuta, A numerical simulation of the Pi2 pulsations associated with the substorm current wedge,J. Geophys. Res., 107(A3), 1027, doi:10.1029/2001JA000137, 2002.Google Scholar
- Keiling, A., Pi2 pulsations driven by ballooning instability, J. Geophys. Res., 117, A03228, doi:10.1029/2011JA017223, 2012.Google Scholar
- Keiling, A. and K. Takahashi, Review of Pi2 Models, Space Sci. Rev., 161, 63–148, doi:10.1007/s11214-011-9818-4, 2011.View ArticleGoogle Scholar
- Kepko, L. and M. G. Kivelson, Generation of Pi2 pulsations by bursty bulk flows,J. Geophys. Res., 104, 25021–25034, 1999.View ArticleGoogle Scholar
- Lee, D.-H., On the generation mechanism of Pi 2 pulsations in the magne-tosphere, Geophys. Res. Lett., 25, 583–586, 1998.View ArticleGoogle Scholar
- Lee, D.-H. and K. Kim, Compressional MHD waves in the magnetosphere: A new approach, J. Geophys. Res., 104, 12379–12385, 1999.View ArticleGoogle Scholar
- McPherron, R. L., C. T. Russell, and M. P. Aubry, Satellite studies of magnetospheric substorms on August 15, 1968. 9. Phenomenological model for substorms, J. Geophys. Res., 78, 3131–3149, 1973.View ArticleGoogle Scholar
- Miura, A., Validity of the fluid description of critical β and Alfven time scale of ballooning instability onset in the near-Earth collisionless high-β plasma,J. Geophys. Res., 109, A02211, doi:10.1029/2003JA009924, 2004.Google Scholar
- Miura, A., S. Ohtani, and T. Tamao, Ballooning instability and structure of diamagnetic hydromagnetic waves in a model magnetosphere, J. Geophys. Res., 94, 15231–15242, 1989.View ArticleGoogle Scholar
- Ohtani, S., K. Takahashi, L. J. Zanetti, T. A. Potemra, R. W. McEntire, and T. Iijima, Initial signatures of magnetic field and energetic particle fluxes at tail reconfiguration: Explosive growth phase, J. Geophys. Res., 97(A12), 19,311–19,324, doi:10.1029/92JA01832, 1992.View ArticleGoogle Scholar
- Olson, J. V., Pi 2 pulsations and substorm onsets: A review, J. Geophys. Res., 104, 17499–17520, 1999.View ArticleGoogle Scholar
- Saito, T., Geomagnetic pulsations, Space Sci. Rev., 10, 319–412, 1969.View ArticleGoogle Scholar
- Saito, T., K. Yumoto, and K. Koyama, Magnetic pulsation Pi 2 as a sensitive indicator of magnetic substorm, Planet. Space Sci.,24, 1025–1029, 1976.View ArticleGoogle Scholar
- Takahashi, K., D.-H. Lee, M. Nosé, R. R. Anderson, and W. J. Hughes, CR-RES electric field study of the radial mode structure of Pi2 pulsations, J. Geophys. Res., 108(A5), 1210, doi:10.1029/2002JA009761, 2003.View ArticleGoogle Scholar
- Tamao, T., Transmission and coupling resonance of hydromagnetic disturbances in the non-uniform Earth’s magnetosphere, Sci. Rep. Tohoku Univ., Ser. 5, Geophys., 17, 43–70, 1965.Google Scholar
- Tanaka, T., A. Nakamizo, A. Yoshikawa, S. Fujita, H. Shinagawa, H. Shimazu, T. Kikuchi, and K. K. Hashimoto, Substorm convection and current system deduced from the global simulation, J. Geophys. Res., 115, A05220, doi:10.1029/2009JA014676, 2010.Google Scholar
- Teramoto, M., K. Takahashi, M. Nose, D.-H. Lee, and P. R. Sutcliffe, Pi2 pulsations in the inner magnetosphere simultaneously observed by the Active Magnetospheric Particle Tracer Explorers/Charge Composition Explorer and Dynamics Explorer 1 satellites, J. Geophys. Res., 116, A07225, doi:10.1029/2010JA016199, 2011.Google Scholar
- Yumoto, K., K. Takahashi, T. Sakurai, P. R. Sutcliffe, S. Kokubun, H. Lühr, T. Saito, M. Kuwashima, and N. Sato, Multiple ground-based and satellite observations of global Pi 2 magnetic pulsations, J. Geophys. Res.,95(A9), 15,175–15,184, 1990.View ArticleGoogle Scholar
- Yumoto, K. and CPMN group, Characteristics of Pi2 geomagnetic pulsations observed at the CPMN stations: A review of the STEP results, Earth Planets Space, 53, 981–992, 2001.View ArticleGoogle Scholar
- Zhu, P., J. Raeder, K. Germaschewski, and C. C. Hegna, Initiation of ballooning instability in the near-Earth plasma sheet prior to the 23 March 2007 THEMIS substorm expansion onset, Ann. Geophys., 27, 1129–1138, doi:10.5194/angeo-27-1129-2009, 2009.View ArticleGoogle Scholar