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J.L. Gómez J.C. Guirado I. Agudo A.P. Marscher A. Alberdi J.M. Marcaide D.C. Gabuzda 《Monthly notices of the Royal Astronomical Society》2001,328(3):873-881
We present multi-epoch 8.4- and 43-GHz Very Long Baseline Array images of the BL Lac object 0735+178. The images confirm the presence of a twisted jet with two sharp apparent bends of 90° within two milliarcseconds of the core, resembling a helix in projection. The observed twisted geometry could be the result of precession of the jet inlet, but is more likely produced by pressure gradients in the external medium through which the jet propagates. Quasi-stationary components are observed at the locations of the 90° bends, possibly produced by differential Doppler boosting.
Identification of components across epochs, since the earliest VLBI observations of this source in 1979.2, proves difficult due to the sometimes large time gaps between observations. One possible identification suggests the existence of superluminal components following non-ballistic trajectories with velocities up to . However, in images obtained after mid-1995, components show a remarkable tendency to cluster near several jet positions, suggesting a different scenario in which components have remained nearly stationary in time, at least since mid-1995. Comparison with the earlier published data, covering more than 19 years of observations, suggests a striking qualitative change in the jet trajectory sometime between mid-1992 and mid-1995, with the twisted jet structure with stationary components becoming apparent only at the later epochs. This would require a re-evaluation of the physical parameters estimated for 0735+178, such as the observing viewing angle, the plasma bulk Lorentz factor, and those deduced from these. 相似文献
Identification of components across epochs, since the earliest VLBI observations of this source in 1979.2, proves difficult due to the sometimes large time gaps between observations. One possible identification suggests the existence of superluminal components following non-ballistic trajectories with velocities up to . However, in images obtained after mid-1995, components show a remarkable tendency to cluster near several jet positions, suggesting a different scenario in which components have remained nearly stationary in time, at least since mid-1995. Comparison with the earlier published data, covering more than 19 years of observations, suggests a striking qualitative change in the jet trajectory sometime between mid-1992 and mid-1995, with the twisted jet structure with stationary components becoming apparent only at the later epochs. This would require a re-evaluation of the physical parameters estimated for 0735+178, such as the observing viewing angle, the plasma bulk Lorentz factor, and those deduced from these. 相似文献
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Characterizing the spatial and temporal variation in surface hydrological dynamics of large boreal landscapes is vital, since these patterns define the occurrence of key areas of land‐to‐lake and land‐to‐atmosphere hydrological and biogeochemical linkages that are critical in the movement of matter and energy at local to global scales. However, monitoring surface hydrological dynamics over large geographic extents and over long periods of time is a challenge for hydrologists, as traditional point measurements are not practical. In this study we used European Remote Sensing satellite radar imagery to monitor the variation in surface hydrological patterns over a 12‐year period and to assess the change in the organization of saturated and inundated areas of the landscape. Using the regional Utikuma River drainage basin (2900 km2) as the test area, the analyses of patterns of wetlands indicated that, during dry climatic conditions, wetland sizes were small and disconnected from each other and receiving bodies of water. As climatic conditions changed from dry to mesic, wetland numbers increased but were still disconnected. Very wet climatic conditions were required before the disconnected wetlands coalesced and connected to lakes. During these wet conditions, the response of the lake level at Utikuma Lake was observed to be much higher than under drier conditions. Analyses of individual wetland maps and integrated wetland probability maps have the potential to inform future biogeochemical and ecological investigations and forest management on the Boreal Plain. Copyright © 2007 John Wiley & Sons, Ltd. 相似文献
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Dynamical analysis of mesoscale eddy-induced ocean internal waves using linear theories 总被引：3，自引：1，他引：2
This study aims to explore generation mechanisms of the ocean internal wave using the dynamical analysis methods based on linear theories. Historical cruise measurements and recent synthetic aperture radar （SAR） observations of mesoscale eddies with diameter of several tens of kilometers to hundreds of kilometers show that the internal wave packets with wavelength of hundreds of meters to kilometer exist inside the mesoscale eddies. This coexistence phenomenon and inherent links between the two different scale processes are revealed in the solutions of governing equations and boundary conditions for the internal wave disturbance with a horizontally slowly variable amplitude in a cylindrical coordinate system. The theoretical solutions indicate that the instability of eddy current field provides the dynamical mechanism to internal wave generation. The derived dispersion relation indicates that the internal wave propagation is modified by the eddy current field structure. The energy equation of the internal waves clearly shows the internal wave energy increment comes from the eddy. The theoretical models are used to explain the observation of the mesoscale eddy-induced internal waves off the Norwegian coast. The two-dimensional waveform solution of the anticyclonic eddy-induced internal wave packet appears as ring-shaped curves, which contains the typical features of eddy stream lines. The comparison of theoretical solutions to the structure of the internal wave packets on SAR image shows a good agreement on the major features. 相似文献
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WANGYan-li CHENZhe 《中国地理科学(英文版)》2003,13(1):91-96
Several image fusion approaches for CCD/SAR images are studied and the performance evaluation of these fusion approaches is completed in this paper,Fistly,the preprocessing of CCD/SAR images before fusion is fulfilled,Then,the imager fusion methods including linear superposition,nonlinear operator method and multiresolution methods,of which the multiresolution methods include Laplacian pyramid ,ratio pyramied,contrast pyramid,gradient pyramid,morphological pyramid and discrete wavelet transform,are adopted to fuse two types of images ,Lastly,the four performance measures,standard deviation,entropy,cross entropy and spatial frequency,are calculated to compare the fusion results by different fusion approaches in this paper,Experimenteal results show that contrast pyramid,morphology pyramid and discrete wavelet transformation in multiresolution approaches are more suitalbe for CCD/SAR image fusion than other ones proposed in this paper and the objective preformance evaluations of CCD/SAR image fusion approaches are effective. 相似文献
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京津冀地区1992—2014年三阶段地面沉降InSAR监测 总被引：1，自引：0，他引：1
京津冀地区是我国地面沉降灾害发育最严重的地区,几乎每年都造成巨大的经济损失。本文提出了改进的时间序列InSAR技术——多主影像相干目标小基线干涉技术（MCTSB-InSAR）,利用4颗卫星摄取的3个时段的时间序列SAR影像：ERS-1/2 SAR（1992—2000年）、ENVISAT ASAR（2003—2010年）、RADARSAT-2（2012—2014年）,获取了京津冀地区1992—2014年间3个时段的地面沉降信息。经与京津两地120个以上水准测量数据进行比较,3个时段的地表监测结果的精度分别为8.7、4.7、5.4mm/a。分析了北京和天津两市22年间地面沉降的时空变化特征,其中北京市地面沉降呈不断加重趋势;天津市地面沉降在1992—2010年间发展迅猛,在2010年以后有所减缓。同时,本文也表明MCTSB-InSAR技术是有效可靠的,在大区域地面沉降监测中具有推广应用价值。 相似文献