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31.
Using data from the Transition Region and Coronal Explorer (TRACE), Solar and Heliospheric Observatory (SOHO), Ramaty High Energy Solar Spectroscopic Imager (RHESSI), and Hida Observatory (HO), we present a detailed study of an EUV jet and the associated Hα filament eruption in
a major flare in the active region NOAA 10044 on 29 July 2002. In the Hα line wings, a small filament was found to erupt out
from the magnetic neutral line of the active region during the flare. Two bright EUV loops were observed rising and expanding
with the filament eruption, and both hot and cool EUV plasma ejections were observed to form the EUV jet. The two thermal
components spatially separated from each other and lasted for about 25 minutes. In the white-light corona data, a narrow coronal
mass ejection (CME) was found to respond to this EUV jet. We cannot find obvious emerging flux in the photosphere accounting
for the filament eruption and the EUV jet. However, significant sunspot decay and magnetic-flux cancelation owing to collision
of opposite flux before the events were noticed. Based on the hard X-ray data from RHESSI, which showed evidence of magnetic
reconnection along the main magnetic neutral line, we think that all of the observed dynamical phenomena, including the EUV
jet, filament eruption, flare, and CME, should have a close relation to the flux cancelation in the low atmosphere. 相似文献
32.
New X-ray observations of the north polar region taken from the X-ray Telescope (XRT) of the Hinode spacecraft are used to analyze several time sequences showing small loop brightenings with a long ray above. We focus on
the formation of the jet and discuss scenarios to explain the main features of the events: the relationship with the expected
surface magnetism, the rapid and sudden radial motion, and possibly the heating, based on the assumption that the jet occurs
above a null point of the coronal magnetic field. We conclude that 2-D reconnection models should be complemented in order
to explain the observational details of these events and suggest that alternative scenarios may exist. 相似文献
33.
利用美国甚长基线阵对3个致密陡谱源3C43、3C48和3C454进行中心频率1.6GHz的观测,获得总流量图和各个子源的结构等信息.对比已有的数据,分析源3C43和3C454的流量变化和各个子源的位置移动,发现3C43的总流量、各子源流量、各子源的相对位置在14年内比较稳定;3C454的总流量和各子源流量也比较稳定,但两个子源相对核心的偏离速度分别是光速的21.6和17.7倍,存在明显的视超光速现象.同时通过对L波段4个频率的总流量结果进行谱指数拟合,获得源3C43和3C454的谱指数分别是0.63和0.86,符合致密陡谱源谱指数α≥0.5的定义,也与已有的结果吻合较好. 相似文献
34.
Philippe André 《Astrophysics and Space Science》1995,224(1-2):29-42
The use of sensitive receivers on large ground-based radiotelescopes such as the JCMT, the IRAM 30 m MRT, and the VLA has recently yielded significant progress in our observational understanding of low-mass protostars. Submillimeter continuum observations suggest that the youngest stellar objects detected in the near-/mid-IR range -the so-called Class I sources or infrared protostars - have only residual amounts of circumstellar material and are thus relatively evolved. At the same time, a smaller number of colder and more obscured YSOs - designated Class 0 - characterized by virtually no emission below 10µm but strong submillimeter emission have been identified. These Class 0 or submillimeter protostars have not yet assembled the bulk of their final stellar mass, and correspond to the youngest protostar stage known to date (probable age 104 yr). Direct evidence for gravitational infall has been found in some of these sources confirming their protostellar nature. However, most (if not all) Class 0 protostars already drive highly collimated CO outflows. 相似文献
35.
利用国家自动气象站和ECMWF-interim再分析资料,从高低空急流的角度对2016年7月1—4日安徽沿江地区的连续性暴雨的成因进行了探讨。研究表明,7月1—4日,高空急流出现明显的北跳、强度增强,低层西南急流强度则达到2016年最大值。伴随着高低空急流的异常变化,在安徽沿江地区上空形成了强烈的高空辐散和低空辐合,同时高低空急流耦合激发形成次级环流,使得旺盛的上升运动一直延伸至对流层上层。高低空急流耦合在1—2日比较强烈,3日起耦合强度逐渐减弱,导致小时雨强进一步减弱。另一方面,低空急流的增强也使得孟加拉湾的水汽源源不断的输送至安徽沿江地区,近地面至3 000 m高度上南风输送为沿江地区连续性暴雨提供了充沛的水汽。 相似文献
36.
In May 1995, we obtained 5-GHz VLBI polarisation observations of 20 sources in the complete sample of BL Lac objects defined by H. Kühr and G. Schmidt. Ten antennas participated in the global VLBI observations. Total intensity and linear polarisation images of five sources have been made and analysed thus far. The images for 0003–066, 1538+149, and 2254+074 are presented, together with an analysis of the evolution of their polarisation structure and estimates of apparent velocities for components in their VLBI jets. 相似文献
37.
38.
The Extreme ultraviolet Imaging Spectrometer (EIS) onboard Hinode is the first solar telescope to obtain wide-slit spectral images that can be used for detecting Doppler flows in transition
region and coronal lines on the Sun and to relate them to their surrounding small-scale dynamics. We select EIS lines covering
the temperature range 6×104 to 2×106 K that give spectrally pure images of the Sun with the 40-arcsec slit. In these images Doppler shifts are seen as horizontal
brightenings. Inside the image it is difficult to distinguish shifts from horizontal structures but emission beyond the image
edge can be unambiguously identified as a line shift in several lines separated from others on their blue or red side by more
than the width of the spectrometer slit (40 pixels). In the blue wing of He ii, we find a large number of events with properties (size and lifetime) similar to the well-studied explosive events seen in
the ultraviolet spectral range. Comparison with X-Ray Telescope (XRT) images shows many Doppler shift events at the footpoints
of small X-ray loops. The most spectacular event observed showed a strong blue shift in the transition region and lower corona
lines from a small X-ray spot that lasted less than 7 min. The emission appears to be near a cool coronal loop connecting
an X-ray bright point to an adjacent region of quiet Sun. The width of the emission implies a line-of-sight velocity of 220 km s−1. In addition, we show an example of an Fe xv shift with a velocity of about 120 km s−1, coming from what looks like a narrow loop leg connecting a small X-ray brightening to a larger region of X-ray emission. 相似文献
39.
The role of spring Wyrtki jets in modulating the equatorial Indian Ocean and the regional climate is an unexplored problem. The source of interannual variability in the spring Wyrtki jets is explored in this study. The relationship between intraseasonal and interannual variability from 1958 to 2008 and its relation with Indian Summer Monsoon is further addressed. Analysis reveals that the interannual variability in spring Wyrtki jets is controlled significantly by their intraseasonal variations. These are mostly defined by a single intraseasonal event of duration 20 days or more which either strengthens or weakens the seasonal mean jet depending on its phase. The strong spring jets are driven by such intraseasonal westerly wind bursts lasting for 20-days or more, whereas the weak jets are driven by weaker intraseasonal westerlies. During the years of strong jets, the conventional westward phase propagation of Wyrtki jets is absent and instead there is an eastward phase propagation indicating the possible role of Madden Julian Oscillation (MJO) in strengthening the spring Wyrtki jets. These strong intraseasonal westerly wind bursts with eastward phase propagation during strong years are observed mainly in late spring and have implications on June precipitation over the Indian and adjoining land mass. Anomalously strong eastward jets accumulate warm water in the eastern equatorial Indian Ocean (EIO), leading to anomalous positive upper ocean heat content and supporting more local convection in the east. This induces subsidence over the Indian landmass and alters monsoon rainfall by modulating monsoon Hadley circulation. In case of weak current years such warm anomalies are absent over the eastern EIO. Variations in the jet strength are found to have strong impact on sea level anomalies, heat content, salinity and sea surface temperature over the equatorial and north Indian Ocean making it a potentially important player in the north Indian Ocean climate variability. 相似文献
40.
S. Cabrit 《Astrophysics and Space Science》1995,233(1-2):81-96
In this contribution, I present a broad historical review of the various hydrodynamical models that have been considered for explaining molecular outflows, and of their merits and failures when compared with observations. Wind-driven bubbles, viscous jet mixing-layers, and jet bowshocks, are discussed in turn. Most general properties of outflows can be understood in terms of a simple bowshock model. However, the detailed structure of outflows is more complex and not yet fully understood, given the presence of time variability in the jet velocity and/or direction. Finally, I discuss constraints on wind properties (momentum, mass-loss rate, radius) that can be derived from molecular outflows driven by jet bowshocks. 相似文献