仿生硬件及其进展

文章详细介绍了仿生硬件的概念、主要特征及用途 ,阐述了仿生硬件的进化原理及实现思想 ,重点分析了仿生硬件的关键技术———可进化硬件电路、硬件进化方法 ,并总结了研究状况与最新进展 ,讨论了需要解决的核心难点问题及其解决思路 ,最后指出了仿生硬件的研究方向及发展前景。     

终端区最优飞行轨迹特征的研究

为了给飞机提供一条能满足多种指标要求的最优飞行轨迹,针对变分最优理论难以求解多指标优化问题,提出了命名为多次优化的方法,即将多要求的优化任务分成先后相继的多次任务,每次任务中选取一种不能边界转化的要求作为最优性能指标,而其余要求转化为边界条件.利用这一方法以时间、转弯次数、转弯角度为最优性能指标给出了终端区最优飞行轨迹的一般特征.     

大气臭氧地基遥感反演的退卷积方法

本文提出了一种大气臭氧地基遥感信息处理的新方法,它利用非线性退卷积方法和等效仪器函数提高光谱分辨率,利用非线性最小二乘法进行大气臭氧反演计算,可以显着提高大气臭氧遥感的可探测高度和精度。     

冗余空间机械臂粗捕获段无碰撞轨迹规划算法

现有的基于C空间的无碰撞轨迹规划算法需要求解C空间以获得C空间障碍边界。对于多自由度的冗余机械臂,求解过程需要消耗很大的计算量和内存,不适用于计算资源紧张的空间机械臂轨迹的快速规划。文章提出了一种不需要求解C空间的试探性规划算法,包含4个子算法：碰撞检测算法、无碰撞目标构型求解算法、无碰撞路径搜索算法和路径平滑算法。已知期望的末端作用器位置和姿态,利用目标构型求解算法得到无碰撞的目标构型,然后由路径搜索算法在C空间障碍边界未知的情况下,利用碰撞检测算法,采用一定的试探规律,在C空间中搜索出一条无碰撞路径,最终由路径平滑算法使该路径平滑,易于实现。仿真算例表明,该算法是快速有效的,适用于冗余空间机械臂粗捕获段的快速轨迹规划。     

基于增量模型的BTT导弹新型解耦补偿控制

详细分析了倾斜转弯(BTT, Bank-To-Turn)导弹传统动态逆控制的特点及其存在的问题,在此基础上提出了一种基于增量模型的BTT导弹解耦补偿控制方法.该方法通过建立一种描述从当前动态转移至期望动态的BTT导弹增量模型,消除了难以测量或不确定较大的模型部分;在此基础上结合动态逆控制思想设计了BTT导弹的增量式解耦跟踪控制律,与传统动态逆相比,该控制律对模型的依赖程度大幅降低;为进一步提高控制系统对干扰的适应性,提出了一种简单的干扰估计/补偿策略;最后通过数学仿真验证了该方法的有效性.     

Noise analysis of continuous GPS coordinate time series for CMONOC

The Crustal Movement Observation Network of China (CMONOC) is one of the major scientific infrastructures, mainly using Global Positioning System (GPS) measurements, to monitor crustal deformation in the Chinese mainland. In this paper, decade-long coordinate time series of 26 continuous GPS sites of CMONOC are analyzed for their noise content using maximum likelihood estimation (MLE). We study the noise properties of continuous GPS time series of CMONOC for the unfiltered, filtered solutions and also the common mode signals in terms of power law plus white noise model. In the spatial filtering, we remove for every time series a common mode error that was estimated from a modified stacking of position residuals from other sites within ∼1000 km of the selected site. We find that the common mode signal in our network has a combination of spatially correlated flicker noise and a common white noise with large spatial extent. We demonstrate that for the unfiltered solutions of CMONOC continuous GPS sites the main colored noise is a flicker process, with a mean spectral index of ∼1. For the filtered solutions, the main colored noise is a general power law process, indicating that a major number of the filtered regional solutions have a combination of noise sources or local effects. The velocity uncertainties from CMONOC continuous GPS coordinate time series may be underestimated by factors of 8–16 if a pure white noise model is assumed. In addition, using a white plus flicker noise model, the median values of velocity errors for the unfiltered solutions are 0.16 (north), 0.17 (east) and 0.58 (vertical) mm/yr, and the median values for the filtered solutions are 0.09 (north), 0.10 (east) and 0.40 (vertical) mm/yr.     

Ionospheric F2-Layer critical frequency retrieved from COSMIC radio occultation: A statistical comparison with measurements from a meridional ionosonde chain over Southeast Asia

In this paper, we compared the F2-Layer critical frequency (foF2) derived from FORMOSAT-3/COSMIC radio occultation (RO) and ionosondes at Chiang Mai, Chumphon and Kototabang during the years 2008–2015 to evaluate the performance of COSMIC RO over Southeast Asia region. The results show that the time development of foF2 values derived from COSMIC RO generally agrees well with those from ionosonde measurements. However, the differences between the foF2 derived from COSMIC RO and that derived from ionosonde observations display latitudinal dependence. COSMIC RO tends to underestimate foF2 at Chiang Mai and Kototabang, which is near to the north EIA crest and the south one, respectively, while a little overestimate foF2 at Chumphon, which is close to the geomagnetic equator. COSMIC RO agrees best with ionosonde at Chumphon and worst at Chiang Mai. At each ionosonde station, the quality of COSMIC RO data degrades with the increase of solar activity. In addition, at the station Chiang Mai and Kototabang, COSMIC RO performs better in summer than in equinox and winter. Furthermore, the differences in foF2 derived from COSMIC RO and that from ionosonde measurements vary with local time, i.e., the differences in foF2 are generally smaller at night and larger in noontime when equatorial ionization anomaly (EIA) is well developed.     

Alfvén gravity waves in viscous solar plasma: Effect of the background flow

We study the Propagation and damping properties of Alfvén gravity waves in the presence of the vertical magnetic field in the viscous solar plasma under influence of the background flow by deriving a fourth order dispersion relation in terms of the Doppler shifted frequency. We derive the dispersion relation under WKB and Boussinesq approximation. We study the damping of Alfvén gravity waves for the wave frequencies less than and greater than the Brunt-Väisälä frequency. We find that the Brunt-Väisälä frequency divides the frequency ranges where the weakly or strongly damped oscillations occur. The background flow exhibits a strong effect on weakly damped oscillations and a weak effect on the strongly damped oscillations. We also notice that the damping of both the strong and weakly damped oscillations depend on the Brunt-Väisälä frequency and wave number. The effect of the background flow is also being governed by the Brunt-Väisälä frequency and wave number. We also study the properties of gravity wave mode after filtering the Alfvén wave mode by minimizing the magnetic field and noticed that the background flow shows a very strong effect on the gravity wave mode.     

Early analysis of precise orbit and clock offset determination for the satellites of the global BeiDou-3 system

Eight new-generation BeiDou satellites (BeiDou-3) have been launched into Medium Earth Orbit (MEO), allowing for global coverage since March 2018, and they are equipped with new hydrogen atomic clocks and updated rubidium clocks. Firstly, we analyzed the signals for the carrier-to-noise-density ratio (C/N0) and pseudorange multipath (MP) by using international GNSS (Global Navigation Satellite System) Monitoring and Assessment System (iGMAS) station data, and found that B1C has a lower C/N0, and B2a has the same level of C/N0 as the B1I and B3I signals. For pseudorange multipath, compared with the BeiDou-2 satellites, the obvious systematic variation of MP scatters related to the elevation angle is greatly improved for the BeiDou-3 and BeiDou-3e satellites signals. For the signals of the BeiDou-3 satellites, the order of the Root Mean Square (RMS) values of multipath and noise is B3I?<?B1I?<?B2a?<?B1C. Then, the comparison of the precise orbit determination and clock offset determination for the BeiDou-2, BeiDou-3, and BeiDou-3 experimental (BeiDou-3e) satellites was done by using 10 stations from iGMAS. The 3D precision of the 24?h orbit overlap is 24.55, 25.61, and 23.35?cm for the BeiDou-3, BeiDou-3e, and BeiDou-2 satellites, respectively. BeiDou-3 satellite has a comparable precision to that of the BeiDou-2 satellite. For the precision of clock offset estimation, the Standard Deviation (STD) of the BeiDou-3 MEO satellite is 0.350?ns, which is an improvement of 0.042?ns over that of the BeiDou-2 MEO satellite. The stabilities of the BeiDou-3 and BeiDou-3e onboard clocks are better than those of BeiDou-2 by factors of 2.84 and 1.61 at an averaging time of 1000 and 10,000?s, respectively.     

空间色噪声下信号频域检测方法性能分析

水下小孔径阵列的应用环境是色噪声环境,针对超增益波束形成方法在色噪声环境下噪声协方差矩阵估计偏差使阵列空间增益不能达到最大的问题,提出了一种频域超增益波束形成方法(FSD, Super-Directive beamforming in Frequency domain),该方法将宽带接收数据分成多个子带,在每个子带内分别估计噪声协方差矩阵,降低了噪声协方差矩阵的估计偏差,并使用估计得到的噪声协方差矩阵对接收数据解相关.最后使用空间谱检测器检测微弱目标信号.实测噪声数据的仿真结果表明,空间有色噪声环境中FSD方法的检测性能优于传统的时域超增益波束形成方法(TSD, Super-Directive beamforming in Time domain)2 dB,优于频域最小方差无畸变响应(FMVDR, Minimum Variance Distortionless Response in Frequency domain)波束形成方法2 dB.