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Solar Energetic Particle Event of 2005 January 20: Release Times and Possible Sources 总被引:1,自引:0,他引:1
Gui-Ming Le Yu-Hua Tang Yan-Ben Han National Astronomical Observatories Chinese Academy of Sciences Beijing Key Laboratory of Radiometric Calibration Validation for Environmental Satellites China Meteorological Administration Beijing Department of Astronomy Nanjing University Nanjing National Center for Space Weather China Meteorological Administration Beijing 《中国天文和天体物理学报》2006,6(6):751-758
Based on cosmic ray data obtained by neutron monitors at the Earth's surface, and data on near-relativistic electrons measured by the WIND satellite, as well as on solar X-ray and radio burst data, the solar energetic particle (SEP) event of 2005 January 20 is studied. The results show that this event is a mixed event where the flare is dominant in the acceleration of the SEPs, the interplanetary shock accelerates mainly solar protons with energies below 130 MeV, while the relativistic protons are only accelerated by the solar flare. The interplanetary shock had an obvious acceleration effect on relativistic electrons with energies greater than 2 MeV. It was found that the solar release time for the relativistic protons was about 06:41 UT, while that for the near-relativistic electrons was about 06:39 UT. The latter turned out to be about 2 min later than the onset time of the interplanetary type III burst. 相似文献
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von Rosenvinge T. T. Richardson I. G. Reames D. V. Cohen C. M. S. Cummings A. C. Leske R. A. Mewaldt R. A. Stone E. C. Wiedenbeck M. E. 《Solar physics》2009,256(1-2):443-462
Solar Physics - The solar energetic particle event on 14 December 2006 was observed by several near-Earth spacecraft including the Advanced Composition Explorer (ACE), STEREO A and B, SOHO and... 相似文献
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Donald V. Reames 《Solar physics》2014,289(3):977-993
This is a study of abundances of the elements He, C, N, O, Ne, Mg, Si, S, Ar, Ca, and Fe in solar energetic particles (SEPs) in the 2?–?15 MeV?amu?1 region measured on the Wind spacecraft during 54 large SEP events occurring between November 1994 and June 2012. The origin of most of the temporal and spatial variations in abundances of the heavier elements lies in rigidity-dependent scattering during transport of the particles away from the site of acceleration at shock waves driven out from the Sun by coronal mass ejections (CMEs). Variation in the abundance of Fe is correlated with the Fe spectral index, as expected from scattering theory but not previously noted. Clustering of Fe abundances during the “reservoir” period, late in SEP events, is also newly reported. Transport-induced enhancements in one region are balanced by depletions in another, thus, averaging over these variations produces SEP abundances that are energy independent, confirms previous SEP abundances in this energy region, and provides a credible measure of element abundances in the solar corona. These SEP-determined coronal abundances differ from those in the solar photosphere by a well-known function that depends upon the first ionization potential (FIP) or ionization time of the element. 相似文献
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A. Hillaris O. Malandraki K.-L. Klein P. Preka-Papadema X. Moussas C. Bouratzis E. Mitsakou P. Tsitsipis A. Kontogeorgos 《Solar physics》2011,273(2):493-509
On 17 January 2005 two fast coronal mass ejections were recorded in close succession during two distinct episodes of a 3B/X3.8
flare. Both were accompanied by metre-to-kilometre type-III groups tracing energetic electrons that escape into the interplanetary
space and by decametre-to-hectometre type-II bursts attributed to CME-driven shock waves. A peculiar type-III burst group
was observed below 600 kHz 1.5 hours after the second type-III group. It occurred without any simultaneous activity at higher
frequencies, around the time when the two CMEs were expected to interact. We associate this emission with the interaction
of the CMEs at heliocentric distances of about 25 R
⊙. Near-relativistic electrons observed by the EPAM experiment onboard ACE near 1 AU revealed successive particle releases
that can be associated with the two flare/CME events and the low-frequency type-III burst at the time of CME interaction.
We compare the pros and cons of shock acceleration and acceleration in the course of magnetic reconnection for the escaping
electron beams revealed by the type-III bursts and for the electrons measured in situ. 相似文献
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R. A. Leske C. M. S. Cohen R. A. Mewaldt E. R. Christian A. C. Cummings A. W. Labrador E. C. Stone M. E. Wiedenbeck T. T. von Rosenvinge 《Solar physics》2012,281(1):301-318
The solar particle event observed at STEREO Ahead on 18?August 2010 displayed a rich variety of behavior in the particle anisotropies. Sectored rates measured by the Low Energy Telescope (LET) on STEREO showed very large bidirectional anisotropies in 4??C?6?MeV protons for the first ???17?hours of the event while inside a magnetic cloud, with intensities along the field direction several hundred to nearly 1000 times greater than those perpendicular to the field. At the trailing end of the cloud, the protons became isotropic and their spectrum hardened slightly, while the He/H abundance ratio plunged by a factor of approximately four for about four hours. Associated with the arrival of a shock on 20?August was a series of brief (<?10?minute duration) intensity increases (commonly called ??shock spikes??) with relatively narrow angular distributions (???45° FWHM), followed by an abrupt decrease in particle intensities at the shock itself and a reversal of the proton flow to a direction toward the Sun and away from the receding shock. We discuss the STEREO/LET observations of this interesting event in the context of other observations reported in the literature. 相似文献
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We study the spatial distribution of solar energetic particles (SEPs) throughout the inner heliosphere during six large SEP events from the period 1977 through 1979, as deduced from observations on the Helios 1 and 2, IMP 7 and 8, ISEE 3, and Voyager 1 and 2 spacecraft. Evidence of intensity maxima associated with the expanding shock wave is commonly seen along its central and western flanks, although the region of peak acceleration or “nose” of the shock is sometimes highly localized in longitude. In one event (1 January 1978) a sharp peak in 20?–?30 MeV proton intensities is seen more strongly by Voyager at ~?2 AU than it is by spacecraft at nearby longitudes at ~?1 AU. Large spatial regions, or “reservoirs,” often exist behind the shocks with spatially uniform SEP intensities and invariant spectra that decrease adiabatically with time as their containment volume expands. Reservoirs are seen to sweep past 0.3 AU and can extend out many AU. Boundaries of the reservoirs can vary with time and with particle velocity, rather than rigidity. In one case, a second shock wave from the Sun reaccelerates protons that retain the same hard spectrum as protons in the reservoir from the preceding SEP event. Thus reservoirs can provide not only seed particles but also a “seed spectrum” with a spectral shape that is unchanged by a weaker second shock. 相似文献
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The SOL2001-12-26 moderate solar eruptive event (GOES importance M7.1, microwaves up to 4000 sfu at 9.4 GHz, coronal mass ejection (CME) speed 1446 km?s?1) produced strong fluxes of solar energetic particles and ground-level enhancement (GLE) of cosmic-ray intensity (GLE63). To find a possible reason for the atypically high proton outcome of this event, we study multi-wavelength images and dynamic radio spectra and quantitatively reconcile the findings with each other. An additional eruption probably occurred in the same active region about half an hour before the main eruption. The latter produced two blast-wave-like shocks during the impulsive phase. The two shock waves eventually merged around the radial direction into a single shock traced up to \(25~\mathrm{R}_{\odot}\) as a halo ahead of the expanding CME body, in agreement with an interplanetary Type II event recorded by the Radio and Plasma Wave Investigation (WAVES) experiment on the Wind spacecraft. The shape and kinematics of the halo indicate an intermediate regime of the shock between the blast wave and bow shock at these distances. The results show that i) the shock wave appeared during the flare rise and could accelerate particles earlier than usually assumed; ii) the particle event could be amplified by the preceding eruption, which stretched closed structures above the developing CME, facilitated its lift-off and escape of flare-accelerated particles, enabled a higher CME speed and stronger shock ahead; iii) escape of flare-accelerated particles could be additionally facilitated by reconnection of the flux rope, where they were trapped, with a large coronal hole; and iv) the first eruption supplied a rich seed population accelerated by a trailing shock wave. 相似文献
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Lanzerotti L.J. Medford L.V. Maclennan C.G. Kraus J.S. Kappenman J. Radasky W. 《Solar physics》2001,204(1-2):351-359
The large solar activity in mid-July 2000 produced a severe geomagnetic storm at Earth during the last half of 15 July universal
time. The enhancements and changes in the ionosphere electrical current systems caused large geopotentials to be induced over
oceanic distances. Across the northern Atlantic, from New Jersey to near the French coast, a geopotential as large as 0.05 V km−1 (a peak-to-peak voltage of about 300 V) was measured during the geomagnetic storm. While large, this was not among the four
largest such geopotentials that have been recorded in the last 60 years across AT&T telecommunications cable routes, ocean
and continental. The geomagnetic and geopotential data that were measured during the storm event are presented and discussed. 相似文献
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On 11 January 2002, using the Multi-channel Infrared Solar Spectrograph (MISS) at the Purple Mountain Observatory (PMO), we obtained Hα, Ca ii 8542 Å and He i 10?830 Å spectra and slit-jaw Hα images of a peculiar solar limb event. A close resemblance of its intensity to that of a small flare and the GOES X-ray flux indicates that it was an active prominence. However, its morphological evolution and velocity variation were different from general typical active prominences, such as limb flares, post-flare loops, surges and sprays. It started with the ejection of material from the flare site. In the early phase, the ejecta was as bright as a limb flare and kept rising until reaching the height of (8????10)×104 km at an almost constant velocity of 91.7 km? s ?1 with its lower part always connected to the solar surface. EUV images in 195 Å show similar structure as in the Hα line, indicating the coexistence of plasmas with temperatures differing by more than two orders of magnitude. Later some material started to fall back to another bright area on the solar surface. The falling material did not show the collimated structure of surges or the arc structure of flaring arches. A red-shift velocity of more than 200 km? s ?1 was detected in a bright point close to the outer edge of the closed loop system formed later, which dispersed in a few minutes and became a part of the newly formed large loop. The ejected material did not leave the sun, indicating that the magnetic reconnection was not sufficient to remove the overlying field lines during the process. The spectral line profiles showed large widths and variable velocities, and therefore the line-pair method is not applicable to this event for the estimation of physical parameters. 相似文献
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Solar Physics - We analyzed the temporal variation of energetic particles measured by the Low Energy Telescope (LET), the Kiel Electron Telescope (KET), and the High Energy Telescope (HET)... 相似文献
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Caroubalos C. Alissandrakis C.E. Hillaris A. Nindos A. Tsitsipis P. Moussas X. Bougeret J.-L. Bouratzis K. Dumas G. Kanellakis G. Kontogeorgos A. Maroulis D. Patavalis N. Perche C. Polygiannakis J. Preka-Papadema P. 《Solar physics》2001,204(1-2):165-177
In this report we present a complex metric burst, associated with the 14 July 2000 major solar event, recorded by the ARTEMIS-IV
radio spectrograph at Thermopylae. Additional space-borne and Earth-bound observational data are used, in order to identify
and analyze the diverse, yet associated, processes during this event. The emission at metric wavelengths consisted of broad-band
continua including a moving and a stationary type IV, impulsive bursts and pulsating structures. The principal release of
energetic electrons in the corona was 15–20 min after the start of the flare, in a period when the flare emission spread rapidly
eastwards and a hard X-ray peak occurred. Backward extrapolation of the CME also puts its origin in the same time interval,
however, the uncertainty of the extrapolation does not allow us to associate the CME with any particular radio or X-ray signature.
Finally, we present high time and spectral resolution observations of pulsations and fiber bursts, together with a preliminary
statistical analysis. 相似文献
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A. J. Prise L. K. Harra S. A. Matthews D. M. Long A. D. Aylward 《Solar physics》2014,289(5):1731-1744
Multi-spacecraft observations are used to study the in-situ effects of a large coronal mass ejection (CME) erupting from the farside of the Sun on 3 November 2011, with particular emphasis on the associated solar energetic particle (SEP) event. At that time both Solar Terrestrial Relations Observatory (STEREO) spacecraft were located more than 90 degrees from Earth and could observe the CME eruption directly, with the CME visible on-disk from STEREO-B and off the limb from STEREO-A. Signatures of pressure variations in the corona such as deflected streamers were seen, indicating the presence of a coronal shock associated with this CME eruption. The evolution of the CME and an associated extreme-ultraviolet (EUV) wave were studied using EUV and coronagraph images. It was found that the lateral expansion of the CME low in the corona closely tracked the propagation of the EUV wave, with measured velocities of 240±19 km?s?1 and 221±15 km?s?1 for the CME and wave, respectively. Solar energetic particles were observed to arrive first at STEREO-A, followed by electrons at the Wind spacecraft at L1, then STEREO-B, and finally protons arrived simultaneously at Wind and STEREO-B. By carrying out a velocity-dispersion analysis on the particles arriving at each location, it was found that energetic particles arriving at STEREO-A were released first and that the release of particles arriving at STEREO-B was delayed by about 50 minutes. Analysis of the expansion of the CME to a wider longitude range indicates that this delay is a result of the time taken for the CME edge to reach the footpoints of the magnetic-field lines connected to STEREO-B. The CME expansion is not seen to reach the magnetic footpoint of Wind at the time of solar-particle release for the particles detected here, suggesting that these particles may not be associated with this CME. 相似文献
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Monte Carlo simulations of interplanetary transport are employed to study adiabatic energy losses of solar protons during
propagation in the interplanetary medium. We consider four models. The first model is based on the diffusion-convection equation.
Three other models employ the focused transport approach. In the focused transport models, we simulate elastic scattering
in the local solar wind frame and magnetic focusing. We adopt three methods to treat scattering. In two models, we simulate
a pitch-angle diffusion as successive isotropic or anisotropic small-angle scatterings. The third model treats large-angle
scatterings as numerous small-chance isotropizations. The deduced intensity–time profiles are compared with each other, with
Monte Carlo solutions to the diffusion-convection equation, and with results of the finite-difference scheme by Ruffolo (1995).
A numerical agreement of our Monte Carlo simulations with results of the finite-difference scheme is good. For the period
shortly after the maximum intensity time, including deceleration can increase the decay rate of the near-Earth intensity essentially
more than would be expected based on advection from higher momenta. We, however, find that the excess in the exponential-decay
rate is time dependent. Being averaged over a reasonably long period, the decay rate of the near-Earth intensity turns out
to be close to that expected based on diffusion, convection, and advection from higher momenta. We highlight a variance of
the near-Earth energy which is not small in comparison with the energy lost. It leads to blurring of any fine details in the
accelerated particle spectra. We study the impact of realistic spatial dependencies of the mean free path on adiabatic deceleration
and on the near-Earth intensity magnitude. We find that this impact is essential whenever adiabatic deceleration itself is
important. It is also found that the initial angular distribution of particles near the Sun can markedly affect MeV-proton
energy losses and intensities observed at 1 AU. Computations invoked during the study are described in detail. 相似文献
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Kuznetsov S. N. Bogomolov A. V. Denisov Yu. I. Kordylewski Z. Kudela K. Kurt V. G. Lisin D. V. Myagkova I. N. Podorol'skii A. N. Podosenova T. B. Svertilov S. I. Sylwester J. Stepanov A. I. Yushkov B. Yu. 《Solar System Research》2003,37(2):121-127
Based on X-ray, gamma-ray, and charged-particle measurements with several instruments onboard the Coronas-F satellite and on ACE and GOES experimental data presented on the Internet, we investigate the parameters of the solar flare of November 4, 2001, and the energetic-particle fluxes produced by it in circumterrestrial space. The increase in relativistic-electron fluxes for about 1.5 days points to a moving source (shock front). The structure of the energetic-particles fluxes in the second half of November 5, 2001, can be explained by the passage of the coronal mass ejection that was ejected on November 1, 2001, and that interacted with the shock wave from the flare of November 4, 2001. 相似文献
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Solar Physics - Elemental composition and energy spectra of ~?0.1?–?1.0 MeV/n heavy ions were analyzed in two corotating interaction region (CIR) events... 相似文献
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把地球作为一个开放系统,本文分析了不同地域范围的地震活动和太阳活动的关系,发现不同地域的地震活动也存在着一个大约11年的周期,这个周期可能与太阳活动的11年左右周期有关,但地震周期的峰值对应于太阳活动的下降段。它们的关系是负相关关系。本文进一步着重分析了地震活动与高速太阳风粒子流和宇宙线高能粒子流的关系,发现它们之间存在着一个信度水平很高的正相关。这样,我们可以推测太阳活动可能是通过调制到达地球的高能粒子流进而调制地震活动的。 相似文献
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Share G.H. Murphy R.J. Dennis B.R. Schwartz R.A. Tolbert A.K. Lin R.P. Smith D.M. 《Solar physics》2002,210(1-2):357-372
The RHESSI high-resolution spectrometer detected γ-ray lines and continuum emitted by the Earth's atmosphere during impact
of solar energetic particles in the south polar region from 16:00–17:00 UT on 21 April 2002. The particle intensity at the
time of the observation was a factor of 10–100 weaker than previous events when gamma-rays were detected by other instruments.
This is the first high-resolution observation of atmospheric gamma-ray lines produced by solar energetic particles. De-excitation
lines were resolved that, in part, come from 14N at 728, 1635, 2313, 3890, and 5106 keV, and the 12C spallation product at ∼ 4439 keV. Other unresolved lines were also detected. We provide best-fit line energies and widths
and compare these with moderate resolution measurements by SMM of lines from an SEP event and with high-resolution measurements
made by HEAO 3 of lines excited by cosmic rays. We use line ratios to estimate the spectrum of solar energetic particles that
impacted the atmosphere. The 21 April spectrum was significantly harder than that measured by SMM during the 20 October 1989
shock event; it is comparable to that measured by Yohkoh on 15 July 2000. This is consistent with measurements of 10–50 MeV protons made in space at the time of the γ-ray observations. 相似文献