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1.
简要描述了用压力测波仪进行的几个深海波浪观测计划。指出在高波级条件下,由于缺乏压力测波仪记录转换的理论和实测依据,提供的波浪资料不需进一步验证。并提出使用Seapac2100方向潮流仪和S4方向潮流仪资料处理软件需注意的几个问题。  相似文献   

2.
采用声学多普勒流速仪(ADV)和多点测波仪的实验资料,对分段式造波机生成的多向随机波浪进行方向谱分析.结果表明,分段式造波机生成的多向随机波浪的时间平稳性优于空间均匀性;贝叶斯方法(BDM)适合于流速实验资料和阵列波浪资料的方向谱分析,给出的方向谱满足随机波浪的内禀性质(如光滑性、连续性等);流速资料和阵列波浪资料给出的方向谱具有相当的精度,但与测速的深度有关;三参量(如三点波浪、两个方向的速度分量和一点波浪等)可给出具有相当精度的方向谱;给出了衡量方向谱精度的初步标准.  相似文献   

3.
使用传统的在海底(或海底以上几米处)固定压力测波仪的方法观测波浪,因水层的滤波作用而无法有效地观测到高频短波。本文提出一种新的观测方法-使用悬挂压力测波仪的方法观测波浪。通过数值方法模拟与实际比较吻合的波面。然后模拟固定压力测波仪和悬挂坟力测波仪两种不同的方法获取此波面的水下压力记录曲线。应用传统谱分析的方法得到各自的压力频谱,再根据不同的情况分别换算成表面谱。通过数值的方法可以证明使用悬挂压力测  相似文献   

4.
近海海洋工程波浪观测中较为广泛使用的测波方法主要包括压力式测波、声学测波和重力式测波等。三种观测方法各有优势,需根据历史资料、地理环境和任务目的设计合理的观测形式,可以选择一种或多种形式组合的形式,以达到最佳的观测效果。使用GPS测波浮标、AWAC声学海流/波浪测量仪和TWR-2050压力式波潮仪的实测资料进行了对比分析,结果显示,测波浮标与AWAC所测数据相关性较一致;TWR压力波潮仪与AWAC测量的波高趋势基本一致,但周期短、波高小的海域和时间段测量准确度较差。  相似文献   

5.
压力式波浪/潮位测量仪对比试验初报   总被引:1,自引:0,他引:1  
介绍了新研制的压力式波浪/潮位测量仪和垂线测波记录仪、S4浪潮流仪在水深8.5m处所作对比试验的结果。结果表明,潮 比测效果明显优于波浪的比测效果。应用压力式波潮仪测浪的比测结果尚可接受,但应该指出,当测量大浪时,误差会减小,其效果将合明显提高。为提高观测的质量,还应在水深较深处(50m)进行比测试验。  相似文献   

6.
用60个波高仪组成2m×2m的方阵,同步测量波面过程,用Doppler声学流速仪获得了二维正向和斜向规则波、二维正向和斜向随机波以及三维随机波浪场中不同水深处的同步Euler水质点速度各方向分量的高精度的时间过程资料.以此为出发点,讨论了分段式造波机生成波浪的周期分布特征,发现三维随机波浪周期分布的μ值与二维随机波浪比较有明显增大的趋势.分别从速度合矢量方向与波向的吻合程度(对二维波浪)、"多点波面"组合与"波面-水质点速度"组合两种方式得到方向谱的吻合程度(对三维随机波浪)等不同角度,论证了分段式造波机产生的波浪的内外部结构的一致性.  相似文献   

7.
全面地比较和总结了当前包括压力式测波、声学式测波、浮标式测波和遥测式测波在内的几种主要的海洋波浪测量方法的技术特点;对相应类型的典型代表型号的仪器主要技术指标进行了对比;对不同类型测量方法及其对应的仪器的具体适用环境给出了分析和建议。实际结合了ADCP,AWAC,Wave Duo测波浮球等几种海洋波浪测量仪器于2014年12月在江苏省南通市近海相近区域的同步实测数据,对这几种仪器的海洋波浪测量的响应和过程特征进行了对比和分析,这对相关的海洋波浪测量技术和对应的测波仪器设备特点也是一个很好的验证。  相似文献   

8.
一、前言连云港是我国重点建设港口之一,为了扩建港口的需要,曾在34°52′48″N、119°42′24″E处投放了“波浪骑士”测波仪。进行波要素的连续观测。我们在整理观测资料过程中,发现波浪记录中有明显的波群现象,即在波列中高度较大的波浪连续几个成群地出现。通常把海面上的不规则波看成是随机过程,并不考虑变量出现的先后次序。也就是  相似文献   

9.
提出了一种实验室波长估计的新方法。在实验室中,使用同步测量的多个测波仪采集波面起伏数据,并根据不同测波仪数据的相关性,计算通过两个测波仪的波浪传播速度,并由此计算波浪波长,计算结果与传统的根据频散关系计算波长对比。分析结果表明:这种新的方法比原有的根据频散关系计算波长更为合理。同时,针对该方法分辨率较低的不足,本文提出了一种新的测波仪数据的插值方法。通过分析实验数据表明:这种新的插值方法有效地提高原有方法的波长计算精度。通过测波仪数据相关性及插值方法配合,该方法可以更合理计算海浪波长。  相似文献   

10.
本文介绍了HDL—2176底压式测波仪的基本特性,给出了水下压力阵列进行波浪方向谱估计的数据计算方法。  相似文献   

11.
This paper analyses the results of an application of a piled wavescreen. Experimental measurements were undertaken in the laboratory conditions for a given structural configuration under the attack of regular and irregular waves. Dynamic pressure distribution along and around the inclined piles was obtained employing pressure transducers. Using these data, in-line dynamic wave forces acting on piles were also determined. Water particle (orbital) velocities were measured at seaward and landward of the wavescreen using two acoustic Doppler velocimeters (ADV) simultaneously. Furthermore, wave data were collected using resistance type wave gauges at the seaward and landward of the structure. Based on those data, wave attenuation performance of the wavescreen was explored for two different depth values. Findings showed that piled wavescreen can provide effective shore protection as an environmentally friendly coastal structure.  相似文献   

12.
This study presents a three-point method for separating incident and reflected waves to explain normally incident waves' propagating over a sloping bed. Linear wave shoaling is used to determine changes in wave amplitude and phase in response to variations of bathymetry. The wave reflection coefficient and incident amplitude are estimated from wave heights measured at three fixed wave gauges with unequal spacing. Sensitivity analysis demonstrates that the proposed method can predict the reflection and amplitude of waves over a sloping bed more accurately than the two-point method.  相似文献   

13.
14.
Except the commonly selected pressure transfer function derived from the linear wave theory, a previous study on the pressure transfer function for recovering surface wave from underwater pressure transducer suggested that the pressure transfer function is a function of frequency parameter only. With careful analysis, this study showed that the pressure transfer function should include a transducer submergence parameter as that given by the linear theory. It was found that the previously suggested empirical formula should be restricted to measurements with the pressure transducer close to the surface; otherwise overestimation of wave height would result. Field measurements were carried out with an acoustic wave gauge and a synchronized pressure transducer located at various depths with submergence parameter close to 1 (near the sea floor). It was shown that the previous one-parameter empirical formula might overestimate the significant wave height by more than 30%. This study found that with deep-water wave bursts excluded, the transfer function based on the linear wave theory provided a fairly good estimation on the significant wave heights, with an average deviation of 3.6%.  相似文献   

15.
波浪作用下粉质土海床的液化是影响海上平台、海底管线等海洋构筑物安全的灾害之一。在进行构筑物设计中应考虑海床液化的深度问题,而液化土体对下部海床的界面波压力是计算海床孔隙水压力增长以及液化深度的重要参量。本文基于波致粉土海床自上而下的渐进液化模式,利用双层流体波动理论,推导了考虑海床土体黏性的海床界面波压力表达式,并与不考虑黏性时的界面波压力进行了比较分析。结果表明,计算液化后土体界面波压力时,是否考虑液化土体的黏性对结果影响较大,进而可能影响粉质土海床液化深度的确定。  相似文献   

16.
Hwa  CHIEN 《中国海洋工程》2002,16(1):89-105
A spatial array of wave gauges installed on an observatoion platform has been designed and arranged to measure the lo-cal features of winter monsoon directional waves off Taishi coast of Taiwan. A new method, named the Bayesian Parameter Estimation Method(BPEM) , is developed and adopted to determine the main direction and the directional spreading parame-ter of directional spectra. The BPEM could be considered as a regression analysis to find the maximum joint probability of parameters, which best approximates the observed data from the Bayesian viewpoint. The result of the analysis of field wave data demonstrates the highly dependency of the characteristics of normalized directional spreading on the wave age. The Mit-suyasu type empirical formula of directional spectrum is therefore modified to be representative of monsoon wave field. More-over, it is suggested that Smax could be expressed as a function of wave steepness. The values of Smax decrease with increas-ing steepness. Finally, a local directi  相似文献   

17.
The Goda's method of separating the frequency spectrum of the unidirectional incident and reflected waves is improved. The proposed method can be applied to the separation of oblique incident and reflected waves and the two wave gauges can be arranged in an arbitrary angle in front of a structure. When the projected distance of the two probes on the incident wave direction is the multiple ofthe half length of the incident waves, the singular problem will emerge by using the method. It is advised that when the projected distance of the two measured points on the incident wave direction is 0.05~0.45 times the wave length of peak frequency wave, good results can be obtained. The simulated resultant waves are separated by the method of numerical simulation and the separated wave spectra are basically corresponding to the target spectra input. The wave trains calculated by the separated incident and reflected wave frequency spectrum are approximated to the input wave trains and the reflected coefficient can be derived correctly. Therefore, the method proposed in this paper is reliable.  相似文献   

18.
Wave-tide-surge coupled model simulation for Typhoon Maemi   总被引:2,自引:2,他引:2  
1 IntroductionThe main reason for coupling the tide and surgehydrodynamic model with a surface wave model canbe found in the physical interactions taking place inthe surface and bottom boundary layers. During thesevere storm conditions such interactions a…  相似文献   

19.
顾倩  张宁川 《海洋学报》2017,39(5):123-137
基于物理模型试验,考虑畸形波参数、相对板宽、相对波高等影响因素,就畸形波对平顶双层水平板防波堤作用进行研究。首先对畸形波作用下双层水平板的波浪力分布特征进行了讨论,然后就最大波动压强、结构最大总垂向力与不规则波作用进行了对比分析。结果表明,畸形波作用下,双层水平板最大波动压力出现在前端迎浪区域附近,向尾端逐渐递减。双层水平板4个受力面的压力分布不同且有相位差,4个受力面的最大波动压力时间差约在0.1Tp~0.4Tp范围内变化。与不规则波作用比较,畸形波作用没有显著改变波压包络分布特征,但增大了波压包络强度值。试验范围内,就最大总力而言,两者最大总浮托力比值在1.06~2.45间变化;向下的最大总垂向力比值在1.22~2.07之间变化;就波动压力而言,其增大的幅度与畸形波参数α1相关性最强,随α1的增大而增大,在α1=2.04~3.1试验范围内,畸形波作用时的最大压强比不规则波作用时可约增大20%~80%。就最大波吸力而言,两者的比值与畸形波参数α4相关性最强,随α4的增大而减小。在α4=0.62~0.75试验范围内,最大波吸力强度的比值在1.61~0.87范围内变化。当α4≤0.72时,畸形波作用时的最大波吸力大于不规则波作用时的最大波吸力;当α4 > 0.72时则刚好相反。  相似文献   

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