陀螺灵敏部运动轨迹参数测定

高精度悬挂式陀螺仪在研制、生产和调试中仍存在无法精确测定和调整陀螺惯性灵敏部静平衡残余量的问题,研究发现含有静平衡残余量和静平衡状态良好的陀螺运动轨迹存在明显的差异,因此精确测定陀螺灵敏部运动轨迹参数可为精确测定陀螺灵敏部静平衡残余量提供有效途径。文中研制利用激光、高清相机、显微放大镜头等部件,结合计算机视觉和图像处理等方法,采用质心跟踪的方式精确测定陀螺灵敏部摆动(未启动马达)轨迹的装置;利用最小二乘方法拟合陀螺摆动轨迹,推导求取陀螺摆动周期、振幅、衰减系数、摆动中心、抖动振幅等参数的方法。最后用文中装置测定JT15陀螺悬挂系统在未启动马达下的运动轨迹参数,验证装置与方法的有效性。     

Is ‘Centre of Volume’ a robust indicator of changes in snowmelt timing?

The centre of volume (COV), or the hydrograph centroid, is a measure of streamflow timing that is a widely used indicator of the effects of warmer temperatures on the hydrology of snowmelt streams. The COV was originally developed as a measure of land‐use effects, and its response is affected by several factors other than temperature, particularly total run‐off. A ‘toy’ model is used to demonstrate some of these effects, and these effects are also shown for streamflow data from Canada's Reference Hydrologic Basin Network. These deficiencies indicate that COV is neither specific nor robust as an indicator. Although these effects might be overcome by streamflow decomposition, the use of COV as an indicator of snowmelt timing should be avoided. Copyright © 2013 John Wiley & Sons, Ltd.     

景德镇地区一次早春飑线天气过程分析及数值模拟

利用常规高空、地面、雷达观测资料和FNL1°×1°再分析资料,应用天气学方法和数值模拟方法对2016年4月3日景德镇地区一次早春飑线天气过程进行了分析。结果表明:高空冷涡低槽引导的冷空气与西南暖湿气流强烈对峙是此次飑线过程的环流背景。高低空急流耦合作用加强了大气的垂直上升运动和锋面的次级环流,造成赣北地区上空大气具备较强的动力不稳定。回波强度超过55 dBz的低质心强对流云体是导致景德镇地区出现5 min降水量达14.3 mm强降水的重要原因。飑线的快速移动和近地面超20 m/s的大风速核可预示下游测站有大风出现。飑线前部辐合明显,上升运动剧烈,有利于强回波的发展。冷池的强度变化、持续时间与此次飑线的维持有关。     

质心法在航空影像框标定位中的应用

航片框标定位的精度直接影响摄影测量测图的质量,传统的基于影像匹配的框标定位算法精度只能达到像素级。文中提出一种模板匹配与质心法相结合的航片框标定位方法,先利用模板匹配进行概略定位,再利用质心法进行框标点的精确定位,将精度提高到亚像素级。实验证明该方法可以有效地提高精度。     

2014年新疆于田MS7.3地震矩心矩张量快速测定

We successfully employ an automatic centroid moment tensor(CMT) inversion system to infer the CMT solutions of the February 12,2014 MS7.3 Yutian,Xinjiang earthquake using near-field seismic waveforms(4° < △ < 12°) observed by the virtual China seismic networks,which have been recently set up.The results indicate that this event occurred on a rupture plane(strike 243°,dip 70°,and rake-18°),showing left-lateral strike-slip faulting with a minor normal-faulting component.The centroid in the horizontal direction is located nearly 13 km east of the epicenter(36.123° N,82.499° E),and the best-fitting centroid depth is around 10 km.The total scalar moment,M0,is retrieved with an average value of 3.05 × 1019N·m,corresponding to moment magnitude MW6.92.Most of the energy is released within about 14 s.Moreover,we discuss about the potential application of this system in earthquake disaster decision.     

基于改进的Ly算子的快速星图质心确定方法

Ly算子是摄影测量中应用较多的一种点特征提取算子,它的解算速度快、抗噪能力强,但精度较低;而质心法是星图质心确定中比较具有代表性的方法,但它对噪声敏感,星图较大时,效率不高。根据Ly算子特点,本文在对Ly算子改进的基础上,提出了基于改进的Ly算子的快速星图质心确定方法,实验结果表明,该方法在信噪比较低、星图较大的情况下,较传统质心法解算速度更快、定位精度更高、抗噪能力更强;较带阈值的质心法,解算精度相当,但解算速度更快。     

星点中心高精度质心定位算法

质心法是星点中心计算的常用算法.为提高质心法的精度,对其进行了深入研究.在分析3种质心法形式的基础上提出了质心法的统一模型,并指出模型中的参数阈值T 和灰度加权指数k 对于质心法的最终精度有很大影响.采用模拟星点和实测星点对质心法精度与参数 T 和k 的关系进行了分析,得出了相同的结论.随着 T 和k 的增加,质心法精度先升高后降低,存在极值点;在极值点处,T 为背景灰度,k 为2.0;为保证信息量,T 不能过高,但增加k 可以获得增加T 同样的精度效果;通过调节 T 和k,可以使质心法精度提高25%以上.     

基于智能决策支持系统的电子邮件过滤技术

通过分析实现邮件过滤技术，提出了基于智能决策支持系统的电子邮件过滤模型，并重点讨论了在模型中如何通过内容分析实现对邮件的分类。     

Source Parameters of the 8 October, 2005 M<Subscript>w</Subscript>7.6 Kashmir Earthquake

During the last six years, the National Geophysical Research Institute, Hyderabad has established a semi-permanent seismological network of 5 broadband seismographs and 10 accelerographs in the Kachchh seismic zone, Gujarat, with the prime objective to monitor the continued aftershock activity of the 2001 M_w7.7 Bhuj mainshock. The reliable and accurate broadband data for the M_w 7.6 (8 Oct., 2005) Kashmir earthquake and its aftershocks from this network, as well as from the Hyderabad Geoscope station, enabled us to estimate the group velocity dispersion characteristics and the one-dimensional regional shear-velocity structure of peninsular India. Firstly, we measure Rayleigh- and Love-wave group velocity dispersion curves in the range of 8 to 35 sec and invert these curves to estimate the crustal and upper mantle structure below the western part of peninsular India. Our best model suggests a two-layered crust: The upper crust is 13.8-km thick with a shear velocity (Vs) of 3.2 km/s; the corresponding values for the lower crust are 24.9 km and 3.7 km/sec. The shear velocity for the upper mantle is found to be 4.65 km/sec. Based on this structure, we perform a moment tensor (MT) inversion of the bandpass (0.05–0.02 Hz) filtered seismograms of the Kashmir earthquake. The best fit is obtained for a source located at a depth of 30 km, with a seismic moment, Mo, of 1.6 × 10²⁷ dyne-cm, and a focal mechanism with strike 19.5°, dip 42°, and rake 167°. The long-period magnitude (M_A ~ M_w) of this earthquake is estimated to be 7.31. An analysis of well-developed sPn and sSn regional crustal phases from the bandpassed (0.02–0.25 Hz) seismograms of this earthquake at four stations in Kachchh suggests a focal depth of 30.8 km.