空中声源水下声场的简正波建模方法

空水界面声信号传播特性是水下检测空中声源首先要研究的问题,文中讨论了空中声源在水下产生声场的简正波模型,仿真分析了空中声源的水下声场,比较了简正波方法与射线方法、快速场方法对空中声源在水下产生的声场传播损失。结论表明简正波方法适用于远场传播损失。     

Equatorial F-region vertical ion drifts during quiet solar maximum

Median values of ionosonde h′F data acquired at Ibadan (Geographic:7.4°N, 3.9°E, Magnetic: dip 6°S, and magnetic declination, 3°W), Nigeria, West Africa, have been used to determine vertical ion drift (electric field) characteristics in the postsunset ionosphere in the African region during a time of high solar activity (average F_10.7 −208). The database spans from January and December 1958 during the era of International Geophysical Year (IGY) for geomagnetic quiet conditions. Bimonthly averaged diurnal variations patterns are very similar, but differ significantly in magnitude and in the evening reversal times. Also, monthly variations of F-region vertical ion drift reversal times inferred from the time of h′F maximum indicates early reversal during equinoxes and December solstice months except for the month of April. Late reversal is observed during the June solstice months. The equatorial evening prereversal enhancement in vertical ion drift (V_zp) occurs largely near 1900 LT with typical values 20–45 m/s. Comparison of Ibadan ionosonde V_zp with the values of prereversal peak velocity reported for Jicamarca (South America), Kodaikanal (India), and Scherliess and Fejer global model show considerable disparity. The changes of postsunset peak in virtual height of F-layer (h′F_P) with prereversal velocity peak V_zp are anti-correlated. Investigation of solar effects on monthly values of V_zp and h′F_P revealed that these parameters are independent of monthly averaged solar flux intensity during quiet-time sunspot maximum conditions.     

基于标定场的激光雷达两步标定方法

针对激光雷达大测量范围高精度测角测距问题,提出一种基于标定场的激光雷达两步标定方法.该方法在分析激光雷达测角误差和测距误差的基础上,提出激光雷达误差修正模型.该模型将距离修正从标定模型中分离,首先利用靶标场完成全视场的角度标定,并确定其外部参数,再利用基线场实现距离标定.以降低距离标定参数与角度标定参数之间的耦合性,保证激光雷达角度和距离标定的精度和准确度.实验结果表明方法合理有效,能够实现激光雷达的高精度标定.     

Driving major solar flares and eruptions: A review

This review focuses on the processes that energize and trigger M- and X-class solar flares and associated flux-rope destabilizations. Numerical modeling of specific solar regions is hampered by uncertain coronal-field reconstructions and by poorly understood magnetic reconnection; these limitations result in uncertain estimates of field topology, energy, and helicity. The primary advances in understanding field destabilizations therefore come from the combination of generic numerical experiments with interpretation of sets of observations. These suggest a critical role for the emergence of twisted flux ropes into pre-existing strong field for many, if not all, of the active regions that produce M- or X-class flares. The flux and internal twist of the emerging ropes appear to play as important a role in determining whether an eruption will develop predominantly as flare, confined eruption, or CME, as do the properties of the embedding field. Based on reviewed literature, I outline a scenario for major flares and eruptions that combines flux-rope emergence, mass draining, near-surface reconnection, and the interaction with the surrounding field. Whether deterministic forecasting is in principle possible remains to be seen: to date no reliable such forecasts can be made. Large-sample studies based on long-duration, comprehensive observations of active regions from their emergence through their flaring phase are needed to help us better understand these complex phenomena.     

Possible physical properties of the flow in the vicinity of the heliopause

An interface between the fully ionized hydrogen plasma of the solar wind (SW) and the partially ionized hydrogen gas flow of the local interstellar medium (LISM) is formed as a region where there is a strong interaction between these two flows. The interface is bounded by the solar wind termination shock (TS) and the LISM bow shock (BS) and is separated on two regions by the heliopause (HP) separating the solar wind and charged component of the LISM (plasma component below). The BS is formed due to the deceleration of the supersonic LISM flow relative to the solar system. Regions of the interface between the TS and HP and between the HP and BS were in literature named as the inner and outer heliosheaths, respectively. An investigation of the structure and physical properties of the heliosheath is at present especially interested due to the fact that Voyager-1 and Voyager-2 have crossed the TS in December 2004 (Burlaga, L.F., Ness, N.F., Acuna, M.Y., et al. Crossing the termination shock into the the heliosheath. Magnetic fields. Science 309, 2027–2029, 2005; Fisk, L.A. Journey into the unknown beyond. Science 309, 2016–2017, 2005; Decker, R.B., Krimigis, S.M., Roelof, E.C., et al. Voyager 1 in the foreshock, termination shock and heliosheath. Science 309, 2020–2024, 2005; Stone, E.C., Cummings, A.C., McDonald, F.B., et al. Voyager 1 explores the termination shock region and the heliosheath beyond. Science 309, 2017–2020, 2005) and in September 2007 (Jokipii, J.R. A shock for Voyager 2. Nature 454, 38–39, 2008; Gurnett, D.A., Kurth, W.S. Intense plasma waves at and near the solar wind termination shock. Nature 454, 78–80, 2008. doi: 10.1038/nature07023; Wang, L., Lin, R.P., Larson, D.E., Luhmann, J.G. Domination of heliosheath pressure by shock-accelerated pickup ions from observations of neutral atoms. Nature 454, 81–83, 2008. doi: 10.1038/nature07068.14; Burlaga, L.F., Ness, N.F., Acuna, M.H., et al. Magnetic fields at the solar wind termination shock. Nature 454, 75–77, 2008. doi: 10.1038/nature07029; Richardson, J.D., Kasper, J.C., Wang, C., et al. Cool heliosheath plasma and deceleration of the upstream solar wind at the termination shock. Nature 454, 63–66, 2008. doi: 10.1038/nature07024; Stone, E.C., Cummings, A.C., McDonald, F.B., et al. An asymmetric solar wind termination shock. Nature 454, 71–74, 2008. doi: 10.1038/nature07022; Decker, R.B., Krimigis, S.M., Roelof, E.C., et al. Mediation of the solar wind termination shock by non-thermal ions. Nature 454, 67–70, 2008. doi: 10.1038/nature 07030), respectively, and entered to the inner heliosheath.     

基于FPGA的可变尺寸块运动估计高效结构

针对可变尺寸块运动估计(VBSME,Variable Block-Size Motion Estimation)的硬件结构在现场可编程门阵列(FPGA, Field Programmable Gate Array)上实现时消耗资源多且速度慢的问题,提出了一种面积和速度优化的VBSME硬件结构.其中,绝对差累加和(SAD,Sum of Absolute Differences)的计算采用基于随机存储器(RAM,Random Access Memory)的累加计算方式,比基于寄存器合并的方式节省了面积并增加了速度;通过采用脉动比较链而非总线结构,增强了多个SAD值的比较能力,并能高效地实现对部分差排除算法(PDE,Partial Difference Elimination)的支持.基于Virtex-II型FPGA器件,本结构消耗了2261个slice,时钟频率达到164MHz,在搜索窗口为16×16时可实时处理标清格式的视频.与同类设计相比,设计的面积可减少77%,速度增加218%,FPGA的硬件效率显著提升.     

消除数据调制影响的FFT捕获方法

在利用快速傅里叶变换(FFT, Fast Fourier Transform)捕获扩频信号的过程中,为了提高捕获精度,会遇到基带数据调制影响捕获性能的问题.主要分析了基带数据符号跳变影响FFT捕获性能的原因:在频域内造成待检测信号的幅度衰减以及频点偏移.提出了一种解决此问题的方法:通过对I和Q两路信号的运算,构造一个不受数据调制影响的复信号,对此信号作FFT,完成捕获.给出了此方法的MATLAB仿真,以及基于现场可编程门阵列(FPGA, Field Programmable Gate Array)的实现方案.实验数据表明,此方法消除了基带数据调制对FFT捕获性能的影响,且在相等积分时间的条件下,比常用方法的捕获精度提高了一倍.      

全玻璃真空管型太阳热水器内流场的CFD模拟

全玻璃真空管型太阳热水器是技术相对成熟、应用最广的太阳能利用方式.通过对全玻璃真空管型太阳热水器内流场的计算流体力学模拟,研究了器内的对流换热过程,分析了真空管截面的流体流动速度分布,考察了真空管不同位置处的流体循环速度及箱体内水温对循环速度的影响.结果表明,随着流体温度的升高,器内出现随机的湍动涡流;涡流的存在将造成管内冷热流体的混和,对换热过程不利;在真空管内安置引流挡板将抑制流体的湍动,确保有序的热对流流动,提高对流换热效率.研究结果有助于剖析热水器内对流换热的机理,对技术革新提供参考.      

亚、跨、超声速下空腔流场特性实验研究

在FL-21跨、超声速风洞中对空腔流场特性进行了较为深入的实验研究.空腔的长深比L/D为7、8、9、12、15,试验马赫数M范围为0.6、0.9、1.2、1.5、1.8,试验雷诺数Re为1.23~2.26×107.研究表明:空腔流场特性主要由空腔长深比L/D和来流马赫数所决定,这两个参数的变化均能引起空腔的流场类型发生变化.另外,边界层厚度涠钥涨坏撞康难沽Ψ植家灿凶畔灾挠跋?随着边界层厚度与空腔深度之比?D的减小,空腔的流场类型有向闭式穴流动转变的趋势.