三维非结构网格的生成及优化

叙述了一种新的生成三维非结构网格的Delaunay方法,该方法能够高效地生成优质四面体网格。由于采用了局部剖分的方法来保证边界的完整性,因而不需要添加新的节点到原始表面三角形中。该方法在四面体外接球的球心处插入新的节点,在插入全部内点后,采用删除边、边/面交换、网格光顺等方法对生成的网格进行了优化,基本能删除质量差的四面体。     

卫星星座整网轨道确定分析与仿真

编队飞行的卫星或卫星星座对轨道确定自主性和精度提出了较高要求。针对这个问题,通过建立星座的轨道动力学模型和星间观测的测量模型,将星座中的星间观测数据和地面观测数据融合起来,将待估的卫星轨道参数和部分动力学参数进行适当的分类,研究卫星星座整网轨道确定的新方法,并在理论上分析了整网定轨方法能提高定轨精度的原因;最后采用自主开发的卫星星座整网轨道确定软件进行了仿真计算。计算表明,该方法能有效地减少对地面站的依赖,并较大幅度提高定轨时卫星绝对位置和相对位置精度。
     

密封舱内漂浮小球运动规律的数值模拟研究

"天宫二号"空间实验室开展了首次人机协同在轨维修技术试验,机械臂操作终端抓取漂浮小球试验为在轨试验任务之一。为研究漂浮小球与机械臂操作终端运动特性之间的匹配性,文章建立了在轨微重力环境下小球运动的物理模型与数学模型,采用动网格方法对不同小球的运动特性进行数值模拟,得到小球的运动规律,由此确定小球的设计参数范围,作为机械臂操作终端系统方案设计的依据。最终,数值模拟结果与"天宫二号"空间实验室在轨试验数据的对比初步验证了该计算结果的正确性。     

Atmospheric response to a Hot SST Event in November 2006 as observed by the AIRS instrument

Using Atmospheric Infrared Sounder (AIRS) products of atmospheric temperature and geopotential height, we investigate the atmospheric response to HE0611, which was found and investigated by [Qin, H., Kawamura, H., Sakaida, F., Ando, K. A case study of the tropical Hot Event in November 2006 (HE0611) using a geostationary meteorological satellite and the TAO/TRITON mooring array. J. Geophys. Res. 113, C08045, doi: 10.1029/2007JC004640, 2008]. HE0611 was formed by connecting two very high SST areas, HE0611-East and HE0611-West. The period-mean atmosphere temperatures at levels of 925 and 850 hPa in HE0611-West are higher, by about 0.5 K, than those in WE0611-East while the atmospheric temperatures at middle to high levels (700–300 hPa) are higher in HE0611-East. The period-mean geopotential heights HE0611-East are much lower than those in HE0611-West for the levels from the surface to 400 hPa. The mean geopotential heights from 400 hPa to 200 hPa are higher in HE0611-East. In the middle and high layers over HE0611-West, the atmosphere temperatures gradually decrease from 7th to 17th, and then increase significantly. The increase in HE0611-East starts from 15th November, which is earlier than that of HE0611-West. The geopotential heights in the high layer of both the areas also show corresponding behaviors. The lagged atmospheric response in the western part is confirmed by the correlation analysis. It emerges that the atmospheric response to HE0611 is well organized and associated with deep convention in HE0611-East and subsidence in HE0611-West. These are also consistent with the HE0611 features and evolution revealed by earlier HE studies.     

厚覆冰导线升力突变机理及数值模拟研究

针对新月形厚覆冰导线的升力系数在风攻角15°附近存在突变的问题,分别采用基于k-ωSST湍流模型的雷诺时均法和大涡模拟(LES)的数值方法对新月形厚覆冰导线在风攻角10°～20°范围进行了模拟.通过对比两种数值方法计算得到的覆冰导线气动力系数、流场结构和表面风压,发现LES方法能够更好地捕捉新月形覆冰导线表面的小尺度涡...     

湍流模型源项的数值处理方法对计算结果的影响研究

涡粘性湍流模型广泛应用于各种工程湍流问题的计算。对于大多数湍流模型,在湍流控制方程的右端会出现源项,其刚性给数值计算带来很大的影响。从源项的物理意义出发分析了源项导致求解困难的原因,并在通用的求解湍流模型方程的点隐法基础上,以源项弱刚性的S-A湍流模型和源项强刚性的k-ωSST湍流模型为例,论述了生成项和耗散项之间的平衡关系对数值模拟的重要意义,给出了针对不同源项的具体处理方法。对RAE2882翼型跨声速流动算例的模拟结果表明,这些处理方法有效的提高了控制方程组的计算稳定性。     

一种嵌入以太网控制装置的实现

以太网控制器随着互联网发展，将被广泛应用于日常生活和工作中．本文介绍以太网控制器RTL8019AS的结构；结合常用的单片机SST89E554RC，分析具体的硬件和软件的实现．     

Fronts and thermohaline structure of the Brazil–Malvinas Confluence System

Fronts and thermohaline structure of the Brazil–Malvinas Confluence System (BMCS) are studied from climatic data, “Marathon Exp. Leg.8, 1984” data, and Sea surface temperature (SST) data base “ds277-Reynolds” (1981–2000). The South Atlantic Central Water (SACW) is divided in two main types: tropical (TW) and subtropical water (ST). Water masses, Fronts, Inter-Frontal and Frontal Zones are analysed and classified: (a) the water masses: Tropical Low-Salinity Water, Tropical Surface Water, Tropical Tropospheric Water, Subtropical Low-Salinity Water, Subtropical Surface Water, Subtropical Tropospheric Water. T,S characteristics of intermediate, deep and bottom water defined by different authors are confirmed and completed; (b) the Inter-Frontal Zones: Tropical/Brazil Current Zone, Subtropical Zone and Subantarctic Zone; (c) the Frontal Zones: Subtropical, Subantarctic and Polar, and (d) the Fronts: Subtropical Front of the Brazil Current, Principal Subtropical Front, North Subtropical Front, Subtropical Surface Front, South Subtropical Front, Subantarctic Surface Front, Subantarctic Front and Polar Front. Several stable T–S relationships are found below the friction layer and at the Fronts. The maximum gradient of the oceanographic characteristics occurs at the Brazil Current Front, which can be any of the subtropical Fronts, depending on season. Minimum mean depth of the pycnocline coincides with the Fronts of the BMCS, indicating the paths of low-salinity shelf waters into the open ocean. In the work it is shown how to recover the horizontal and vertical thermohaline structure of waters from satellite data RSMAS SST.     

基于改进SST模型的分离流动数值模拟

对SST湍流模型进行了改进,并通过对典型分离流动进行数值模拟,来检验和提高模型预测分离流动的能力.基于亚声速分离流动,提出了提高雷诺应力的模拟精度和分离流修正的改进方法,并进行了对比研究得出结论;在亚声速分离流动分析结论基础上,采用了可压缩性修正方法,开展了跨声速、超声速和高超声速激波/边界层干扰分离流动的数值模拟研究.结果表明:提高雷诺应力的模拟精度和采用分离流修正明显地提高了SST湍流模型对分离流动的模拟能力;适当地可压缩性修正对超声速和高超声速分离流动的计算精度有改善作用.     

壁面函数在激波诱导分离流动中的应用

以数值模拟激波-附面层干扰引起的流动分离问题为研究背景,发展了基于有限体积方法的雷诺平均Navier—Stokes（RANS）方程的流场数值模拟方法。利用壁面函数模型得到壁面剪切应力,通过修正壁面粘性通量,构造了一种新的湍流边界处理方法,并将其耦合到RANS方程和SSTk-ω湍流模型的数值求解中;同时,针对激波诱导引起的附面层流动分离问题,提出一种附面层网格加密技术,能够自适应加密分离区内附面层网格,使得在流动分离区域也能够使用壁面函数模型。数值算例表明,壁面函数模型能够降低数值模拟结果对网格的依赖性;同时也验证了壁面函数耦合附面层网格自适应方法,在处理激波诱导引起的附面层流动分离问题时的有效性和准确性。