辽西—内蒙地区地壳结构的转换波测深研究

为研究华北地台、西拉木伦加里东褶皱带及贺根山海西褶皱带交界地区的深部构造,在辽西-内蒙地区进行了转换波地震测深。本文给出了转换波测深的基本结果,同时试图通过对转换波方法本身的进一步研究,给出更多的关于地壳结构和间断面性质的信息,并据此进行测深结果的构造意义的讨论。     

浅水风波波高,波周期分布

通过浅水风波试验，探讨了浅水波高、波周期的分布形式，重点分析了水深因素对波高、波周期分布的影响，给出了浅水波高、波周期分布的表达式，并确定了浅水特征波高间的关系。     

几种疑难心电波形的自动识别方法探讨

本文提出几种疑难心电波形的识别方法,该方法的特点在于将医生读图的经验引入识别过程,设定可能性识别判据,从而显著提高了自动诊断系统对于预激综合症、完全性左、右束支传导阻滞和心肌梗塞等病种的诊断准确性。     

Coupling and propagating of mesoscale sea level variability between the western Pacific and the South China Sea

The coupling and propagating features of mesoscale sea level variability between the western Pacific (WP) and the South China Sea (SCS) were studied based on time series analyses of satellite altimeter measured, along-track sea surface height anomalies (SSHA) along 21°N and the slope of the northern SCS. The analyses show that mesoscale sea level fluctuations in the WP have rather limited coherent effects on the SCS, and no statistically significant propagation of mesoscale variability through the Luzon Strait was observed except in the 45-day band. Evidence suggests that the 45-day fluctuation is very much likely a character of the Kuroshio originating from its low-latitude beginning. It is also sug- gested that the westward propagating Rossby waves will deform when they encounter the dynamical barrier of the Kuroshio. The Kuroshio will then acts on the SCS in its own way. The SCS is a relatively isolated system in the sense of coupling and propagating of oceanic mesoscale waves.     

福建东山湾海浪现场观测的统计特征

为分析福建省南部港湾──东山湾的波浪特征,采用S4型压力式方向波浪仪观测获取现场一个月的风浪过程资料,对其进行了统计分析和频谱分析,给出了波高和周期分布,特征波要素与频谱关系,结果表明:实测波高分布与瑞利分布基本相符;波浪谱的显著部分在狭窄的频率内,对应3、5、6、7级风谱峰密度值(m2s)分别为0.084 3、0.372 8、0.941 8、1.837 7,随着风速的增加,谱能也显著地增加,谱曲线下面的总面积增大,谱的显著部分波及的频率范围也扩大,且谱的显著部分沿低频率的方向推移,对应风浪的波高及周期范围增大.     

扩展的双曲正切函数法的一个新应用

给出扩展的双曲正切函数法中Riccati方程的12个新精确解，将这些解与双曲正切函数法结合应用，得到KdV—Burger-Kuramoto方程的多个新类型的精确行波解．     

Nonlinear interactions between gravity waves and background winds

Using the nonlinear propagating gravity waves (GW) model in the two-dimensional compressible atmosphere and the linear GW theory, the process of GW propagation in different background winds, e.g. the direction of the background wind is opposite to (dead wind) or the same as (tail wind) the direction of the horizontal phase velocity of GW, is studied. The results show that the dead wind prolongs the vertical wavelength and accelerates GW propagation. Therefore, GW propagates up to a higher height becomes instable in a short time and eventually induces an inverse jet flow. Then, the vertical wavelength is becoming short due to the nonlinear interactions between GW and the inverse jet flow. The vertical wavelength and group velocity decrease after GW propagates into the tail wind. The initial instable time is delayed. Although most of GW is trapped in the instable region, some of GW propagates above the instable region. Compared with GW propagation in the tail wind, the nonlinear interactions between GW and the dead wind are also strong. In contrast, the linear GW theory predicts that GW can propagate freely in the dead wind. The vertical wavelength simulated by the nonlinear numerical model is different from that predicted by the linear theory greatly after GW propagates into the dead wind.     

高斯束谐振系统对遗迹高频引力波方向的选择效应

高斯束谐振系统为早期宇宙遗留的随机高频引力波的探测开启了一个非常重要的窗口．本文指出,当入射引力波的传播方向与高斯束不同时,高斯束谐振系统产生的一阶扰动光子流将降低几个数量级,即高斯束谐振系统只对沿某一特定方向传播的高频引力波产生响应．因此,高斯束谐振系统对高频引力波的传播方向具有良好的选择效应．     

双目标旅行商问题及其蚂蚁算法实验研究

对双目标旅行商问题设计了基于Pareto概念的多目标蚂蚁算法.借助于算法的全局搜索能力,在整个解空间内快速搜索多目标组合的Pareto有效解,并利用多目标蚂蚁算法维持解集多样性的特点,使搜索到的Pareto解在前沿均匀分布.经大量算例求解验证了其有效性,该算法具有较好的通用性.     

基于遗传算法的约束性多TSP问题及其应用

针对一类具有约束条件的汽车调度问题 ,提出了约束性的多重 TSP(CMTSP)问题及其模型 ,给出了一种遗传算法解法。对比实验结果表明 :遗传算法具有比启发式算法更好的结果。