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1.
地磁钩扰是太阳耀斑效应的直观表现之一,其研究有助于深入理解太阳爆发对地球空间环境的影响过程,并能为空间天气建模和预报提供科学依据.本文利用山东大学威海地磁台和Intermagnet地磁链与子午工程的地磁观测数据,联合GOES卫星及数字测高仪等的数据,研究了一个由M5.6级太阳耀斑引发的地磁钩扰事件的全球响应特征.研究发现：地磁钩扰特征呈现出南北半球与午前/午后的差异,且地磁响应相对于太阳耀斑存在约3 min的滞后现象,而夜侧无明显扰动;利用位于日侧的50余个地磁台站的数据统计分析后发现地磁钩扰幅度呈现正态分布,且在当地时正午附近达到峰值;利用地磁数据反演出钩扰发生时电离层的电流体系Ss和宁静日电流Sq,并用该电流体系解释了此事件中地磁数据的变化特征.另外,本文初步统计了1996-2015年的地磁钩扰事件数以及相关的太阳耀斑事件数,分析后发现X级耀斑引发地磁钩扰的可能性最大,达42%,由M级耀斑引发的地磁钩扰事件数最多,A、B、C级等小耀斑引发地磁钩扰的可能性很小. 相似文献
2.
为研究太阳耀斑的短期生物效应,统计分析了198-199年中16万婴儿出生日与光学耀斑的关系. 结果表明,婴儿出生数的变化与耀斑辐射的能量,以及能量到达地球的时间有关. 太阳活动较平稳年白天爆发的各级耀斑的当天都对应着一个平均出生数高峰,而且耀斑的亮度和面积越大,对应的出生峰值越大. 2B耀斑当天平均出生数超过前后21d总均值的13.6髎,具有p＜0.001的统计高度显著性水平. 这些出生高峰与耀斑的电磁和高能辐射有关. 2B、2N和1B三类耀斑后的第2-4d还有一个出生峰,它们与耀斑引发的地球物理变化的时间符合. 相似文献
3.
The results of a three-dimensional MHD simulation and data obtained using specialized spacecraft made it possible to construct
an electrodynamic model of solar flares. A flare results from explosive magnetic reconnection in a current sheet above an
active region, and electrons accelerated in field-aligned currents cause hard X rays on the solar surface. In this review,
we considered works where the boundary and initial conditions on the photosphere were specified directly from the magnetic
maps, obtained by SOHO MDI in the preflare state, in order to simulate the formation of a current sheet. A numerical solution
of the complete set of MHD equations, performed using the new-generation PERESVET program, demonstrated the formation of several
current sheets before a series of flares. A comparison of the observed relativistic proton spectra and the simulated proton
acceleration along a magnetic field singular line made it possible to estimate the magnetic reconnection rate during a flare
(∼107 cm s−1). Great flares (of the X class) originate after an increase in the active region magnetic flux up to 1022 Mx. 相似文献
4.
A forecasting scheme of geomagnetic activity is presented, based on the analysis of the geoeffectiveness of X-ray flares,
accompanied by Type II and/or Type IV radio bursts (RSP) observed on the solar disc in the years 1996–2004. The neural network
was used to construct this scheme enabling us to determine the probability, with which flares will be followed by a geomagnetic
response of a particular intensity. The successfulness of forecasts produced after the fact depended on the flare class and
on the combination of radio-burst types. In the case of RSP IV, 58% of the geomagnetic responses of X-ray flares of at least
B class were successful. If only RSP II was observed, the forecast was successful only for flares of the X class (67% of successful
forecasts). In the second step, a strong geomagnetic response was correctly forecast after geoeffective flares in 58% of the
cases. The results are in a good agreement with recent papers based on physical modelling.
fridrich@geomag.sk
ph@ig.cas.cz, jboch@ig.cas.cz 相似文献
5.
《Journal of Atmospheric and Solar》2000,62(16):1449-1455
Sympathetic flaring is defined as the initiation of a solar flare as a result of a transient phenomenon occurring elsewhere on the Sun. Discovery of sympathetic flaring or lack thereof, may lead to a greater understanding of the physics of flare initiation. Knowledge of a mechanism for initiating solar flares would also aid in predicting at least some solar flares. Two studies of sympathetic flaring are presented in this paper. The first part of the paper presents a test for sympathetic flaring in flares observed with the Burst and Transient Source Experiment. A Monte Carlo simulation is used to compare the distribution of solar X-ray flares in time to that expected from a time-varying, Poisson distribution. No evidence for sympathetic flaring is found, though it cannot be ruled out. The X-ray flare data also do not allow discovery of sympathetic flares occurring within 2 min of the initial flare. Because the observations do allow for at least some flares to occur sympathetically, the second part of the paper examines one possible mechanism for initiating flares. The mechanism examined is large-scale coronal transients observed by the SOHO/Extreme Ultraviolet Imaging Telescope: EIT waves. A comparison of the rate of flaring in the interval prior to an EIT wave to the rate of flaring while the wave traverses the solar disk shows no increase in the number of flares due to the EIT wave. 相似文献
6.
Based on statistical data and a detailed analysis of geomagnetic response to the hard electromagnetic radiation of the X17
solar flare of September 7, 2005, we considered spatial features of current systems producing the geomagnetic solar flare
effect (SFE). During flares accompanied by intensive X-rays and gamma rays, SFEs are shown to be observed globally, including
the night hemisphere and high latitudes. Cause-effect relations of phenomena under consideration are discussed. 相似文献
7.
JJI甚低频台站信号对太阳耀斑事件的响应特性 总被引：1，自引：0，他引：1
太阳耀斑发生时,日地空间的X射线通量会随之增大,进而影响到地球电离层的电子密度分布,导致地球-电离层波导状态发生改变,因此接收到的甚低频(VLF,Very Low Frequency)信号会表现出对应的扰动现象.2017年9月8日,位于湖北省内武汉和随州两站点的VLF接收机分别监测到与X射线太阳耀斑相关的来自日本宫崎县(130°49′E,32°04′N)的JJI甚低频台站信号(22.2 kHz)的振幅异常事件.分析当日的数据发现JJI信号的振幅对不同的太阳耀斑出现不同的响应类型,而且对于同一个耀斑,两地的信号响应类型不尽相同.通过统计2017—2019年间与太阳耀斑相关的JJI信号振幅扰动事件,发现两接收站点的JJI信号响应类型都与耀斑强度及其发生时间存在一定的关系,且呈现出四种响应类型,即两次上升下降型、先上升后下降型、下降型和上升型,但是四种响应类型的事件占比不同.拟合结果表明信号的扰动幅度与X射线通量的积分成正相关,但是两站点的线性拟合斜率存在差异.JJI信号到武汉和随州均属于近似沿纬度方向的短距离传播,且两接收站点相距较近,因此两传播路径大致相似.研究两路径上JJI信号对太阳耀斑响应的差异性有助于理解VLF信号的传播以及探索其在太阳活动监测方面的应用. 相似文献
8.
A statistical study of pressure changes in the troposphere and lower stratosphere after strong solar flares 总被引：2，自引：0，他引：2
Summary The average change in height of several constant pressure levels in the troposphere and lower stratosphere after a strong solar flare is described. The analysis covers the northern hemisphere north of 10°N and is based on a sample of 81 carefully selected flares from the period July 1957 through December 1959.The statistical significance of the results is tested by drawing a comparison with the results obtained when one applies exactly the same analysis to three samples of 81 random key-dates selected from the same period.Properties of the reaction pattern are (1) it is pronounced at high as well as low latitudes, (2) it consists of alternating cells of positive and negative height change, (3) it is established within six hours after the flare, and (4) the maximum response occurs near the tropopause.It appears more likely that the atmospheric reaction pattern can be attributed to very energetic solar particles rather than to enhanced ultraviolet radiation. 相似文献
9.
10.
As deduced from the data with high spatial resolution obtained at the radio heliographs of the Siberian Solar Radio Telescope
(SSRT, 5.7 GHz) and the Nobeyama radio heliograph (NoRH, 17 GHz), radio brightness centers in the distribution of the Stokes
parameter I are shifted relative to the distribution of the parameter V 1–2 days before an intense flare. It has been shown that this phenomenon can be related to the behavior of quasi-stationary
sources over the inversion line of the radial component of the magnetic field (neutral-line associated sources (NLSs)). These
sources have a brightness temperature up to 106 K and a circular polarization up to 90%. The origination of NLSs is associated
with the outflow of a new magnetic flux into the atmosphere of an active region that is a classical factor of the flare activity.
Therefore, an NLS is a precursor of power solar flares and can be used as a forecast factor. Owing to the high resolution
of the SSRT, the deviation of the observed polarization distribution of microwave radiation of the active region from the
normal one within the solar disk zone containing the active region can be used as a precursor of the preflare state of the
active region. As a result, the single-frequency Tanaka-Enome criterion is modified. The use of the data from two radio heliographs
(SSRT and NoRH) allows us to propose a two-frequency criterion of normal longitudinal zones that is more efficient for short-term
forecasting of solar flares. Preflare features associated with the displacement of brightness centers in I and V, which is manifested as the transformation of NLSs into spot sources, are fine attributes added to forecast according to
the two-frequency criterion. This is illustrated by an example of active region 10930, which produced power proton flares
on December 6 and 13, 2006. 相似文献
11.
The morphological peculiarities of the 1N (N09W22) two-ribbon spotless flare on March 16, 1981, as well as its connection
with a magnetic field, have been considered. In contrast to major flares of the active region, this spotless flare is characterized
by a large-scale development process, a large distance from the magnetic neutral line, and the absence of the spread of the
ribbons. The development of the flare had four periods. At the beginning of each period, a sharp increase in the brightness
of the flare was observed along with a simultaneous decrease in the area of the flare ribbons. The areas of the ribbons varied
synchronously during all of the periods. However, the situation changed abruptly near the maximum: the area of one of the
ribbons increased, whereas the area of the other ribbon decreased. In our opinion, this behavior is a manifestation of real
physical processes in the flare source and was a precursor of the beginning of the flare decay. The magnetic field and its
topology, as well as the cellular structure of the chromosphere, were primarily responsible for the evolution of the flare.
Almost all of the mottles and bright parts of the flare were localized in the immediate vicinity of magnetic hills with field
intensities from 80 to 250 G. The main structural elements of the flare have been identified. A phenomenon called the tunnel
effect has been revealed: the flare progresses inside a tunnel formed by the system of dark arch structures (filaments). The
results indicate that spotless flares apparently constitute a specific class of flare phenomena and the study of them is of
great interest for understanding of the origin of solar flares. 相似文献
12.
N. A. Barkhatov V. N. Obridko S. E. Revunov S. D. Snegirev D. V. Shadrukov O. A. Sheiner 《Geomagnetism and Aeronomy》2016,56(2):249-255
We compare long-period pulsations of the horizontal component of the geomagnetic field at intervals that precede extreme solar flares. To this end, we use the wavelet–skeleton technique to process the geomagnetic field disturbances recorded at magnetic stations over a wide geographical range. The synchronization times of wavelet–skeleton spectral distributions of long-period pulsations of geomagnetic oscillations over all magnetic stations are shown as normalized histograms. A few days before an intense solar flare, the histograms show extremes. This means that these extremes can be regarded as flare precursors. The same technique is used to analyze the parameters of near-Earth space. The histograms obtained in this case are free of the aforementioned extrema and, therefore, cannot point to an upcoming flare. The goal of this study is to construct a correlation–spectral method for the short-term prediction of solar flare activity. 相似文献
13.
The measurements of an increase in the total electron content (TEC) of the ionosphere during solar flares, obtained based
on the GPS data, indicated that up to 30% of TEC increments corresponded to the ionospheric regions above 300 km altitude
in some cases, and TEC increased mainly below altitudes of 300 km in other cases. The theoretical model of the ionosphere
and plasmasphere was used to study the obtained effects. The altitude-time variations in the charged particle density in the
ionospheric region from 100 to 1000 km were used depending on the solar flare spectrum. An analysis of the modeling results
indicated that an intensification of the flare UV emission in the 55–65 and 85–95 nm spectral ranges results in a pronounced
increase in the electron density in the topside ionosphere (above 300 km). The experimental dependences of the ionospheric
TEC response amplitude on the localization and peak power of flares on the Sun in the X-ray range, obtained based on the GPS
data, are also presented in the work. 相似文献
14.
Coronal mass ejections (CMEs) and solar flares are the large-scale and most energetic eruptive phenomena in our solar system and able to release a large quantity of plasma and magnetic flux from the solar atmosphere into the solar wind. When these high-speed magnetized plasmas along with the energetic particles arrive at the Earth, they may interact with the magnetosphere and ionosphere, and seriously affect the safety of human high-tech activities in outer space. The travel time of a CME to 1 AU is about 1–3 days, while energetic particles from the eruptions arrive even earlier. An efficient forecast of these phenomena therefore requires a clear detection of CMEs/flares at the stage as early as possible. To estimate the possibility of an eruption leading to a CME/flare, we need to elucidate some fundamental but elusive processes including in particular the origin and structures of CMEs/flares. Understanding these processes can not only improve the prediction of the occurrence of CMEs/flares and their effects on geospace and the heliosphere but also help understand the mass ejections and flares on other solar-type stars. The main purpose of this review is to address the origin and early structures of CMEs/flares, from multi-wavelength observational perspective. First of all, we start with the ongoing debate of whether the pre-eruptive configuration, i.e., a helical magnetic flux rope (MFR), of CMEs/flares exists before the eruption and then emphatically introduce observational manifestations of the MFR. Secondly, we elaborate on the possible formation mechanisms of the MFR through distinct ways. Thirdly, we discuss the initiation of the MFR and associated dynamics during its evolution toward the CME/flare. Finally, we come to some conclusions and put forward some prospects in the future. 相似文献
15.
The influence of the spectral nature and position on the solar disk of solar flares related to the production of magnetic effects on earth (from now on, sfe) over a more than 30-year period has been studied. Regarding the spectral issue, we found that the probability of a flare to produce sfe depends on the spectral band in which we observe it, being higher when the flare is important both in Hα and X-ray emissions. On the other hand, Hα and X-ray emissions have been considered in many different divisions of the solar surface and their effectiveness on sfe production have been compared. We found that there is not any privileged region on the solar disk for sfe production. These results end with the controversy generated by distinct conclusions obtained in classical studies on the subject. 相似文献
16.
M. I. Divlekeev 《Geomagnetism and Aeronomy》2012,52(8):1044-1049
The observations of active region (AR) NOAA 10792 in the Ca II 8498 ? line with an ATB-1 solar telescope at the Sternberg State Astronomical Institute, Moscow State University (SSAI MSU) on July 30, 2005, are illustrated, and the events are analyzed using the data obtained on spacecraft. Three flares and accompanying coronal mass ejections (CMEs) are considered. It has been indicated that the beginning of the first compact CME lagged behind the flare onset by 3 min. Plasma ascended with acceleration that reached 0.4 km/s2 at the flare maximum. The matter was also apparently accelerated after the flare maximum, since an ejection could only appear at the edge of the occulting C 2 LASCO coronograph disk at 0557 UT when acceleration is about 0.5 km/s2. The second CME (of the halo type) leaded the beginning of the corresponding flare. 相似文献
17.
18.
《Journal of Atmospheric and Solar》2007,69(13):1587-1598
In this paper, we investigate the solar flare effects of the ionosphere at middle latitude with a one-dimensional ionosphere theoretical model. The measurements of solar irradiance from the SOHO/Solar EUV Monitor (SEM) and GOES satellites have been used to construct a simple time-dependent solar flare spectrum model, which serves as the irradiance spectrum during solar flares. The model calculations show that the ionospheric responses to solar flares are largely related to the solar zenith angle. During the daytime most of the relative increases in electron density occur at an altitude lower than 300 km, with a peak at about 115 km, whereas around sunrise and sunset the strongest ionospheric responses occur at much higher altitudes (e.g. 210 km for a summer flare). The ionospheric responses to flares in equinox and winter show an obvious asymmetry to local midday with a relative increase in total electron content (TEC) in the morning larger than that in the afternoon. The flare-induced TEC enhancement increases slowly around sunrise and reaches a peak at about 60 min after the flare onset. 相似文献
19.
日地系统学中的太阳活动研究（Ⅱ）爆发型太阳活动—太阳耀斑 总被引：1，自引：0，他引：1
爆发型太阳活动是日地系统中重要的扰动源。本文介绍日地系统学中最剧烈的爆发型太阳活动－太阳耀斑的观测研究进展。综述了最近两个太阳周的地面与空间观测所得到的耀斑的物理图象和统计性质，简单讨论了空间观测设备的发展和面临的研究课题。 相似文献
20.
N. S. Shilova 《Geomagnetism and Aeronomy》2008,48(6):709-712
The duration of elementary eruption process and intervals between them for flares of different importance have been determined based on the photometric data for flares, observed by a TRACE spacecraft at a wavelength of 195 Å. It has been revealed that the values of these parameters increase with increasing flare importance. It is assumed that the appearance of elementary nonstationary flare centers correlates with the origination of solitons at self-organized criticality. 相似文献