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。     

小波变换法求电磁波动方程的高频解

提出了一种利用小波变换求解不连续性变系数电磁波动方程高频解的新方法,解决了 Ｆｏｕｒｉｅｒ 变换法无法解决的分层非均匀无耗媒质中波的传播与反射问题。并用该方法计算了一个 Ｆｏｕｒｉｅｒ 变换法能求解的特例,两种方法计算结果完全一致     

彗—木相撞辐射引力波的估算

选用一合理的模型，估算了１９９４年７月发生的彗（ＳＬ９）—木相撞辐射引力波的强度和功率．所得结果表明引力辐射强度远低于目前引力波检测装置所达到的灵敏度．计算过程与所得结果富有启发性     

引力场是产生熵之源还是吸收熵之沟

首先对Penrose以及Bekenstein等人有关物质熵和熵的演化的基本论述作了扼要介绍,揭示出他们理论的核心论点是:确认Clausius熵增加原理是适用于宇宙物质一切演化过程的普适原理,把物质熵的增加方向规定为唯一(可观测)的时间箭头方向.进一步剖析了Penrose等人关于熵的演化理论中存在的基本矛盾,最后通过对正、负能谱系统中熵的演化理论的建立,有力地批驳了Penrose等关于熵和熵的演化理论中的错误论点,并对物质熵的具体演化过程进行了理论自恰的论述.     

分立元器件的模型建立

当电阻、电容、电感、二极管和三极管等元器件在高频应用时,并不表现为一般的理想特性,也通常会因为它们的这种高频特性而影响实验的预期结果.为了进一步分析实验中具体电路的实际情况,首先要建立分立元器件的高频等效模型.本文选用了现在工程上公认的优秀软件Matlab来辅助分析.     

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.     

金融市场中高频数据的分析方法

对高频数据所得到的市场波动率特征和常用的模型及估计方法进行系统的总结,归纳出模型的共同特征、不足之处和修正方法,指出了应用高频数据所面临的问题,提出了在中国股票市场中高频数据的应用方法．     

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.