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.     

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．     

橡胶接触轮硬度、槽形和工件硬度对砂带磨削的影响

本文主要研究橡胶接融轮硬度、槽形和工件硬度对金属切除量、砂带磨损、磨削比、磨削力 和工件表面粗糙度的影响，它对砂带磨削时根据不同的工件硬度、不同的技术要求正确选用橡胶接触轮的硬度和槽形提供了依据．     

船舶流体动力系数与频率响应计算

利用拉普拉斯变换技术及优化方法对船舶运动的试验衰减曲线进行分析处理，提 出了计算船舶流体动力系数及频率响应的新方法，与既往的方法比较将更加合理， 并且方法简单易行，误差较小．可同时求出各个频率下的流体动力系数及运动频率响 应。与试验结果及其他理论方法比较，针算结果是令人满意的。     

无规扩散类反应表面生长动力学行为

研究了无规扩散类表面生长的动力学和标度行为，研究了两种粒子（Ａ、Ｃ）在二维衬底上的聚集．当Ｃ粒子的几率ｑ＝０时，系统表现出泊松生长．当ｑ≠０时，表面表现出粗化的形貌特性，存在着粗化转变．对Ｃ粒子扩散步长以及扩散几率对粗化转变的影响也进行了研究     

广义Davey—Stewartson系统中驻波的稳定性

对非线性Ｓｃｈｒｏｄｉｎｇｅｒ方程中驻波的稳定性进行了研究，讨论了在广义Ｄａｖｅｙ－Ｓｔｅｗａｒｔｓｏｎ系统中稳定驻波的存在条件．     

大学物理学教学中初相位的求解——旋转矢量法

在大学物理中有关振动方程和波动方程的教学中发现,很多学生不知怎么求解振动方程和波动方程,其主要原因是大多学生不知如何求解初相位。文章从实际教学过程出发,论述如何用旋转矢量法来求解初相位。通过旋转矢量法来求解初相位,方法简捷,学生学习起来方便、易懂。     

金属表面合金化的研究

Rh(001),(111)和(111)表面被Mo合金化的原子绪构已首次成功地用场离子显微镜直接观察到。表面合金化是采用在超高真空系统中气相沉积及随后淬火,低温扩散来实现。交换机制是可能的扩散机制。观察到的环状结构是Rh-Mo合金中Mo原子优先场蒸发造成的。