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1.
三维随机海浪的数值模拟   总被引:1,自引:0,他引:1  
本文首先分析了三维随机海浪的方向谱函数和三维随机海浪的数学模型,然后在MATLAB环境下设计了数值模拟程序,并模拟出三维随机海浪的方向谱和三维随机海浪的三维空间模型。  相似文献   

2.
董玉杰 《海洋通报》1997,16(2):57-62
网格分辨率对WAM海浪模式预报结果的准确伺有重要影响。本文提出了一种移动套网格方法,并在西北太平洋海域的区域化模型中加以实现。利用模型飓风场物模拟风场检验了该方法,结果表明,该方法在计算量增加不多的前提下,可以有铲地校正由于网格过粗导致的WAM模式预报结果偏代的缺陷,对业务预报具有重要实用意义。  相似文献   

3.
针对实体嵌入对海面的随机干扰问题,提出一种海浪三维可视化方法。该方法采用扰动的思想改进了海浪的数学模型,并利用信息更加全面的方向谱描述海浪,进而将方向谱和改进海浪模型共同应用于海浪的三维可视化,形象展示实体嵌入时对海浪的随机性影响,并给出了三维实体的建模方法。通过多组实体嵌入的海浪可视化仿真试验的比较与分析,验证了本文提出方法的有效性。  相似文献   

4.
近岸台风浪的嵌套数值模式   总被引:2,自引:0,他引:2  
程展  戴明瑞 《海洋预报》1994,11(4):6-12
本文将混合数值海浪模式与第三代海浪模式结合起来研究近岸台风浪。在西北太平洋及中国海域采用混合数值海浪模式预报海浪,而在近岸台风区域采用包括海底绕射项的WAM模式,该小区域的浪边界条件由大区域上得到的计算结果提供。我们建立的数值近岸台风浪预报系统既利用了混合海模式节省计算机时的优点,又用细网格的WAM模式抓住了近岸海底地形对海浪的作用,该模式的后报结果表明,模式计算的近岸台风浪台站的实测资料符 合料  相似文献   

5.
赵希人  刘胜 《海洋学报》1989,11(2):226-232
固定点波的海浪模型对研究船舶操纵与控制是十分必要的.皮尔逊(Pierson)在1952年最先利用谱来描述海浪并提出固定点波面的一种运动模型,即海浪模型[1,2].  相似文献   

6.
分析几种低频线谱参数估计方法的优点与不足,结合舰艇噪声低频线谱所具有的特点,应用数字滤波一相关谱估计(DF—C)和自回归移动平均(ARMA)模型相结合的方法(DF—ARMA)对低频线谱作估计,所得线谱的强度和频率估计值准确度较高。  相似文献   

7.
利用航天飞机成像雷达图像分析南海内波   总被引:1,自引:1,他引:1  
利用航天央南海海面获取的内波的合成孔径雷达(SAR)图像数据,计算并对比分析了不同波段海面的后向散射系数的差异。系统给出了SAR图谱到海浪二维谱的计算过程,改进了一些处理方法以适用于内波分布海面,并利用众SAR图像获得的海浪谱,简要分析了内波与风成海浪的相互作用,探讨该区内波的激励因素,认为潮流是激励温跃层在该海区产生有规模内波的主要因素。  相似文献   

8.
本文首先介绍了INMARSAT-C的概况,着重介绍与具体应用有关的技术特性;然后,分析它在海洋环境监测系统中应用时,从技术上必须考虑的若干问题,给出了初步的试验结果;最后,对INMARSAT-C在我国海洋环境监测系统的推广应用提出了建议。  相似文献   

9.
极值风速和极值波高是海洋工程、海洋能开发、防灾减灾等极为关注要素。文章基于来自欧洲中期天气预报中心(ECMWF)的ERA-interim 海浪再分析资料、ERA 阵风资料,计算了“21世纪海上丝绸之路”涉及海域的年极值风速、极值波高,并首次计算了不同季节的极值。结果表明:①南海的50年一遇年极值风速大于孟加拉湾,孟加拉湾大于阿拉伯海;极值波高的分布特征与极值风速大体一致。②南海的极值风速在各个季节都大于孟加拉湾,孟加拉湾大于阿拉伯海;南海- 北印度洋的极值风速在JJA 和SON 期间明显大于MAM 期间,DJF期间最小。③南海各个季节的极值波高都大于北印度洋,阿拉伯海的极值波高在MAM和JJA 期间明显大于孟加拉湾;南海的极值波高在JJA 和SON 期间明显大于MAM 和DJF期间;北印度洋的极值波高在JJA 期间最大,MAM 次之,DJF最小。  相似文献   

10.
本文首先介绍INMARSAT─C的概况,着重介绍与具体应用有关的技术特性;然后,分析它在海洋环境监测系统中应用时,从技术上必须考虑的若干问题,给出了初步的试验结果;最后,对INMARSAT─C在我国海洋环境监测系统中的推广应用提出了建议。  相似文献   

11.
The correlation between individual waves in a real sea state has a central role in existing theories of wave grouping. The attractive Kimura (1980) theory has two critical assumptions, that the sequence of individual wave heights follows a Markov process and that the joint distribution of consecutive wave heights follows a bivariate Rayleigh form. Analysis of measured water surface records suggests that sequences of individual waves can reasonably be described as a first order mixed autoregressive, moving-average or ARMA process, though a distinction among ARMA (1,0), ARMA (0,1) and ARMA (1,1) models was beyond the resolution of the data. These include the Markov or ARMA (1,0) model. The decisive detail, the joint distribution of consecutive wave heights in the sea state, was evaluated by a simulation methodology that is consistent with the Gaussian random wave model. The estimates are dependent on spectral shape and are consistently narrower and more sharply focussed at the peak than the corresponding bivariate Rayleigh estimate. The resulting predictions of run and group length statistics differ from the Kimura theory, though not by a sufficient margin to displace the Kimura theory as a pragmatic choice for wave grouping.  相似文献   

12.
13.
14.
In this paper, without recourse to the nonlinear dynamical equations of the waves, the nonlinear random waves are retrieved from the non-Gaussian characteristic of the sea surface elevation distribution. The question of coincidence of the nonlinear wave profile, spectrum and its distributions of maximum (or minimum) values of the sea surface elevation with results derived from some existing nonlinear theories is expounded under the narrow-band spectrum condition. Taking the shoaling sea wave as an example, the nonlinear random wave process and its spectrum in shallow water are retrieved from both the non-Gaussian characteristics of the sea surface elevation distribution in shallow water and the normal sea waves in deep water and compared with the values actually measured. Results show that they can coincide with the actually measured values quite well, thus, this can confirm that the method proposed in this paper is feasible.  相似文献   

15.
Analytical models for predicting wave reflection from a perforated-wall caisson breakwater have been developed. Most of the existing models deal with the case in which the waves are normally incident to the caisson lying on a flat sea bottom. In the present paper, using the Galerkin-eigenfunction method, an analytical model is developed that can predict the reflection coefficient of a perforatedwall caisson mounted on a rubble mound foundation when waves are obliquely incident to the breakwater at an arbitrary angle. The developed model is compared with other theoretical results and hydraulic experimental data.  相似文献   

16.
The role of surface waves in the ocean mixed layer   总被引:7,自引:6,他引:1  
Previously, most ocean circulation models have overlooked the role of the surface waves. As a result, these models have produced insufficient vertical mixing, with an under - prediction of the ,nixing layer (ML) depth and an over - prediction of the sea surface temperature (SST), particularly during the summer season. As the ocean surface layer determines the lower boundary conditions of the atmosphere, this deficiency has severely limited the performance of the coupled ocean - atmospheric models and hence the climate studies. To overcome this shortcoming, a new parameterization for the wave effects in the ML model that will correct this systematic error of insufficient mixing. The new scheme has enabled the mixing layer to deepen, the surface excessive heating to be corrected, and an excellent agreement with observed global climatologic data. The study indicates that the surface waves are essential for ML formation, and that they are the primer drivers of the upper ocean dynamics; therefore, they are critical for climate studies.  相似文献   

17.
The objective of this study is to determine numerical estimations of seismic amplifications of waves traveling from offshore to shore considering the effect of sea floor configurations. According to the Boundary Element Method, boundary elements were used to irradiate waves and density force can be determined for each element. From this hypothesis, Huygens’ Principle is implemented since diffracted waves are constructed at the boundary from which they are radiated and this is equivalent to Somigliana's theorem. Application of boundary conditions leads to determine a system of integral equations of Fredholm type of second kind, which is solved by the Gaussian method. Various numerical models were analyzed, a first one was used to validate the proposed formulation and some other models were used to show various ideal sea floor configurations to estimate seismic amplifications. Once the formulation was validated, basic slope configurations were studied for estimating spectra of seismic amplifications for various sea floor materials. In general terms, compressional waves (P-waves) can produce seismic amplifications of the incident wave in the order of 2–5. On the other hand, distortional waves (S-waves) can produce amplifications up to 5.5 times the incident wave. A relevant finding is that the highest seismic amplifications due to an offshore earthquake are always located near the shore-line and not offshore despite the seafloor configuration.  相似文献   

18.
Extrapolating from the propagation theories of electromagnetic waves in a layered medium, a three-layer medium model is deduced in this paper by using microwave radiometric remote sensing technology which is suitable to first-year sea ice condition of the northern part of China seas. Comparison with in situ data indicates that for microwave wavelength of 10 cm, the coherent model gives a quite good fit result for the thickness of sea ice less than 20 cm, and the incoherent model also works well for thickness within 20 to 40 cm. Based on three theoretical models, the inversion soft ware from microwave remote sensing data for calculating the thickness of sea ice can be set up. The relative complex dielectrical constants of different types of sea ice in the Liaodong Gulf calculated by using these theoretical models and measurement data are given in this paper. The extent of their values is (0. 5-4. 0)-j(0. 07~0. 19).  相似文献   

19.
关皓  周林  王汉杰  景丽 《海洋学报》2008,30(4):30-38
利用LINUX操作系统下的进程通讯(IPC)技术将中尺度大气模式MM5(V3)与第三代海浪模式WW3进行双向耦合,建立考虑大气-海浪相互作用的风浪耦合模式,在耦合模式中引入3种海表粗糙度参数化方案,通过对一次热带气旋过程的模拟,研究大气-海浪相互作用对热带气旋系统的影响及耦合模式对海表粗糙度参数化方案的敏感性。结果表明:LINUX系统下的进程通讯技术可以方便有效地实现大气和海浪模式的双向耦合,模式运行稳定;耦合模式能够较好的模拟热带气旋的发展和演变过程及其影响下海浪场的分布和演变,模拟结果对海表粗糙度参数化方案较敏感;海浪的反馈作用同时影响了海气间的动力和热力作用过程,不同的海表粗糙度参数化方案下,海浪对两种作用过程不同的影响程度决定了其对气旋系统强度的影响。  相似文献   

20.
利用实测和实验室数据分析了未破碎变浅海浪波面高度分布三阶矩(或波面偏度)相对于Hs/d的空间演化,利用本文的经验关系,在二阶近似下,给出了以Hs/d为参量的非线性波面表示模式,并推导了功率谱、二阶谱以及波面高度分布函数等特征量.文中还讨论了波面偏度和峰度的相关关系.  相似文献   

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