Optimum viscous damper for connecting adjacent SDOF structures for harmonic and stationary white‐noise random excitations     

A. V. Bhaskararao  R. S. Jangid 《地震工程与结构动力学》2007,36(4):563-571

The dynamic behaviour of two adjacent single‐degree‐of‐freedom (SDOF) structures connected with a viscous damper is studied under base acceleration. The base acceleration is modelled as harmonic excitation as well as stationary white‐noise random process. The governing equations of motion of the connected system are derived and solved for relative displacement and absolute acceleration responses of connected structures. The response of structures is found to be reduced by connecting with a viscous damper having appropriate damping. For undamped SDOF structures, the closed‐form expressions for optimum damping of viscous damper for minimum steady state as well as minimum mean square relative displacement and absolute acceleration of either of the connected SDOF structures are derived. The optimum damper damping is found to be functions of mass and frequency ratio of two connected structures. Further, numerical results had indicated that the damping of the connected structures does not have noticeable effects on the optimum damper damping and the corresponding optimized response. This implies that the derived closed‐form expressions for optimum damper damping of undamped structures can also be used in practical applications for damped structures. Copyright © 2006 John Wiley & Sons, Ltd.  相似文献   

再论夏季西太平洋副热带高压的西伸北跳   总被引：68，自引：4，他引：68       下载免费PDF全文

陶诗言  卫捷 《应用气象学报》2006,17(5):513-525

利用NCEP/NCAR再分析资料, 选择了1998年、2003年和2005年夏季我国东部雨带位置变化过程进行诊断分析。研究表明:夏季我国东部暴雨带位置的变动, 受西太平洋副热带高压西伸北跳 (南撤东退) 的调节。当副热带高压西伸北跳 (南撤东退) 时, 暴雨带向北 (向南) 移动。在副热带高压西伸北跳持续时期, 长江流域中下游地区出现高温酷暑天气。副热带高压西伸北跳是由于欧亚大陆上空存在静止Rossby波列, 波的能量沿着高空副热带急流向东传播到我国沿海海岸 (115°~130°E) 时, 在该地区激发出一个长波脊。这个长波脊的建立, 使得副热带高压和对流层上部的青藏高压都朝长波脊方向伸展, 表现为“相向”而行。而当在沿海海岸上空激发出一个长波槽时, 副热带高压南撤东退而青藏高压退回到高原上空。当夏季沿海海岸上空的长波脊持续维持时, 长江中下游会出现持久的高温酷暑天气。根据夏季天气预报的经验, 欧洲中期数值预报中心发布的预报对副热带高压的西伸北跳有较好的可预报性。  相似文献   

Representation of microscale ocean wavenumber spectrum correct to the second order   总被引：1，自引：0，他引：1  

YUAN Yeli & HUA Feng    . Institute of Oceanology  Chinese Academy of Sciences  Qingdao  China  . Key Laboratory of Marine Science  Numerical Modeling  State Oceanic Administration  Qingdao  China  . Graduate School of the Chinese Academy of Sciences  Beijing  China 《中国科学D辑(英文版)》2005,48(4):549-554

Up to now the finest synthetic aperture radar(SAR) sea surface image is still the state-of-art oceanimage provided by the satellite microwave remotesensing due to its high spatial resolution and dynamicremote sensing mechanism. Early in 1978, Valenzueladerived the analytical representation of SAR image(backscaterring cross section distribution) on the tem-porally stationary and locally homogeneous assump-tion[1] σ0 (θ)IJ = 4πkm cos4θ gIJ (θ) E0(k,0), (1) (1) …  相似文献   

Standard cumulative semivariograms of stationary stochastic processes and regional correlation     

Zekâi Sen 《Mathematical Geology》1992,24(4):417-435

The standard cumulative semivariograms (SCS), obtained analytically from the currently employed stationary stochastic processes, provide a basis for the model identification and its parameter as well as regional correlation estimations. The analytical solutions for different stationary stochastic processes such as independent (IP), moving average (MA), autoregressive (AR), and autoregressive integrated moving average ARIMA (1,0,1) processes give rise to different types of SCSs which can be expressed in terms of the autocorrelation structure parameters only. The SCSs of independent and MA processes appear as linear trends whereas other type of processes have SCSs which are nonlinear for short distances but become linear at large distances. Irrespective of the stationary stochastic process type the linear portions of SCSs have unit slopes. The vertical distance between these linear portions and that of the IP cumulative semivariogram (CS), provide an indicator for measuring the regional correlation. In the case of stationary processes, the straight line portions of any CS are parallel to each other. Hence, it is possible to identify the model from the sample CS. Finally, necessary procedures are provided for the model parameters estimation. The methodology developed, herein, is applied to some hydrochemical ions in the groundwater of the Wasia aquifer in central part of Kingdom of Saudi Arabia.  相似文献   

Simulations of non‐stationary frequency content and its importance to seismic assessment of structures     

Junjie Wang  Lichu Fan  Shie Qian  Jing Zhou 《地震工程与结构动力学》2002,31(4):993-1005

To verify the importance of the non‐stationary frequency characteristic of seismic ground motion, a joint time–frequency analysis technique of time signals, called chirplet‐based signal approximation, is developed to extract the non‐stationary frequency information from the recorded data. The chirplet‐based signal approximation is clear in concept, similar to Fourier Transform in mathematical expressions but with different base functions. Case studies show that the chirplet‐based signal approximation can represent the joint time–frequency variation of seismic ground motion quite well. Both the random models of uniform modulating process and evolutionary process are employed to generate artificial seismic waves. The joint time–frequency modulating function in the random model of evolutionary process is determined by chirplet‐based signal approximation. Finally, non‐linear response analysis of a SODF system and a frame structure is performed based on the generated artificial seismic waves. The results show that the non‐stationary frequency characteristic of seismic ground motion can significantly change the non‐linear response characteristics of structures, particularly when a structure goes into collapse phase under seismic action. It is concluded that non‐stationary frequency characteristic of seismic ground motion should be considered for the assessment of seismic capacity of structures. Copyright © 2002 John Wiley & Sons, Ltd.  相似文献   

Probabilistic approach for modal identification using non‐stationary noisy response measurements only     

Ka‐Veng Yuen  James L. Beck  Lambros S. Katafygiotis 《地震工程与结构动力学》2002,31(4):1007-1023

This paper addresses the problem of identification of the modal parameters for a structural system using measured non‐stationary response time histories only. A Bayesian time‐domain approach is presented which is based on an approximation of the probability distribution of the response to a non‐stationary stochastic excitation. It allows one to obtain not only the most probable values of the updated modal parameters and stochastic excitation parameters but also their associated uncertainties using only one set of response data. It is found that the updated probability distribution can be well approximated by a Gaussian distribution centred at the most probable values of the parameters. Examples using simulated data are presented to illustrate the proposed method. Copyright © 2002 John Wiley & Sons, Ltd.  相似文献   

诊断天气气候时间序列极值特征的一种新方法   总被引：11，自引：2，他引：11       下载免费PDF全文

丁裕国  金莲姬  刘晶淼 《大气科学》2002,26(3):343-351

将平稳过程的交叉理论用于天气气候极值分析,提出了一种诊断天气气候时间序列极值特征量的新方法,在正态假设下,推证出天气气候记录中,极值出现频数、持续时间和等待时间的估计公式,论证了极值出现频数与其频谱结构的对应关系及其相互推算方法.实例应用表明,其理论计算值与实测值相当一致,这种方法对于气候变化诊断与预测和天气预报具有很强的实用价值.  相似文献   

Using the Entropy of Curves to Segment a Time or Spatial Series   总被引：1，自引：0，他引：1  

A. Denis  F. Crémoux 《Mathematical Geology》2002,34(8):899-914

The concept of the thermodynamics of curves is used to analyze change in the variability of time or spatial series. More specifically, the entropy of a curve makes it possible to divide a nonstationary random field, because of a change in variance, into subdomains where data are said to be stationary. It is demonstrated that for time and spatial series the entropy of a curve is the slope of the cumulative sum of absolute differences. Numerical simulations show the efficiency of this tool. It can be shown that the presence of a linear or quadratic trend is without effect on the localization of the stationary subdomains. A practical case is studied with data collected from a tunnel boring machine where several parameters are recorded. This analysis can bring more information on the mechanical behavior of the different geological formations and explain or justify unplanned delays.  相似文献   

辐散风和瞬变的涡度通量对定常波的强迫          下载免费PDF全文

耿全震  黄荣辉 《大气科学》1997,21(1):73-82

本文从理论分析、资料诊断和正压模式数值试验三个方面研究了瞬变的涡度通量的辐合与辐散风产生的涡度源之间的关系及它们在对流层上层定常波维持中的作用。结果表明， 瞬变涡度通量的辐合对辐散风产生的涡度源有抵消或耗散的趋势；定常波是在两种强迫力的共同作用下维持的。同时还研究了不同地区散度场对定常波的作用， 结果表明，中纬度东亚地区的辐合场对维持东亚大槽是重要的，并且这一辐合场与位于印度尼西亚地区的辐散场是维持西太平洋上副热带反气旋系统的主要强迫源。  相似文献   

THE FORCING OF ANOMALOUS DIVERGENT WIND AND TRANSIENT VORTICITY FLUXES TO THE ANOMALY OF STATIONARY WAVES          下载免费PDF全文

Geng Quanzhen  Huang Ronghui 《Acta Meteorologica Sinica》1997,11(1):1-11

The forcing of anomalous divergent wind and transient vorticity fluxes to the anomaly ofstationary waves of DJF (December—January—February) 1982/1983 is studied.The results showthat the anomaly of the transient vorticity flux convergence tends to cancel or dissipate the anomalyof the vorticity sources generated by divergent wind.The stationary wave anomalies are maintainedby both of these forcings.It is also found that,for the DJF 1982/1983 case,both of the vorticitysource anomaly over the tropical and equatorial eastern Pacific and that over the midlatitude NorthPacific are important to maintain the atmospheric circulation anomaly over the Pacific/NorthAmerica region.  相似文献