掲載種別：研究論文（研究会，シンポジウム資料等）  

researchmap

掲載種別：研究論文（研究会，シンポジウム資料等）  

DOI： 10.11517/pjsai.JSAI2023.0_4Xin121

researchmap

掲載種別：研究論文（学術雑誌）   出版者・発行元：Oxford University Press (OUP)  

<title>ABSTRACT</title>
We perform radiative magnetohydrodynamic calculations for the solar-quiet region to investigate the dependence of statistical flow on magnetic properties and the three-dimensional structure of magnetic patches in the presence of large-scale flow that mimics differential rotation. It has been confirmed that strong magnetic field patches move faster in the longitudinal direction at the solar surface. Consequently, strong magnetic patches penetrate deeper into the solar interior. The motion of the deep-rooted magnetic patches is influenced by the faster differential rotation in the deeper layer. In this study, we perform realistic radiative magnetohydrodynamic calculations using r2d2 code to validate that stronger patches have deeper roots. We also add large-scale flow to mimic the differential rotation. The magnetic patches are automatically detected and tracked, and we evaluate the depth of 30 000 magnetic patches. The velocities of 2.9 million magnetic patches are then measured at the photosphere. We obtain the dependence of these values on the magnetic properties, such as field strength and flux. Our results confirm that strong magnetic patches tend to show deeper roots and faster movement, and we compare our results with observations using the point spread function of instruments at the Hinode and Solar Dynamics Observatory (SDO). Our result is quantitatively consistent with previous observational results of the SDO.

DOI： 10.1093/mnras/stab710

researchmap

その他リンク： http://academic.oup.com/mnras/article-pdf/503/3/3610/36855183/stab710.pdf

掲載種別：研究論文（学術雑誌）   出版者・発行元：American Astronomical Society  

DOI： 10.3847/1538-4357/ab6a90

researchmap

その他リンク： https://iopscience.iop.org/article/10.3847/1538-4357/ab6a90

掲載種別：研究論文（学術雑誌）   出版者・発行元：{MDPI} {AG}  

DOI： 10.3390/atoms7020055

researchmap

掲載種別：研究論文（学術雑誌）   出版者・発行元：American Astronomical Society  

DOI： 10.3847/1538-4357/aaebfc

researchmap

その他リンク： http://stacks.iop.org/0004-637X/869/i=2/a=99?key=crossref.00e9647cb345c28f6a46ce2b8d141e68

記述言語：英語   掲載種別：研究論文（学術雑誌）   出版者・発行元：Springer Netherlands  

We clarify the uncertainty in the inferred magnetic field vector via the Hanle diagnostics of the hydrogen Lyman-α line when the stratification of the underlying atmosphere is unknown. We calculate the anisotropy of the radiation field with plane-parallel semi-empirical models under the nonlocal thermal equilibrium condition and derive linear polarization signals for all possible parameters of magnetic field vectors based on an analytical solution of the atomic polarization and Hanle effect. We find that the semi-empirical models of the inter-network region (FAL-A) and network region (FAL-F) show similar degrees of anisotropy in the radiation field, and this similarity results in an acceptable inversion error (e.g., ∼40G instead of 50 G in field strength and ∼100∘ instead of 90 ∘ in inclination) when FAL-A and FAL-F are swapped. However, the semi-empirical models of FAL-C (averaged quiet-Sun model including both inter-network and network regions) and FAL-P (plage regions) yield an atomic polarization that deviates from all other models, which makes it difficult to precisely determine the magnetic field vector if the correct atmospheric model is not known (e.g., the inversion error is much larger than 40% of the field strength
&gt
70G instead of 50G). These results clearly demonstrate that the choice of model atmosphere is important for Hanle diagnostics. As is well known, one way to constrain the average atmospheric stratification is to measure the center-to-limb variation of the linear polarization signals. The dependence of the center-to-limb variations on the atmospheric model is also presented in this paper.

DOI： 10.1007/s11207-018-1293-6

Scopus

researchmap

掲載種別：研究論文（学術雑誌）   出版者・発行元：American Astronomical Society  

DOI： 10.3847/1538-4357/aa8e44

researchmap

記述言語：日本語   掲載種別：研究論文（学術雑誌）  

DOI： 10.3847/1538-4357/836/1/40

researchmap

記述言語：英語   掲載種別：研究論文（学術雑誌）   出版者・発行元：EDP Sciences  

The solar dynamo problem is the question of how the cyclic variation in the solar magnetic field is maintained. One of the important processes is the transport of magnetic flux by surface convection. To reveal this process, the dependence of the squared displacement of magnetic flux concentrations on the elapsed time is investigated in this paper via a feature-recognition technique and a continual five-day magnetogram. This represents the longest time scale over which a satellite observation has ever been performed for this problem. The dependence is found to follow a power law and differ significantly from that of diffusion transport. Furthermore, there is a change in the behavior at a spatial scale of 103.8 km. A super-diffusion behavior with an index of 1.4 is found at smaller scales, while changing to a sub-diffusion behavior with an index of 0.6 on larger ones. We interpret this difference in the transport regime as coming from the network-flow pattern.

DOI： 10.1051/swsc/2016022

Scopus

researchmap

記述言語：英語   掲載種別：研究論文（学術雑誌）   出版者・発行元：{IOP} Publishing  

In this second paper in the series, we investigate occurrence frequencies of apparent unipolar processes, cancellation, and emergence of patch structures in quiet regions. Apparent unipolar events are considerably more frequent than cancellation and emergence, per our definition, which is consistent with Lamb et al. Furthermore, we investigate the frequency distributions of changes in flux during apparent unipolar processes and find that they concentrate around the detection limit of the analysis. Combining these findings with the results of our previous paper, Iida et al., which found that merging and splitting are more dominant than emergence and cancellation, these results support the understanding that apparent unipolar processes are actually interactions with and among patches below the detection limit and that there still are numerous flux interactions between the flux range in this analysis and below the detection limit. We also investigate occurrence frequency distributions of flux decrease during cancellation. We found a relatively strong dependence, 2.48 +/- 0.26 as a power-law index. This strong dependence on flux is consistent with the model, which was suggested in the previous paper.

DOI： 10.1088/0004-637X/814/2/134

Web of Science

researchmap

掲載種別：研究論文（学術雑誌）  

DOI： 10.1088/0004-637X/799/2/139

researchmap

記述言語：英語   掲載種別：研究論文（学術雑誌）   出版者・発行元：OXFORD UNIV PRESS  

To elucidate the flare trigger mechanism, we have analyzed several flare
events which were observed by Hinode/Solar Optical Telescope (SOT), in our
previous study. Because of the limitation of SOT field of view, however, only
four events in the Hinode data sets have been utilizable. Therefore, increasing
the number of events is required for evaluating the flare trigger models. We
investigated the applicability of data obtained by the Solar Dynamics
Observatory (SDO) to increase the data sample for a statistical analysis of the
flare trigger process. SDO regularly observes the full disk of the sun and all
flares although its spatial resolution is lower than that of Hinode. We
investigated the M6.6 flare which occurred on 13 February 2011 and compared the
analyzed data of SDO with the results of our previous study using Hinode/SOT
data. Filter and vector magnetograms obtained by the Helioseismic and Magnetic
Imager (HMI) and filtergrams from the Atmospheric Imaging Assembly (AIA) 1600A
were employed. From the comparison of small-scale magnetic configurations and
chromospheric emission prior to the flare onset, we confirmed that the trigger
region is detectable with the SDO data. We also measured the magnetic shear
angles of the active region and the azimuth and strength of the flare-trigger
field. The results were consistent with our previous study. We concluded that
statistical studies of the flare trigger process are feasible with SDO as well
as Hinode data. We also investigated the temporal evolution of the magnetic
field before the flare onset with SDO.

DOI： 10.1093/pasj/psu091

Web of Science

arXiv

researchmap

その他リンク： http://arxiv.org/pdf/1407.1887v1

記述言語：英語   掲載種別：研究論文（学術雑誌）   出版者・発行元：SPRINGER  

We present a comparison of the Solar Dynamics Observatory (SDO) analysis of NOAA Active Region (AR) 11158 and numerical simulations of flux-tube emergence, aiming to investigate the formation process of this flare-productive AR. First, we use SDO/Helioseismic and Magnetic Imager (HMI) magnetograms to investigate the photospheric evolution and Atmospheric Imaging Assembly (AIA) data to analyze the relevant coronal structures. Key features of this quadrupolar region are a long sheared polarity inversion line (PIL) in the central delta-sunspots and a coronal arcade above the PIL. We find that these features are responsible for the production of intense flares, including an X2.2-class event. Based on the observations, we then propose two possible models for the creation of AR 11158 and conduct flux-emergence simulations of the two cases to reproduce this AR. Case 1 is the emergence of a single flux tube, which is split into two in the convection zone and emerges at two locations, while Case 2 is the emergence of two isolated but neighboring tubes. We find that, in Case 1, a sheared PIL and a coronal arcade are created in the middle of the region, which agrees with the AR 11158 observation. However, Case 2 never builds a clear PIL, which deviates from the observation. Therefore, we conclude that the flare-productive AR 11158 is, between the two cases, more likely to be created from a single split emerging flux than from two independent flux bundles.

DOI： 10.1007/s11207-014-0502-1

Web of Science

researchmap

記述言語：英語   掲載種別：研究論文（学術雑誌）   出版者・発行元：IOP PUBLISHING LTD  

We report a detailed event analysis on the M6.6-class flare in the active
region (AR) NOAA 11158 on 2011 February 13. AR 11158, which consisted of two
major emerging bipoles, showed prominent activities including one X- and
several M-class flares. In order to investigate the magnetic structures related
to the M6.6 event, particularly the formation process of a flare-triggering
magnetic region, we analyzed multiple spacecraft observations and numerical
results of a flare simulation. We observed that, in the center of this
quadrupolar AR, a highly sheared polarity inversion line (PIL) was formed
through proper motions of the major magnetic elements, which built a sheared
coronal arcade lying over the PIL. The observations lend support to the
interpretation that the target flare was triggered by a localized magnetic
region that had an intrusive structure, namely a positive polarity penetrating
into a negative counterpart. The geometrical relationship between the sheared
coronal arcade and the triggering region was consistent with the theoretical
flare model based on the previous numerical study. We found that the formation
of the trigger region was due to a continuous accumulation of the small-scale
magnetic patches. A few hours before the flare occurrence, the series of
emerged/advected patches reconnected with a preexisting fields. Finally, the
abrupt flare eruption of the M6.6 event started around 17:30 UT. Our analysis
suggests that, in a triggering process of a flare activity, all magnetic
systems of multiple scales, not only the entire AR evolution but also the fine
magnetic elements, are altogether involved.

DOI： 10.1088/0004-637X/773/2/128

Web of Science

arXiv

researchmap

その他リンク： http://arxiv.org/pdf/1306.2451v1

記述言語：英語   掲載種別：研究論文（学術雑誌）   出版者・発行元：IOP PUBLISHING LTD  

Solar flares and coronal mass ejections, the most catastrophic eruptions in our solar system, have been known to affect terrestrial environments and infrastructure. However, because their triggering mechanism is still not sufficiently understood, our capacity to predict the occurrence of solar eruptions and to forecast space weather is substantially hindered. Even though various models have been proposed to determine the onset of solar eruptions, the types of magnetic structures capable of triggering these eruptions are still unclear. In this study, we solved this problem by systematically surveying the nonlinear dynamics caused by a wide variety of magnetic structures in terms of three-dimensional magnetohydrodynamic simulations. As a result, we determined that two different types of small magnetic structures favor the onset of solar eruptions. These structures, which should appear near the magnetic polarity inversion line (PIL), include magnetic fluxes reversed to the potential component or the nonpotential component of major field on the PIL. In addition, we analyzed two large flares, the X-class flare on 2006 December 13 and the M-class flare on 2011 February 13, using imaging data provided by the Hinode satellite, and we demonstrated that they conform to the simulation predictions. These results suggest that forecasting of solar eruptions is possible with sophisticated observation of a solar magnetic field, although the lead time must be limited by the timescale of changes in the small magnetic structures.

DOI： 10.1088/0004-637X/760/1/31

Web of Science

researchmap

記述言語：英語   掲載種別：学位論文（博士）  

researchmap

記述言語：英語   掲載種別：研究論文（学術雑誌）   出版者・発行元：IOP PUBLISHING LTD  

Frequencies of magnetic patch processes on the supergranule boundary, namely, flux emergence, splitting, merging, and cancellation, are investigated through automatic detection. We use a set of line-of-sight magnetograms taken by the Solar Optical Telescope (SOT) on board the Hinode satellite. We found 1636 positive patches and 1637 negative patches in the data set, whose time duration is 3.5 hr and field of view is 112 '' x 112 ''. The total numbers of magnetic processes are as follows: 493 positive and 482 negative splittings, 536 positive and 535 negative mergings, 86 cancellations, and 3 emergences. The total numbers of emergence and cancellation are significantly smaller than those of splitting and merging. Further, the frequency dependence of the merging and splitting processes on the flux content are investigated. Merging has a weak dependence on the flux content with a power-law index of only 0.28. The timescale for splitting is found to be independent of the parent flux content before splitting, which corresponds to similar to 33 minutes. It is also found that patches split into any flux contents with the same probability. This splitting has a power-law distribution of the flux content with an index of -2 as a time-independent solution. These results support that the frequency distribution of the flux content in the analyzed flux range is rapidly maintained by merging and splitting, namely, surface processes. We suggest a model for frequency distributions of cancellation and emergence based on this idea.

DOI： 10.1088/0004-637X/752/2/149

Web of Science

researchmap

記述言語：英語   掲載種別：研究論文（学術雑誌）  

DOI： 10.1088/2041-8205/751/1/L9

researchmap

記述言語：英語   掲載種別：研究論文（学術雑誌）   出版者・発行元：EDP SCIENCES S A  

Context. The anelastic approximation is often adopted in numerical calculations with low Mach numbers, such as those including stellar internal convection. This approximation requires so-called frequent global communication, because of an elliptic partial differential equation. Frequent global communication is, however, negative factor for the parallel computing performed with a large number of CPUs.
Aims. We test the validity of a method that artificially reduces the speed of sound for the compressible fluid equations in the context of stellar internal convection. This reduction in the speed of sound leads to longer time steps despite the low Mach number, while the numerical scheme remains fully explicit and the mathematical system is hyperbolic, thus does not require frequent global communication.
Methods. Two- and three-dimensional compressible hydrodynamic equations are solved numerically. Some statistical quantities of solutions computed with different effective Mach numbers (owing to the reduction in the speed of sound) are compared to test the validity of our approach.
Results. Numerical simulations with artificially reduced speed of sound are a valid approach as long as the effective Mach number (based on the lower speed of sound) remains less than 0.7.

DOI： 10.1051/0004-6361/201118268

Web of Science

researchmap

記述言語：英語   掲載種別：研究論文（国際会議プロシーディングス）  

Web of Science

researchmap

記述言語：英語   掲載種別：研究論文（国際会議プロシーディングス）  

Web of Science

researchmap

記述言語：英語   掲載種別：研究論文（学術雑誌）   出版者・発行元：IOP PUBLISHING LTD  

A cancellation is thought to be a basic process of the photospheric magnetic field and plays an important role in magnetic flux budget and in various solar activities. There are two major theoretical scenarios for this phenomena, the "U-loop emergence" and the "Omega-loop submergence" models. It is important to clarify which is the dominant process during the cancellation for the estimation of the solar magnetic flux transport through the surface. We study the vector magnetic field and velocity structures around a quiet-Sun cancellation by using the Solar Optical Telescope on board the Hinode satellite. Transverse magnetic field connecting the canceling magnetic features and strong long-lasting Doppler redshift signal are found. The transverse field is observed in the first spectropolarimetric observation after the occurrence of the cancellation while the redshift is clearly delayed to the cancellation by 20 minutes. These results indicate that the observed cancellation is an "Omega-loop submergence."

DOI： 10.1088/0004-637X/713/1/325

Web of Science

researchmap

J-GLOBAL

researchmap

J-GLOBAL

researchmap

記述言語：日本語   出版者・発行元：一般社団法人日本物理学会  

CiNii Article

CiNii Books

researchmap

記述言語：日本語   掲載種別：記事・総説・解説・論説等（学術雑誌）  

researchmap

J-GLOBAL

researchmap

記述言語：日本語   出版者・発行元：一般社団法人日本物理学会  

CiNii Article

CiNii Books

researchmap

記述言語：日本語   出版者・発行元：京都大学大学院理学研究科附属天文台  

CiNii Article

CiNii Books

researchmap