Blazars are the most violent steady/recurrent sources of high-energy gamma-ray emission in the known Universe. They are prominent
emitters of electromagnetic radiation throughout the entire electromagnetic spectrum. The observable radiation most likely
originates in a relativistic jet oriented at a small angle with respect to the line of sight. This review starts out with
a general overview of the phenomenology of blazars, including results from a recent multiwavelength observing campaign on
3C279. Subsequently, issues of modeling broadband spectra will be discussed. Spectral information alone is not sufficient
to distinguish between competing models and to constrain essential parameters, in particular related to the primary particle
acceleration and radiation mechanisms in the jet. Short-term spectral variability information may help to break such model
degeneracies, which will require snap-shot spectral information on intraday time scales, which may soon be achievable for
many blazars even in the gamma-ray regime with the upcoming GLAST mission and current advances in Atmospheric Cherenkov Telescope
technology. In addition to pure leptonic and hadronic models of gamma-ray emission from blazars, leptonic/hadronic hybrid
models are reviewed, and the recently developed hadronic synchrotron mirror model for TeV γ-ray flares which are not accompanied by simultaneous X-ray flares (“orphan TeV flares”) is revisited.
The U.S. Government’s right to retain a non-exclusive, royalty-free license in and to any copyright is acknowledged. 相似文献
We study transverse loop oscillations triggered by 17flares and filament destabilizations; only 2 such cases have been reported
in the literature until now. Oscillation periods are estimated to range over a factor of ∼15, with most values between 2 and
7 min. The oscillations are excited by filament destabilizations or flares (in 6% of the 255 flares inspected, ranging from
about C3 to X2). There is no clear dependence of oscillation amplitude on flare magnitude. Oscillations occur in loops that
close within an active region, or in loops that connect an active region to a neighboring region or to a patch of strong flux
in the quiet Sun. Some magnetic configurations are particularly prone to exhibit oscillations: two active regions showed two,
and one region even three, distinct intervals with loop oscillations. The loop oscillations are not a resonance that builds
up: oscillations in loops that are excited along their entire length are likely to be near the fundamental resonance mode
because of that excitation profile, but asymmetrically excited oscillations clearly show propagating waves that are damped
too quickly to build up a resonance, and some cases show multiple frequencies. We discuss evidence that all oscillating loops
lie near magnetic separatrices that outline the large-scale topology of the field. All magnetic configurations are more complicated
than a simple bipolar region, involving mixed-polarities in the interior or vicinity of the region; this may reflect that
the exciting eruptions occur only in such environments, but this polarity mixing likely also introduces the large-scale separatrices
that are involved. Often the oscillations occur in conjunction with gradual adjustments in loop positions in response to the
triggering event. We discuss the observations in the context of two models: (a) transverse waves in coronal loops that act
as wave guides and (b) strong sensitivity to changes in the field sources for field lines near separatrices. Properties that
favor model b are (1) the involvement of loops at or near separatrices that outline the large-scale topology of the field,
(2) the combined occurrence of oscillations and loop translations, (3) the small period spread and similar decay time scale
in a set of oscillating loops in one well-observed event, and (4) the existence of loops oscillating in antiphase with footpoints
close together in two cases. All other properties are compatible with either model, except the fact that almost all of the
oscillations start away from the triggering event, suggestive of an outward-pushing exciting wave more in line with model
a. The spread in periods from event to event suggests that the oscillations may reflect the properties of some driver mechanism
that is related to the flare or mass ejection.
Supplementary material to this paper is available in electronic form at http://dx.doi.org/10.1023/A:1014957715396 相似文献
EUV images show the solar corona in a typical temperature range of T >rsim 1 MK, which encompasses the most common coronal structures: loops, filaments, and other magnetic structures in active regions,
the quiet Sun, and coronal holes. Quantitative analysis increasingly demands automated 2D feature recognition and 3D reconstruction,
in order to localize, track, and monitor the evolution of such coronal structures. We discuss numerical tools that “fingerprint”
curvi-linear 1D features (e.g., loops and filaments). We discuss existing finger-printing algorithms, such as the brightness-gradient
method, the oriented-connectivity method, stereoscopic methods, time-differencing, and space–time feature recognition. We
discuss improved 2D feature recognition and 3D reconstruction techniques that make use of additional a priori constraints, using guidance from magnetic field extrapolations, curvature radii constraints, and acceleration and velocity
constraints in time-dependent image sequences. Applications of these algorithms aid the analysis of SOHO/EIT, TRACE, and STEREO/SECCHI
data, such as disentangling, 3D reconstruction, and hydrodynamic modeling of coronal loops, postflare loops, filaments, prominences,
and 3D reconstruction of the coronal magnetic field in general. 相似文献
The development and numerical values of the new absolute phase-center correction model for GPS receiver and satellite antennas, as adopted by the International GNSS (global navigation satellite systems) Service, are presented. Fixing absolute receiver antenna phase-center corrections to robot-based calibrations, the GeoForschungsZentrum Potsdam (GFZ) and the Technische Universität München reprocessed more than 10 years of GPS data in order to generate a consistent set of nadir-dependent phase-center variations (PCVs) and offsets in the z-direction pointing toward the Earth for all GPS satellites in orbit during that period. The agreement between the two solutions estimated by independent software packages is better than 1 mm for the PCVs and about 4 cm for the z-offsets. In addition, the long time-series facilitates the study of correlations of the satellite antenna corrections with several other parameters such as the global terrestrial scale or the orientation of the orbital planes with respect to the Sun. Finally, completely reprocessed GPS solutions using different phase-center correction models demonstrate the benefits from switching from relative to absolute antenna phase-center corrections. For example, tropospheric zenith delay biases between GPS and very long baseline interferometry (VLBI), as well as the drift of the terrestrial scale, are reduced and the GPS orbit consistency is improved. 相似文献
Boundary-Layer Meteorology - Lagrangian particle dispersion models (LPDMs) are frequently used for regional-scale inversions of greenhouse gas emissions. However, the turbulence parameterizations... 相似文献
Holocene climate variability is punctuated by episodic climatic events such as the Little Ice Age (LIA) predating the industrial-era warming. Their dating and forcing mechanisms have however remained controversial. Even more crucially, it is uncertain whether earlier events represent climatic regimes similar to the LIA. Here we produce and analyse a new 7500-year long palaeoclimate record tailored to detect LIA-like climatic regimes from northern European tree-ring data. In addition to the actual LIA, we identify LIA-like ca. 100–800 year periods with cold temperatures combined with clear sky conditions from 540 CE, 1670 BCE, 3240 BCE and 5450 BCE onwards, these LIA-like regimes covering 20% of the study period. Consistent with climate modelling, the LIA-like regimes originate from a coupled atmosphere–ocean–sea ice North Atlantic-Arctic system and were amplified by volcanic activity (multiple eruptions closely spaced in time), tree-ring evidence pointing to similarly enhanced LIA-like regimes starting after the eruptions recorded in 1627 BCE, 536/540 CE and 1809/1815 CE. Conversely, the ongoing decline in Arctic sea-ice extent is mirrored in our data which shows reversal of the LIA-like conditions since the late nineteenth century, our record also correlating highly with the instrumentally recorded Northern Hemisphere and global temperatures over the same period. Our results bridge the gaps between low- and high-resolution, precisely dated proxies and demonstrate the efficacy of slow and fast components of the climate system to generate LIA-like climate regimes.
Natural Hazards - Himalayan mountains are one of the most seismo-tectonically active zones on the surface of the earth. Recurring moderate and high magnitude earthquakes are not uncommon in this... 相似文献
The corona associated with an active region is structured by high-temperature, magnetically dominated closed and open loops. The projected 2D geometry of these loops is captured in EUV filtergrams. In this study using SDO/AIA 171 Å filtergrams, we expand our previous method to derive the 3D structure of these loops, independent of heliostereoscopy. We employ an automated loop recognition scheme (Occult-2) and fit the extracted loops with 2D cubic Bézier splines. Utilizing SDO/HMI magnetograms, we extrapolate the magnetic field to obtain simple field models within a rectangular cuboid. Using these models, we minimize the misalignment angle with respect to Bézier control points to extend the splines to 3D (Gary, Hu, and Lee 2014). The derived Bézier control points give the 3D structure of the fitted loops. We demonstrate the process by deriving the position of 3D coronal loops in three active regions (AR 11117, AR 11158, and AR 11283). The numerical minimization process converges and produces 3D curves which are consistent with the height of the loop structures when the active region is seen on the limb. From this we conclude that the method can be important in both determining estimates of the 3D magnetic field structure and determining the best magnetic model among competing advanced magnetohydrodynamics or force-free magnetic-field computer simulations. 相似文献