Diel patterns in pelagic fish behaviour and distribution observed from a stationary, bottom-mounted, and upward-facing transducer   总被引：1，自引：1，他引：1  

Axenrot  Thomas; Didrikas  Tomas; Danielsson  Charlotte; Hansson  Sture 《ICES Journal of Marine Science》2004,61(7):1100-1104

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Application of Random Process in Soil Profile Modeling     

Yan Shuwang  Jia Xiaoli  Deng Weidong Professor  Dept. of Hydraulic Eng.  Tianjin University  Tianjin Graduate student  Dept. of Hydraulic Eng.  Tianjin University  Tianjin Senior Engineer  Chongqing Institute of Highway Science 《中国海洋工程》1994,(4)

When using the random process in soil profile modeling, the stationary and ergodicity of thesoil properties in the profile must be tested. This paper describes a procedure for stationary and ergodicity testing. Numerical examples were given for demonstration. A log-cosine function is suggested to simulate the correlation function, which has been proved to be good for soil profile modeling.  相似文献   

Stochastic analysis of the linear equivalent response of bridge piers with aseismic devices     

Luisa Carlotta Pagnini  Giovanni Solari 《地震工程与结构动力学》1999,28(5):543-560

The dynamic response of bridge piers with aseismic devices to earthquake excitation is evaluated by the stochastic equivalent linearization technique. The seismic acceleration is schematized through a Gaussian stationary random process. The pier is considered linear elastic, the span is idealized as a rigid mass, the restoring force of the device is represented through a non-linear differential model. The study of the complex modes of the linearized system gives an interpretation of the mechanical behaviour, leads to a formally elementary solution and highlights some phenomena which are typical of the hysteretic systems, particularly of those marked by weak hardening. Even though the solution is limited to the stationary field, it brings out several noteworthy considerations about the effective non stationary behaviour of the structure. Copyright © 1999 John Wiley & Sons, Ltd.  相似文献   

基于用户和卫星概略位置的信号传播时延估计   总被引：2，自引：0，他引：2  

王梦丽  许晓勇  王飞雪 《全球定位系统》2005,30(4):1-5

辅助长码直捕的一个最重要的先验信息是时间信息,卫星信号传播时延估计是减少时域搜索范围的一个重要方面。针对地面静止用户,给出了基于用户和卫星概略位置的卫星信号传播时延估计算法,并指出用户和卫星位置误差对传播时延的影响可以分离计算。数值计量考印,即使用户和卫星的位置误差均达到1000km,也能将传播时延不确定范围压缩一半。  相似文献   

平稳函数线性内插的教学探讨     

陈本富  邹自力  郭先春  赵宝贵  ZHAO Bao-gui 《测绘科学》2011,36(3):250-251

平稳函数线性内插是最小二乘配置的一种特例.本文结合测绘专业教学中采用较多的经典教材<测量平差原理>,对教材中的内插公式做了通用表达形式的推导,在保持原书编排风格的同时,不仅增强了原公式表达的逻辑性,而且,新的补充公式的推导,使教材中通过算例显示并强调的信号估值及其方差的特性,从理论上得到了较为严谨的证明.  相似文献   

滇黔静止锋大暴雨的锋面特征及其对MCS的影响     

唐延婧  胡跃文  谢清霞 《气象科技》2014,42(1):151-157

2012年5月21—22日,贵州省出现了一次典型的Ⅲ型静止锋在南支槽的引导下锋生而触发MCS形成暴雨的过程。MCS有非线性、降水强的特征。分析发现:低层静止锋锋区强,锋生明显;锋前有高能舌及低涡切变发展,切变南侧有偏南急流。垂直方向上锋区陡峭,锋前上凸区内上升气流强,对流不稳定;南支槽及高低空系统的前倾配置是上升气流强的原因。这些锋面特征为MCS发生发展提供了有利条件:低层高能舌和低涡切变为MCS提供了热力和动力条件;偏南急流是影响MCS的重要因素。锋前上凸区是MCS发展的重要区域,锋区附近的θse场及高低空系统前倾配置利于MCS发生发展。锋前到锋区附近的水汽条件好,急流出口处的水汽辐合及上升气流为MCS和大暴雨提供了有利水汽输送。  相似文献   

Instability of wave propagation in saturated poroelastoplastic media     

Xikui Li  Junbo Zhang  Hongwu Zhang 《国际地质力学数值与分析法杂志》2002,26(6):563-578

In the present work, stationary discontinuities and fluttery instabilities of wave propagation in saturated poro‐elastoplastic media are analysed in the frame of Biot theory. The generalized Biot formulations are particularly employed for simulating non‐linear coupled hydro‐mechanical behaviour of the media. Inertial coupling effect between the solid and the fluid phases of the media is also taken into account. The non‐associated Drucker–Prager criterion to describe non‐linear constitutive behaviour of pressure dependent elasto‐plasticity for the solid skeleton of the media is particularly considered. With omission of compressibility of solid grains and the pore fluid, the critical conditions of stationary discontinuities and flutter instabilities occurring in wave propagation are given in explicit forms. It is shown that when the stationary discontinuity is triggered at the surface of discontinuity there still may exist real wave speeds. The wave speeds across the stationary discontinuity surface entirely cease to be real only in non‐associated plasticity, certain ranges of value of Poisson's ratio and when compression stress normal to the surface of discontinuity dominates the stress state at the surface. It is also indicated that the fluttery instabilities, under which some wave speeds cease to be real even in strain hardening stage, may occur prior to stationary discontinuities only for non‐associated plasticity under certain conditions. These conditions are: (1) both the porosity and the Poisson's ratio possess relatively low values and (2) the deviatoric part of the effective stress normal to the surface of discontinuity is compressive. A region in the porosity–Poisson's ratio plot, in which fluttery instabilities are possible to occur, is given. Copyright © 2002 John Wiley & Sons, Ltd.  相似文献   

水文站水准基面关系分析   总被引：3，自引：3，他引：0  

刘琦  王峰  周珂  周宜富 《水文》2012,32(3):20-28

本文定义了基面关系式的概念,提出了基面与基本水准点考证的原则,分析了十六类基面关系式的计算方法,通过研究得出结论:基本水准点变动,冻结高程变动,基本水准点不变,冻结高程不变;绝对基面变化国冻差变化,绝对基面不变国冻差不变;冻结高程及国冻差有一项变动标准高程变动,冻结高程及国冻差都不变动标准高程不变。  相似文献   

超随机特性对地震动谱特性和时间历程的影响   总被引：1，自引：1，他引：0  

徐国栋周锡元  闫维明董娣 《地震工程与工程振动》2005,25(5):6-16

本文从单个地震动样本的角度分析了超随机部分对地震动波形的影响,认为自相关函数噪声部分或功率谱的随机波动部分对地震动波形的影响不大,对地震动的波形起主要控制作用的是地震动的相位谱或相位差谱,而自相关函数的噪声部分（或功率谱的随机波动成分）只对地震动波形起一定程度的调整作用。文中基于平稳随机过程的理论,用蒙特卡罗方法分析了自相关函数噪声项对人工合成地震动振幅和反应谱的影响：由于自相关函数的随机噪声项对地震动总功率或平方和的贡献为零,因此随机噪声项对合成地震动幅值的影响不大,但是由于自相关函数随机噪声项明显改变了地震动功率谱的形状和分布特征,使其出现了明显的波动,也在一定程度上提高了平均反应谱的峰值,从而对平均反应谱也产生一些影响。考虑地震动自相关函数中的随机噪声部分有助于更真实地模拟和反映地震动的真实特性。  相似文献   

A Comparison of Polar Vortex Response to Pacific and Indian Ocean Warming   总被引：1，自引：0，他引：1  

Shuanglin Li 《大气科学进展》2010,27(3):469-482

During recent decades,the tropical Indo-Pacific Ocean has become increasingly warmer.Meanwhile,both the northern and southern hemispheric polar vortices(NPV and SPV)have exhibited a deepening trend in boreal winter.Although previous studies have revealed that the tropical Indian Ocean warming(IOW)favors an intensifying NPV and a weakening SPV,how the tropical Pacific Ocean warming(POW) influences the NPV and SPV remains unclear.In this study,a comparative analysis has been conducted through ensemble atmospheric general circulation model(AGCM)experiments.The results show that,for the Northern Hemisphere,the two warmings exerted opposite impacts in boreal winter,in that the IOW intensified the NPV while the POW weakened the NPV.For the Southern Hemisphere,both the IOW and POW warmed the southern polar atmosphere and weakened the SPV.A diagnostic analysis based on the vorticity budget revealed that such an interhemispheric difference in influences from the IOW and POW in boreal winter was associated with different roles of transient eddy momentum flux convergence between the hemispheres.Furthermore,this difference may have been linked to different strengths of stationary wave activity between the hemispheres in boreal winter.  相似文献