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《海洋技术学报》2021,(4)
海浪是我国海洋环境业务化观测要素之一,也是海洋预报的重要参数之一,波浪观测仪器对海浪长期、稳定、准确的观测直接影响了科学研究和海洋海岸工程设计的科学性和合理性。为此,波浪观测仪器需进行室内实验室测试和室外海上测试,但目前进入业务化系统的波浪观测仪器一般只进行了实验室计量检定,缺乏现场测试评价。现阶段,用于波浪观测的主要仪器为重力式波浪浮标,为进一步检验重力式测波浮标的稳定性、可靠性,验证波浪数据的有效性、准确性,本文设计了实验室和海上比测试验,分析对比了国内外几种主流测波浮标的观测结果,总体来看,山东省科学院海洋仪器仪表研究所的SBF3-2型波浪浮标和国家海洋技术中心的SBF6-1型波浪浮标观测效果最好,准确性较高,稳定性较强。 相似文献
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ＬＰＢ１－１型海洋平台测波系统是一种适用于海洋平台,港口码头,海岛等环境条件测量波浪的仪器。对该系统的工作原理、组成,主要技术性能,特点以及实现方法作了概要描述,并对系统采用的信号处理技术进行简要分析。 相似文献
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GPS测波技术分析与初步实验研究 总被引：1，自引：0，他引：1
测波浮标是一种方便可行的波浪测量方法,首先分析了单点GPS接收机测波浮标的测量原理,然后做了单点GPS接收机测速实验和单点GPS接收机模拟测波实验,并对这两个实验的数据进行了分析处理,最后提出了单点GPS接收机测波浮标的初步设计方案,为进一步推动这项测波技术的国产化打下了基础。 相似文献
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最近,我院首次从美国恩迪柯公司进口了一套1156遥控测波仪。货已到,待验收消化后即可正式投入使用。1156测波仪是原956测波仪的改进型,它以遥测浮标内的加速度计为传感器,是目前世界上最先进的测波系统之一。该系统使用甚为方便,不仅适用于测量近岸沿海波浪,也适用于远海测波,是当前交通、海洋、石油勘探和航海事业中一种较为理想的测波仪器。它的引进增加了我院现场测波研究工作的手段。 1156测波仪除了能如同956那样测取波浪的波高、波周期和波向外,如若配置一些部件,尚能进行风、气压、水温和气温等要素的测量。 相似文献
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To plan for proper mitigation measures, one should have an advanced knowledge of the phenomenon of tsunami propagation from the deep ocean to coastal waters. There are a few methods to predict tsunamis in the ocean waters; one method is the effective use of data buoy measurements. Although data buoys have been used along the Indian waters there has been a tremendous growth in the number of buoy deployment recently. Under the National Data Buoy Programme (NDBP) of India, the 2.2 m diameter discus data buoys were deployed along the east and west coasts of India for measuring meteorological and ocean parameters. It would be advantageous if these buoys could be efficiently used to measure rare events such as tsunamis. Understanding the dynamic behavior of the buoy is of prime importance if a tsunami warning system is to be successful. This may be accomplished through experimental or numerical studies. A comprehensive experimental study has been conducted to understand the dynamic behavior of a wave rider buoy exposed to a variety of waves. It is common that tsunami waves are represented in terms of shallow water waves, namely solitary and cnoidal waves. Hence, in the present study, the discus type data buoy is scale modeled and tested under the action of solitary and cnoidal waves in the laboratory. The time histories of wave elevations, as well as heave and pitch motions of the buoy model, were analyzed through a spectral approach as well as through wavelet transformations. The wavelet approach gives more detailed insight into the spectral characteristics of the buoy motion in the time scale. The harmonic analyses were performed for the cnoidal wave elevations and subsequent motion characteristics that give an insight into the energy variations. The details of the model, instrumentation, testing conditions and the results are presented in this paper. 相似文献
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波浪观测在海洋环境预报、海洋工程建设、海洋资源调查、航海安全等领域具有重要作用。基于全球导航卫星系统（Global Navigation Satellite System,GNSS）浮标进行波浪观测的方法具有全天候、实时、准确度高、价格低等诸多优点，同时还可以在浮标上集成其他海洋环境测量仪器，因此越来越受到世界各国研究者的重视。本文提出一种基于GNSS浮标的波浪参数反演方法，并成功应用于浙江温州海域，在海试过程中，同公认的波浪骑士浮标对比，平均波高相关系数达到0.95，标准差为4.06 cm，平均波周期相关系数为0.92，标准差为0.24 s，完全符合国家标准。本文所用浮标系统还可以搭载多种海洋环境要素观测传感器，可将数据实时传输至接收终端，具有较高的应用价值。 相似文献
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海洋观测浮标系统应用广泛,浮标体的平衡性能是影响海洋观测浮标使用的重要因素之一(着重观测波浪等水文参数除外)。以一种主体直径为2.3 m的浮标体为例,运用动力学平衡理论,通过数学分析法进行推演计算,分析后得到了此浮标体的重心和浮心的位置。其中,重心位于主浮体的中轴线偏下位置;按照浮标体倾斜一定角度的情况下,推算出浮标体浮心位置,并由此得出其稳心的位置。依据计算,得出浮标体倾斜20°的情况下,此浮标体依然处于稳态平衡,理论结果表明此浮标体设计具有一定的可行性。通过海上实际测试,验证了理论计算分析的正确性。文中对浮标体平衡性的研究采用了理论分析与实验印证相结合的方法,其分析计算方法具有普适性,适用于其他型号的海洋观测浮标体,乃至所有水面浮体的平衡性分析,可为水面浮体设计提供借鉴。 相似文献
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GPS浮标数据反演海浪谱的理论仿真与试验验证 总被引：1，自引：1，他引：0
GPS浮标作为一种新型的海洋测量设备,近年来在海面高度现场测量和星载高度计定标方面取得了重要应用。通过仿真试验对反演海浪谱的方法和流程进行研究,旨在探索从GPS浮标测量的海面高度序列中提取海浪谱的方法。首先,使用Longuest模型生成了海浪波面位移时间序列,并通过Pierson-Moscowitz风浪谱对波面位移的统计特性进行约束,其随机性由相位引入。结合典型潮汐和GPS浮标仪器噪声的仿真时间序列,合成了仿真时间长度1h的1Hz(每秒1次)随机海面高度序列。然后,利用自相关函数法,进行高通滤波和数据压缩,得到了仿真的海浪谱。该仿真结果和理论海浪谱非常接近,可满足海浪谱反演的需求。最后,通过山东石岛外海的GPS浮标现场试验,验证了本文提出的反演方法的适用性。本文的研究解决了GPS浮标反演海浪谱的关键问题,丰富了海浪谱反演的手段,拓展了GPS浮标的应用领域,有望为未来我国的星载波谱仪定标服务。 相似文献
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冰区四季通用灯浮标是一种为满足北方冬季冰冻港口一年四季的助航服务需求研制的新型灯浮标,二阶波浪力对其漂浮姿态和漂移运动有较大影响。文中研究了浮标受到的二阶波浪力的数值计算方法,计算了不同流速下罐形和锥形灯浮标的二阶波浪力。研究结果显示,罐形和锥形灯浮标受到的一阶波浪力相差不大,罐形的二阶波浪力明显小于锥形,具有一定的外形优势。 相似文献
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海浪对ASCAT散射计反演风场的影响研究 总被引：1，自引：1，他引：0
To improve retrieval accuracy, this paper studies wave effects on retrieved wind field from a scatterometer. First, the advanced scatterometer(ASCAT) data and buoy data of the National Data Buoy Center(NDBC) are collocated. Buoy wind speed is converted into neutral wind at 10 m height. Then, ASCAT data are compared with the buoy data for the wind speed and direction. Subsequently, the errors between the ASCAT and the buoy wind as a function of each wave parameter are used to analyze the wave effects. Wave parameters include dominant wave period(dpd), significant wave height(swh), average wave period(apd) and the angle between the dominant wave direction(dwd) and the wind direction. Collocated data are divided into sub-datasets according to the different intervals of each wave parameter. A root mean square error(RMSE) for the wind speed and a mean absolute error(MAE) for the wind direction are calculated from the sub-datasets, which are considered as the function of wave parameters. Finally, optimal wave conditions on wind retrieved from the ASCAT are determined based on the error analyses. The results show the ocean wave parameters have correlative relationships with the RMSE of the retrieved wind speed and the MAE of the retrieved wind direction. The optimal wave conditions are presented in terms of dpd, swh, apd and angle. 相似文献
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This study makes use of the concept of wave age in estimating ocean wave period from space borne altimeter measurements of backscattering coefficient and significant wave height. Introduction of wave age allowed better accounting of the difference between swells and wind waves. Using two years (1998 and 1999) data of TOPEX/Poseidon altimeter and ocean data buoy observations in the Indian Ocean, coefficients were generated for wave period, which were subsequently tested against data for the years 2000 and 2001. The results showed the wave period accuracy to be of the order of 0.6 sec (against 1.3 sec obtained with the semiempirical approach, reported earlier). 相似文献
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This study makes use of the concept of wave age in estimating ocean wave period from space borne altimeter measurements of backscattering coefficient and significant wave height. Introduction of wave age allowed better accounting of the difference between swells and wind waves. Using two years (1998 and 1999) data of TOPEX/Poseidon altimeter and ocean data buoy observations in the Indian Ocean, coefficients were generated for wave period, which were subsequently tested against data for the years 2000 and 2001. The results showed the wave period accuracy to be of the order of 0.6 sec (against 1.3 sec obtained with the semiempirical approach, reported earlier). 相似文献