混合计算方法在无人机RCS预估中的应用

现代军用无人机外形隐身设计时对整机雷达散射截面（RCS）的快速预估分析是一项重要的研究课题。无人机作为一种电大尺寸的目标模型体,采用电磁场的高频计算方法,对于机体面目标散射场贡献采用物理光学算法（PO）,对于由面元结合部所形成的棱边绕射场贡献采用改进的等效电磁流（IMEC）算法分析,散射总场由两部分共同叠加计算生成。利用PO＋IMEC算法完成了对一种无人机目标模型RCS的模拟计算,将模拟结果与暗室实测结果对比获得了较为满意的结果。     

Drifter trajectory tracking experiment and analysis with multi-frequency HFSWR in the East China Sea

We conducted the drifter trajectory tracking experiment for two drifters in the East China Sea,in which the currents were detected by two multi-frequency HFSWRs using the Lagrange-tracking method.The tracking drifter trajectory shows good agreement with the GPS records by qualitative and quantitative analysis that indicates that drifter tracking by HFSWR is valid.In the 12-hour tracking for drifters P1 and P2,the average errors are 1.84 km,1.73 km,and the maximum errors are 3.52 km and 3.12 km,respectively.The current measurement is evaluated by an acoustic Doppler current profilers(ADCP) in-situ observation,and it is the first multi-frequency HFSWR ocean surface monitoring experiment in China.In addition,the main aspects(HFSWR current measurement error,wind,and wave) influencing the tracking accuracy are discussed,and especially the wind factor’s impact is analyzed through the wind filed data.     

B~-→ρ~-ρ~0衰变中的b→u右手流研究

利用推广因子化方法,研究b→u右手流对B-→ρ-ρ0衰变的影响.发现最新实验数据支持右手流混合强度取负值,横向极化比f⊥/f‖对右手流很敏感,可以作为以后实验检验该系统右手流的物理参量.     

三维正压非线性潮汐潮流伴随同化模型开边界反演研究

在数学物理反问题的框架下,基于渤海、黄海M2分潮波的数值模拟,本文设计孪生实验研究了三维正压非线性潮汐潮流模型中开边界条件的伴随法反演问题,以验证所建立的伴随模型的有效性和正确性。本文同时讨论了开边界条件的空间分布、初值、观测误差以及观测数量对开边界反演的影响,对此参数估计反问题的适定性进行了初步研究.     

场向电流与地磁和亚暴活动的相关性

检验了场向电流与地磁和亚暴活动的相关性。按极光电集流指数AL的大小,地磁活动被分为4个水平,即|AL|<=50,50<|AL|<=150,150<|AL|<=300和|AL|>300分别相应于非常平静、平静、扰动和强烈扰动。统计结果表明,场向电流的发生率、强度和密度都随地磁活动的增加而增大。在最低活动水平,发生率只有8.9%,而73.2%的事件发生在扰动水平以上。对于夜间的场向电流,65.5%的事件伴随着磁层亚暴。     

Application of adjoint assimilation technique in simulating tides and tidal currents of the Bohai Sea, the Yellow Sea and the East China Sea

Considering the interaction of different tidal waves, an adjoint numerical model is developed to simulate M2, S2, K1 and O1 tidal waves in the Bohai Sea, the Yellow Sea and the East China Sea （B-Y-E） simultaneously. Compared with previous researches, by using the adjoint assimilation technique to inverse open boundary conditions and bottom friction coefficients based on altimetric data from TOPEX/Poseidon （T/P） and tidal gauges data, the precision of the numerical simulation is significantly improved. Selecting 14 days of simulated results after the initial wanning run to conduct harmonic analysis, the results can show the characteristics of M2, S2, K1 and O1 tidal wave systems perfectly in B-Y-E. Compared with 9 current stations, the calculated harmonic constants of tidal currents for M2 and K1 are in good agreement with the observed ones.     

Simulation study on optimal currents and winds for the spaceborne SAR mapping of sea bottom topography

A simulation model for the radar backscattering cross section of the sea surface has been developed based on the synthetic aperture radar (SAR) imaging mechanism of the sea bottom topography. The relationship between tidal currents, sea surface winds and the SAR mapping of the sea bottom topography has been analyzed using the results of the simulation. It is shown that the sea bottom topography can be observed by spaceborne SAR more easily at high current speeds. The optimal direction of the currents for mapping the sea bottom topography is the direction perpendicular to the bathymetric features while the direction parallel to the bathymetric features is the worst. The optimal range of wind speeds for mapping the sea bottom topography is between 3 and 9 m/s. The wind directions between 30° and 89° are preferred although the effect of the wind direction on SAR mapping of bottom topography is complicated.     

防城港口门外抛泥区潮流及质点轨迹模拟

模拟研究了防城港倾倒区潮流流场及质点的拉格朗日漂移，结果表明潮流动力场及倾倒点所选位置有利于保证航道的疏浚效果。     

电子镇流器谐波含量及功率因数研究

通过电路分析对电子镇流器存在的电源电流谐波高和功率因数低等问题。提出几种能够降低谐波含量和提高功率因数的方法，并给出理论分析。     

Circulation in the western tropical Pacific Ocean and its seasonal variation

An assimilation data set based on the GFDL MOM3 model and the NODC XBT data set is used to examine the circulation in the western tropical Pacific and its seasonal variations. The assimilated and observed velocities and transports of the mean circulation agree well. Transports of the North Equatorial Current (NEC), Mindanao Current (MC), North Equatorial Countercurrent (NECC) west of 140°E and Kuroshio origin estimated with the assimilation data display the seasonal cycles, roughly strong in boreal spring and weak in autumn, with a little phase difference.The NECC transport also has a semi-annual fluctuation resuiting from the phase lag between seasonal cycles of two tropical gyres' recirculations. Strong in summer during the southeast monsoon period, the seasonal cycle of the Indonesian throughfiow (ITF) is somewhat different from those of its upstreams, the MC and New Guinea Coastal Current (NGCC), implying the monsoon's impact on it.