On the peculiarity of the sound channel on the shelf of the North-European basin     

I. P. Voloshina  O. Ya. Sochnev 《Physical Oceanography》1991,2(5):393-396

Analysis of the sections traversing the polar hydrological front on the shelf of the North-European basin has enabled us to reveal the areas limited by closed isotaches of the sound velocity existing in the interfrontal zone at depths of 50–150 m. These areas represent the closed waveguide which has the property of an underwater sound channel.Translated by Mikhail M. Trufanov.  相似文献   

沙坝—泻湖海岸动力地貌学研究进展   总被引：6，自引：0，他引：6  

何为  李春初  雷亚平 《台湾海峡》2001,20(4):565-572

国内外对沙坝－泻湖海岸的研究主要采取动力地貌学的方法，本文评述了近一个半世纪以来在这一领域所取得的重要成果。波浪、潮汐、径流等特殊的动力场决定了泥沙输运的方式和路径，从而形成了与其相应的沙坝、泻湖、潮汐通道三大地貌体系。  相似文献   

轻质硬壳海堤断面设计初探     

叶培伦  陶松垒等 《海洋工程》2001,19(2):88-91

从海堤本身角度看，坝体过重与填料松散是影响其稳定性的主要因素，因此轻质硬壳堤坝是一种很好的选择。该结构采用高强度材料作为外壳，以松散材料填充坝体。根据受力特性、构造要求、施工条件及抗滑稳定条件拟解决结构断面设计的一些基本问题，并结合实例通过对比计算分析，说明轻质硬壳海堤比传统海堤具有更高的整体稳定性。  相似文献   

潮流场数学方程交错分区并行计算方法研究   总被引：1，自引：0，他引：1  

张树生  陶建华 《海洋技术学报》2005,24(1):72-76

文章对潮流场数学方程进行可并行性方法研究。分析了两种可并行实现的方法，并对两种可并行化的方法可行性进行分析。最后采用虚拟区域分解法对问题进行了实现，并利用串行计算的结果对并行计算的结果进行了验证。  相似文献   

波浪作用下近岸区污染物输移扩散的数学模型及其实验验证   总被引：2，自引：1，他引：2       下载免费PDF全文

孙涛  陶建华 《海洋学报》2003,25(3):104-112

在近岸缓坡浅水海岸,波浪破碎产生沿岸流是近岸海域流场的重要组成部分,它对污染物输移扩散规律的影响重大,在高阶近似抛物化缓坡方程求解大面积波浪场基础上,建立了波浪作用下污染物输移扩散数学模型.计算结果与不同坡度均匀斜坡地形上具有不同波高、周期的规则波及不规则波浪作用下污染物输移扩散实验结果进行了比较,分析了各种因素对波浪作用下沿岸流分布规律影响,所得结论认为地形坡度及入射波高对污染物输移扩散的影响较大,波浪作用将使缓坡海滩上污染物的输移扩散平行岸线方向.  相似文献   

Regularities of variation of the heliospheric current sheet orientation during the solar activity cycle     

R. A. Gulyaev  N. Ya. Vanyarkha 《Solar physics》1992,140(2):369-378

Evolution of spatial orientation of the heliospheric current sheet (HCS) has been studied in detail using synoptic maps of the HCS configuration over the period 1971–1989. Analysis involves all phases of the sunspot cycle except for two years of maximum solar activity. The helmet-like coronal streamers are confirmed to be structural elements of the HCS. The r.m.s. deviation of a real HCS configuration from a plane does not exceed about 10° during most of the sunspot cycle length. Hence, minimum-type corona should be observed every time the HCS is oriented parallel to the line-of-sight, independent of the cycle phase. Such occasions have been observed apart from the sunspot minimum epochs at the solar eclipses of 31 August, 1932 and 11 July, 1991.Regularities of variation of the two following parameters of the HCS orientation have been revealed: obliquity to the solar equator plane (heel or tilt) and longitudinal orientation (yawing). Behaviour of the above parameters is repeated in different cycles. However, heeling and yawing occur probably not synchronous but rather independent of one another.  相似文献   

Tectonics of the Venus and the early Precambrian     

M. S. Markov  Ya. B. Smirnov  L. F. Dobrzhinetskaya 《Earth, Moon, and Planets》1989,45(2):101-113

Analyzing the tectonics of planets and their satellites we use all the information available from the studies of the Earth and other celestial bodies such as the Moon, Mars and Mercury. An important condition in such analysis is naturally the scale of the phenomena compared. Most surface structures of Venus are known to have no direct analogues on the surface of the present Earth, with its global systems of mid-oceanic ridges, deep trenches and vast lithospheric plates. This might be due to the sharp differences in the present thermal regimes of the Earth and Venus. It has already been suggested in numerous papers that the key to the genesis of the Cytherean surficial structures must be looked for in the geodynamics of the Early Precambrian Earth.Such an approach appears very logical indeed since the rheology of the present Cytherean crust must be closer to that of the Precambrian rigid lithosphere of the Earth which is as if floating in the low-viscous asthenosphere. An attempt has therefore been made to evaluate certain elements in the tectonics of Venus through the theological properties of its crust comparing structural formation in the low-viscous layers of the Earth crust in the Early Precambrian with data on the morphology of structures on the surface of Venus.  相似文献   

Intelligent control for modeling of real‐time reservoir operation,part II: artificial neural network with operating rule curves     

Ya‐Ting Chang  Li‐Chiu Chang  Fi‐John Chang 《水文研究》2005,19(7):1431-1444

To bridge the gap between academic research and actual operation, we propose an intelligent control system for reservoir operation. The methodology includes two major processes, the knowledge acquired and implemented, and the inference system. In this study, a genetic algorithm (GA) and a fuzzy rule base (FRB) are used to extract knowledge based on the historical inflow data with a design objective function and on the operating rule curves respectively. The adaptive network‐based fuzzy inference system (ANFIS) is then used to implement the knowledge, to create the fuzzy inference system, and then to estimate the optimal reservoir operation. To investigate its applicability and practicability, the Shihmen reservoir, Taiwan, is used as a case study. For the purpose of comparison, a simulation of the currently used M‐5 operating rule curve is also performed. The results demonstrate that (1) the GA is an efficient way to search the optimal input–output patterns, (2) the FRB can extract the knowledge from the operating rule curves, and (3) the ANFIS models built on different types of knowledge can produce much better performance than the traditional M‐5 curves in real‐time reservoir operation. Moreover, we show that the model can be more intelligent for reservoir operation if more information (or knowledge) is involved. Copyright © 2004 John Wiley & Sons, Ltd.  相似文献   

Editorial note to the special issue on the Chelyabinsk Event     

M. Ya. Marov  B. M. Shustov 《Solar System Research》2013,47(4):239-239

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Late Pleistocene-Holocene events on the continental slope of the Laptev Sea: Evidence from benthic and planktonic foraminiferal assemblages     

Ya. S. Ovsepyan  E. E. Taldenkova  H. A. Bauch  E. S. Kandiano 《Stratigraphy and Geological Correlation》2015,23(6):645-660

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