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水面目标辐射噪声模拟技术是测试被动声呐系统、目标识别定向及水声软对抗的关键技术。通过对辐射噪声信号特性的描述及分析,建立了水面目标频域线谱及连续谱分量的数理仿真模型。针对水声信道影响因素,将Kraken简正波声场模型与信号本身特性有机结合。以1/3倍频程滤波带宽算法为基础,完成了对宽带FIR滤波器组的设计。采用现在应用广泛的GPU(Graphic Processing Unit)并行加速平台,实时实现了目标噪声模拟器整体架构,大大降低了系统硬件资源的消耗。通过对模拟器输出信号进行数理分析,证明了该模拟器能较好地实现水面目标的辐射噪声特性,具备良好的科研应用价值。 相似文献
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运用平面二维数值模拟的方法,在长乐海上风电场B区建成之后对海域的影响进行了研究,将风电桩基概化为边长为6. 4 m的正六边形,采用网格嵌套、逐层加密的方式对研究区地形进行刻画,模型经过6个测点和1个临时潮位站实测资料的验证,表明模型结果良好,能够反映研究区潮流性质,并模拟风电场建成后对所在海域和风电桩基附近的影响。模型计算结果表明,风电场建成后对所在海域的主要影响集中在桩基附近,对流场影响主要体现在流速的变化上,在桩基根部附近,流速会因为桩基之间的束水效应增大;在桩基周围因为其阻水效应,桩基背水面和迎水面流速均会减小,且背水面流速变化范围会大于迎水面。工程会对北部两排桩基周围的余流产生10%左右的影响,产生30%数值变化的范围仅在桩基根部。 相似文献
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提出直接由MATLAB读入光纤端面图实现复杂结构光子晶体光纤(PCF)模型的快速建立,并综合平面波法(PWM)和频域有限差分(FDFD)法,模拟分析带隙型光子晶体光纤(PBG-PCF)的带隙和模场分布.利用PWM计算得到了在PBG-PCF中传输的光波频率及模式有效折射率范围;基于FDFD法在给定波长及模式有效折射率范围情况下,模拟得到了PBG-PCF中可能存在的模场分布及其他特性.以市售的PBG-PCF为例,验证了数值模拟的正确性,随后系统地分析了结构参数(晶格结构、"原子"占有率、背景材料折射率及"原子 相似文献
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A three-dimensional, eddy-permitting ocean circulation model with implemented bottom boundary layer model and flux-corrected transport scheme is used to calculate the pathways and ages of various water masses in the Baltic Sea. The agreement between simulated and observed temperature and salinity profiles of the period 1980–2004 is satisfactory. Especially the renewal of the deep water in the Baltic proper by gravity-driven dense bottom flows is better simulated than in previous versions of the model. Based upon these model results details of the mean circulation are analyzed. For instance, it is found that after the major Baltic inflow in January 2003 saline water passing the Słupsk Furrow flows directly towards northeast along the eastern slope of the Hoburg Channel. However, after the baroclinic summer inflow in August/September 2002 the deep water flow spreads along the southwestern slope of the Gdansk Basin. Further, the model results show that the patterns of mean vertical advective fluxes across the halocline that close the large-scale vertical circulation are rather patchy. Mainly within distinct areas are particles of the saline inflow water advected vertically from the deep water into the surface layer. To analyze the time scales of the circulation mean ages of various water masses are calculated. It is found that at the sea surface of the Bornholm Basin, Gotland Basin, Bothnian Sea, and Bothnian Bay the mean ages associated to inflowing water from Kattegat amount to 26–30, 28–34, 34–38, and 38–42 years, respectively. Largest mean sea surface ages of more than 30 years associated to the freshwater of the rivers are found in the central Gotland Basin and Belt Sea. At the bottom the mean ages are largest in the western Gotland Basin and amount to more than 36 years. In the Baltic proper vertical gradients of ages associated to the freshwater inflow are smaller than in the case of inflowing saltwater from Kattegat indicating an efficient recirculation of freshwater in the Baltic Sea. 相似文献
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象山港水交换数值研究 Ⅱ.模型应用和水交换研究 总被引:21,自引:4,他引:21
使用水平二维对流-扩散型水交换模式模拟研究了象山港的水交换,对不同区域的水交换控制机理作了初步探讨,象山港水交换状况与其控制机制的区域性变化很大。牛鼻水道至佛渡水道是一个潮流较强的潮通道;90%水交换周期为5天左右。象山港狭湾内水交换周期较长,湾顶处90%水交换的周期约为80天左右。 相似文献
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Estimation of horizontal salt transfer from the central part of the Black Sea to the continental slope is carried out based on numerical modeling. A box hydrodynamic model of the Black Sea based on the POM model is used. Horizontal transport caused by seasonal variability of vertical velocity in the central part of the Black Sea and horizontal turbulent diffusion is considered. In this work we demonstrate that, in the 0- to 30-m layer on average for the year, there is an outflow of salty water under the impact of both factors. In the surface layer, the transport caused by seasonal variability contributes significantly (30%). In the 80- to 150-m layer on average over the year, the waters from the continental slope arrive into the central part of the basin; they are characterized by higher salinity due to the inflow of the Marmara Sea waters across the Bosporus Strait. 相似文献
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北极冰海耦合模式对两种不同大气再分析资料响应的分析 总被引:2,自引:2,他引:0
本文中我们比较了Climate Forecast System Reanalysis(CFSR)高分辨率的再分析数据集和低分辨率的Japanese 25-year Reanalysis Project(JRA25)再分析数据集在向下短波辐射、向下长波辐射、10m风场、近地面气温、降水、湿度上的不同,发现二者差异最大的为降水数据,其次为向下短波辐射数据、向下长波辐射数据。用这两个数据集驱动同一冰海耦合模式,CFSR强迫的海冰、北冰洋中层水和加拿大海盆温盐结构与实测相比有很大差距,等密度面上的地转流速在加拿大海盆和欧亚海盆比JRA25强迫的结果高20%,同时等密度面的深度偏深、位温偏高,在弗拉姆海峡的流通量也比海洋再分析数据Simple Ocean Data Assimilation(SODA)偏多。CFSR的向下辐射数据更加接近实测,采用此数据的敏感性实验模拟结果与实测符合的更好。对于海冰的模拟,云量起着至关重要的作用,降水带来的淡水通量通过影响大西洋入流水携带的热量进而影响到冰区。此外,CFSR过量的降水也是二者对于北冰洋温盐结构、弗拉姆海峡流通量以及地转流强度模拟产生偏差的主要原因。尽管风场的分辨率不同,在海盆尺度上对于海冰和海水温盐结构的影响并不大。 相似文献
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The dynamics in the transition zone between the North Sea and Baltic Sea are analyzed here using data from a 22-year-long climatic simulation with a focus on the periods 1992–1994 and 2001–2003 when two recent major inflow events occurred. Observations from gauges and in situ measurements are used to validate the model. Parameters, which cannot be easily measured, such as water and salt transports through straits, have been compared against similar previous estimates. The good performance of simulations is attributed to the finer resolution of the model compared to earlier set ups. The outflow in the Kattegat, which is an analogue of the tidal outflows, tends to propagate to the North over the shallows without showing a substantial deflection to the right due to the Earth's rotation. The inflow follows the topography. The different inflow and outflow pathways are explained as a consequence of the specific combination of bathymetry, axial and lateral processes. The circulation in Kattegat is persistently clockwise with an eastern intensification during inflow and a western one during outflow regimes. The tidal wave there propagates as Kelvin wave, keeping the coast on its right. The flows in the two main straits reveal very different responses to tides, which are also highly asymmetric during inflow and outflow conditions. The circulation has a typical two-layer structure, the correlation between salinity and velocity tends to increase the salt transport in the salinity conveyor belt. The transversal circulation in the entrance of the Sound enhances the vertical mixing of the saltier North Sea water. The long-term averaged ratio of the water transports through the Great Belt and the Sound is ∼2.6-2.7 but this number changes reaching lower values during the major inflow in 1993. The transports in the straits are asymmetric. During inflow events the repartition of water penetrating the Baltic Sea is strongly in favor of the pathway through the Sound, which provides a shorter connection between the Kattegat and Baltic proper. The wider Great Belt has a relatively larger role in exporting water from the Baltic into the North Sea. A demonstration is given that the ventilation of the Baltic Sea deep water is not only governed by the dynamics in the straits and the strong westerly winds enhancing the eastward propagation of North Sea water (a case in 1993), but also by the clockwise circulation in the Kattegat acting as a preconditioning factor for the flow-partitioning. 相似文献
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A 0.4 m diameter (1:30th scale) horizontal axis marine current turbine (MCT) was tested in a circulating water channel. The turbine performance and wake characteristics were determined over a range of flow speeds and rotor thrust coefficients. Measurements of the water surface elevation profiles indicated increasing variation and surface turbulence with increasing flow speeds. Blockage-type effects (where the measured point velocity was greater than the inflow velocity) occurred around the sides of the rotor for all flow speeds. Although the effects were exaggerated at model scale, it is expected that reasonable variations in water level and flow velocity could also occur over a full scale MCT array. 相似文献
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渤、黄、东海夏季环流的数值模拟 总被引:18,自引:1,他引:18
在POM的基础上 ,建立一个σ坐标系下的三维斜压预报模式 ,考虑了海底地形、外来流、长江径流、海面风应力、海面热交换等多方面因素的影响 ,较好地模拟了夏季东中国海环流的情况。其结果表明 ,黑潮在流经东海时沿东海陆坡流动 ,其途径随陆坡等深线走向而变 ,在其两侧出现一些涡旋。夏季台湾暖流上层水主要来自台湾海峡 ,底层水主要由台湾东面黑潮的次表层水入侵陆架生成。夏季进入朝鲜海峡的对马暖流的来源是多方面的 ,其中有 :台湾暖流、黑潮分支、长江冲淡水与西朝鲜沿岸流的混合水。长江冲淡水在出长江口后 ,很快转向北流动 ,到34°N附近转向东南方向。在长江口东北面存在两个中尺度的涡旋。夏季黄海冷水环流由南北两部分组成 ,表层流速大 ,底层流速小。在青岛 石岛附近还存在一个中尺度的反气旋型涡旋 相似文献
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A 3D,time-dependent,baroclinic,hydrodynamic and salinity model was implemented and applied to the Oujiang River estuarine system in the East China Sea.The model was driven by the forcing of tidal elevations along the open boundaries and freshwater inflows from the Oujiang River.The bottom friction coefficient and vertical eddy viscosity were adjusted to complete model calibration and verification in simulations.It is demonstrated that the model is capable of reproducing observed temporal variability in the water surface elevation and longitudinal velocity,presenting skill coefficient higher than 0.82.This model was then used to investigate the influence of freshwater discharge on residual current and salinity intrusion under different freshwater inflow conditions in the Oujiang River estuary.The model results reveal that the river channel presents a two-layer structure with flood currents near the bottom and ebb currents at the top layer in the region of seawater influenced on north shore under high river flow condition.The river discharge is a major factor affecting the salinity stratification in the estuarine system.The water exchange is mainly driven by the tidal forcing at the estuary mouth,except under high river flow conditions when the freshwater extends its influence from the river’s head to its mouth. 相似文献
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D. G. Chechin I. A. Repina V. M. Stepanenko 《Izvestiya Atmospheric and Oceanic Physics》2010,46(4):499-510
The influence that cool skin has on the energy exchange between the atmosphere and the ocean is investigated in this work.
For this purpose, a series of numerical experiments with the use of the one-dimensional LAKE model of a water body were performed.
Three types of cold-skin parameterization were used in this model. The data of in situ measurements in the coastal zone of
the Black Sea, in the Arctic Ocean, and over Lake Sparkling served as the boundary and initial conditions. It has been established
from the results of experiments that the LAKE model with the incorporated parameterization of the cool skin successfully reproduces
cold-skin characteristics, namely, the difference between the temperature of the cool skin surface and the water temperature
below the skin. The results of numerical experiments are within the variability of the results of in situ measurements. It
has been shown that the presence of a cool skin reduces the heat losses of a body of water. The numerical experiments showed
that the presence of a cool skin can change the thermal regime of a water body and its stratification by changing the heat
balance at the surface. This result can be important for the modeling of many processes inside a body of water and at its
surface, for example, gas and heat exchange. 相似文献
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S. N. Moshonkin G. V. Alekseev N. A. Dianskii A. V. Gusev V. B. Zalesny 《Izvestiya Atmospheric and Oceanic Physics》2011,47(5):628-641
Calculations were performed using a model of the combined circulation of the Atlantic Ocean (from 20° S), the Arctic Ocean, and the Bering Sea with a resolution of 0.25° by latitude and longitude for 1958–2006. The results are compared with observational data and results obtained by other models. Model estimates were obtained for the evolution of the Atlantic water inflow into the Arctic basin through the Fram Strait and the Barents Sea. Increased transports of Atlantic water inflow into the Arctic basin were found for the first half of the 1990s and 2004–2006. The relation between Atlantic water transports into the Arctic basin and variations in the North Atlantic oscillation is shown. A positive trend of Atlantic water inflow into the Arctic basin through the Fram Strait (0.061 Sv per year) was revealed. The evolution of the freshwater-layer thickness in the Beaufort Circulation (BC) is considered. There are three periods of its increased values combined with the increased anticyclonic vorticity of BC currents: the 1960s, the 1980s, and from 1999 until now. The model estimate for a statistical mean timescale of the cycle of freshwater concentration and sink from the BC is 16 years, which is close to currently existing estimates. The evolution of anticyclonic vorticity of currents leads the variations in the freshwater-layer thickness of the BC by 1.75 years. Since the mid-1970s, there have been long positive trends of both the freshwater-layer thickness and anticyclonic vorticity of currents in the BC. In the same time period, there has been a satellite-registered negative trend in the ice area in the Arctic, which was reproduced by the model. 相似文献