Meissel-Stokes核函数应用于区域大地水准面分析   总被引：1，自引：0，他引：1  

荣敏  周巍  任红飞 《测绘工程》2015,(9):5-10

为提高区域大地水准面计算精度,基于EGM2008地球重力场位系数模型分析Meissel-Stokes核函数、截断误差系数以及截断误差。选取实验区,采用移去-恢复法评价Meissel-Stokes核函数计算大地水准面的精度。结果表明:Meissel-Stokes核函数及其截断误差系数收敛速度快;截断误差小且稳定。在积分半径不易扩展的情况下,应用Meissel-Stokes核函数计算区域大地水准面,比标准Stokes计算大地水准面精度略高。  相似文献   

Analysis of water seepage in a pavement system using the particulate approach     

Kalyani Jeyisanker  Manjriker Gunaratne 《Computers and Geotechnics》2009

A particulate model has been developed to analyze the effects of transient and steady state seepage of water through a randomly-packed coarse-grained soil as an alternative to conventional seepage analysis based on continuum models. In this model, the soil skeleton and the pore water are volumetrically coupled in the transient and steady-state conditions. The concept of relative density has been used to define different compaction levels of the soil layers forming a pavement filter system and observe the seepage response to compaction. First, Monte–Carlo simulation is used to randomly pack discrete spherical particles from a specified particle size distribution (PSD) to achieve a desired relative density based on the theoretical minimum and maximum void ratios. Then, a water pressure gradient is applied across one two-layer unit to trigger water seepage. The interstitial pore water motion is idealized using Navier–Stokes (NS) equations with provision to incorporate the drag forces acting between the pore fluid and soil particles. The NS equations are discretized using finite differences and applied to discrete elements in a staggered, structured grid. The model predicted hydraulic conductivities are validated using widely used equations.  相似文献   

Variation of the Sectional Drag Coefficient of a Group of Buildings with Packing Density   总被引：2，自引：2，他引：0  

J. L. Santiago  O. Coceal  A. Martilli  S. E. Belcher 《Boundary-Layer Meteorology》2008,128(3):445-457

Reynolds-averaged Navier–Stokes (RANS) simulations of turbulent flow over groups of buildings with different packing densities are reported. The results for a selected packing density are compared with direct numerical simulations (DNS) previously validated against wind-tunnel data. The present study is focused on average properties of the flow, especially on the drag coefficients, and is a first attempt to provide information on these parameters (their values are not generally known) for a range of packing densities, for a given staggered arrangement of cubes using RANS methods. However, some of the limitations of RANS have come to light. Hence, it is recommended that such simulations are ‘calibrated’ against experimental or DNS data, as is done here.  相似文献   

���ֵ����Ŷ���������ģ�͵ķ�����Ƚ�     

马彪  刘晓刚  张丽萍 《大地测量与地球动力学》2012,32(1):105-109

??360??EGM2008???????????????????????????????????????????п????????????????????????????????????Ч???????????????????????????п?????????????????????????????????????????????????????????????????????????????????????????????  相似文献   

热力学效应及斯托克斯漂流对混合层影响的研究     

李雪薇  赵栋梁  邹仲水 《海洋学报(英文版)》2020,42(5):35-45

本文通过理想化的外部强迫以及海洋站点实测数据驱动普林斯顿海洋模式来研究海洋热力学效应和斯托克斯漂流对上混合层数值模拟的影响。在Mellor-Yamada湍流闭合方案中，经常出现夏季海表面温度偏暖和混合层深度偏浅的模拟误差。实验表明，斯托克斯漂流在冬季和夏季均能增强湍流动能，加深混合层深度。这种效应可以改善夏季的模拟结果，但与观测数据相比，将增大冬季混合层深度的模拟误差。斯托克斯漂流可以通过增强湍动能来加深混合层深度。结果表明，将斯托克斯漂流与冷皮层和暖层对上部混合层的热效应相结合，可以正确地模拟混合层深度。在夏季，海洋冷皮层和暖层通过“阻挡结构”和双温跃层结构模拟出更真实的上混合层变化。在冬季，海洋热力学效应通过增强上层海洋层结平衡了斯托克斯漂流的影响，并且由斯托克斯漂流引起的过度混合被校正。  相似文献   

台风过程中浪致Stokes漂流对海洋上层温度影响的数值模拟     

史剑  朱超  刘经东  刘振宇 《海洋与湖沼》2019,50(6):1209-1222

Stokes漂流对海洋上层温度变化具有重要影响。本文以"麦德姆(Matmo)"台风过程为例,基于浪流耦合模型,通过对比分析考虑和未考虑Stokes漂流的模拟结果,研究了台风过程中浪致Stokes漂流及其效应对海洋上层温度变化的影响。研究表明Stokes漂流及其效应与海浪大小的分布密切相关,海浪越大, Stokes漂流、Stokes输运和Ekman-Stokes数相对越大。Stokes漂流在台风过程中起降低海表面温度的作用,台风路径处的Stokes漂流及其效应较大,降温较明显,最大降温约2°C。产生降温的原因是Stokes漂流造成海表流场改变,以及Stokes输运引起海水辐散等作用加强了上下层海水质量和能量的交换。利用Argo资料进行验证,发现考虑了Stokes漂流作用的海洋上层温度模拟结果与Argo测量结果更接近。  相似文献   

一种改进的基于逆Omega-K算法的海面场景SAR原始数据仿真方法     

端和阳  刘保昌  何宜军  李秀仲 《海洋与湖沼》2019,50(2):291-300

合成孔径雷达(SAR)海面场景原始数据仿真是研究海洋动力参数(表面波浪、风矢量和洋流)的有效工具。目前海面场景原始数据仿真方法已经基于逆Omega-K算法实现了海洋运动参数的空间变化。但是目前仅仅讨论了正侧视情况下的海面场景仿真,应用范围有限,同时没有考虑Stokes漂流以及Bragg相速度的影响,而这两者都是存在于真实海面的。通常情况下为了反演得到海面流场的二维速度矢量,雷达需要从两个不同的方位方向观察海面的同一个区域,因此这就需要考虑大斜视的雷达波束,同时Stokes漂流和Bragg相速度是SAR海表面流场观测不容忽视的两种运动。本文在不改变原有正侧视逆Omega-K算法的情况下,通过增加重新计算零方位时刻的斜视波束中心位置坐标,并据此确定SAR原始数据在多普勒域的位置来将其扩展到大斜侧视逆Omega-K算法,并通过时域Stokes漂流公式到频域内离散化Stokes漂流公式的推导来加入Stokes漂流,以及根据Bragg散射机制加入了Bragg相速度。仿真结果表明,经过聚焦成像后的SAR图像很好的体现了真实海面波浪场的形状,同时能够很好地反演出设定的雷达径向流场速度,且流速精度误差控制在6%以内。最后也证明了Bragg相速度以及Stokes漂流对于海面流场的影响不可忽视。  相似文献   

全球Stokes 漂流的时空分布特征研究     

张晓爽  王智峰  王斌  吴克俭  韩桂军  李威 《海洋科学》2015,39(1):93-103

利用海浪模式WWIII(Wave Watch III)2008年的模拟结果对海面Stokes漂流、Stokes输运、Stokes深度以及全球Langmuir数的年平均分布特征和季节平均分布特征分别进行了详细的研究与分析。结果表明,海面Stokes漂流和Stokes输运均呈现高纬度偏大的特征,以南极绕极流海域最为突出。全球大部分海域Stokes漂流影响深度在20 m以内,呈现大洋东部偏大,西部偏小的分布特征。全球大部分海域的混合作用是剪切不稳定性和Langmuir湍效应并存的状态,甚至有些海域是以Langmuir湍效应为主。因此,在进行大尺度的海洋数值模拟时,应该考虑波浪导致的混合效应。  相似文献   

The validity of the independence principle applied to the vortex-induced vibration of an inclined cylinder in steady flow     

《Applied Ocean Research》2015

The validity of the independence principle applied to the vortex-induced vibration (VIV) of an inclined cylinder in steady flow is investigated by conducting numerical simulations. In order to create a perfect end-effect-free condition, periodic boundary condition is applied on the two end boundaries that are perpendicular to the cylinder. It is found that the response amplitude and frequency for an inclination angle of α = 45° agree well with their counterparts for α = 0°. The numerical results demonstrated the validity of the independence principle in the case of vortex-induced vibration, which has not been demonstrated by laboratory tests due to the difficulty in avoiding the end effects.  相似文献   

Evaluation of the simulation capability of the Wavewatch Ⅲ model for Pacific Ocean wave   总被引：1，自引：0，他引：1  

毕凡  宋金宝  吴克俭  徐尧 《海洋学报(英文版)》2015,34(9):43-57

Wave climate analysis and other applications for the Pacific Ocean require a reliable wave hindcast. Five source and sink term packages in the Wavewatch III model(v3.14 and v4.18) are compared and assessed in this study through comprehensive observations, including altimeter significant wave height, advanced synthetic aperture radar swell, and buoy wave parameters and spectrum. In addition to the evaluation of typically used integral parameters, the spectra partitioning method contributes to the detailed wave system and wave maturity validation. The modified performance evaluation method(PS) effectively reduces attribute numbers and facilitates the overall assessment. To avoid possible misleading results in the root mean square error-based validations, another indicator called HH(indicating the two authors) is also calculated to guarantee the consistency of the results. The widely used Tolman and Chalikov(TC) package is still generally efficient in determining the integral properties of wave spectra but is physically deficient in explaining the dissipation processes. The ST4 package performs well in overall wave parameters and significantly improves the accuracy of wave systems in the open ocean. Meanwhile, the newly published ST6 package is slightly better in determining swell energy variations. The two packages(ACC350 and BJA) obtained from Wavewatch III v3.14 exhibit large scatters at different sea states. The three most ideal packages are further examined in terms of reproducing waveinduced momentum flux from the perspective of transport. Stokes transport analysis indicates that ST4 is the closest to the NDBC-buoy-spectrum-based transport values, and TC and ST6 tend to overestimate and underestimate the transport magnitude, respectively, in swell mixed areas. This difference must be considered,particularly in air–wave–current coupling research and upper ocean analysis. The assessment results provide guidance for the selection of ST4 for use in a background Pacific Ocean hindcast for high wave climate research and China Sea swell type analysis.  相似文献